A Global Index for Mapping the Exposure of Water Resources to Wildfire
Open accessAbstract
Wildfires are keystone components of natural disturbance regimes that maintain ecosystem structure and functions, such as the hydrological cycle, in many parts of the world. Consequently, critical surface freshwater resources can be exposed to post-fire effects disrupting their quantity, quality and regularity. Although well studied at the local scale, the potential extent of these effects has not been examined at the global scale. We take the first step toward a global assessment of the wildfire water risk (WWR) by presenting a spatially explicit index of exposure. Several variables related to fire activity and water availability were identified and normalized for use as exposure indicators. Additive aggregation of those indicators was then carried out according to their individual weight. The resulting index shows the greatest exposure risk in the tropical wet and dry forests. Intermediate exposure is indicated in mountain ranges and dry shrublands, whereas the lowest index scores are mostly associated with high latitudes. We believe that such an approach can provide important insights for water security by guiding global freshwater resource preservation.
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Written from the paper’s full text.
TL;DR
The paper introduces the Global Wildfire Water Exposure Index (GWWEI), a 0–100 global raster index combining seven fire and water indicators to map where water resources are exposed to wildfire. It finds highest exposure in tropical wet and dry forests, intermediate exposure in mountains and dry shrublands, and lowest exposure at high latitudes, while sensitivity analysis shows water indicators dominate the index.
Key findings
- Highest GWWEI scores are concentrated in tropical latitudes, especially the Amazon basin, Congo basin, and Indonesia; moderately high scores occur in subtropical humid forests, fire-prone dry forested savannas, and many mountain ranges; intermediate scores appear in dry savannas, dry steppes, and dry shrublands; lowest scores are in temperate prairies, northern boreal forest, and tundra.
- Spearman correlations with the GWWEI are highest for water indicators: AET 0.76, SM 0.74, and SR 0.66; among fire indicators, NI is 0.55 and AB is 0.21, while FD (0.11) and AI (0.06) show low influence.
- The weighting scheme assigns 50% to fire indicators and 50% to water indicators, with 16.6% per water indicator and 12.5% per fire indicator; final pixel scores theoretically range from 0 to 100.
- Sensitivity analysis created 51 modified indices; highest coefficient of variation is mostly at northern latitudes, the tundra, and the northern circumboreal fringe, with moderately high variability in dense human-pressure areas and some mountain ranges, while lowest variability is in tropical savannas and dry temperate steppes except the North American prairies and northern Australia.
Methods
- Design: a spatially explicit global exposure index (GWWEI) for wildfire water risk, using seven indicators—area burned (AB), fire danger (FD), natural ignitions (NI), anthropogenic influence (AI), surface runoff (SR), soil moisture (SM), and actual evapotranspiration (AET)—normalized to 0–100 and aggregated additively by weight.
- Data: off-the-shelf global datasets were rasterized, reprojected to WGS84, and resampled to 0.5°; the FWI layer was used as an extraction mask to exclude deserts, and small islands, Greenland, and Antarctica were removed (28% of global land surface).
- Analysis: sensitivity was tested with one non-spatial approach and six spatial approaches—Spearman/Pearson correlations, stepwise addition, jackknifing, low/high case scenarios, random weighting, and systematic weighting—producing 51 modified indices and coefficient-of-variation maps.
Limitations
- Stated: water resource indicators overwhelm fire-related indicators in the GWWEI pattern, raising questions about the equal-weight assumption; future versions should use expert opinion or a larger variable set to improve weighting.
- Stated: the indicator list is intentionally simple, data availability dependent, and based on long-term averages with some temporal mismatches; global proxies may not be suitable for small areas, and the framework only considers overlapping additive effects without downstream cumulative effects or spatial transmission/downstream routing.
- Evident from the text: the GWWEI does not describe a quantitative likelihood or probability of impacts; it depicts geographic overlay of drivers and should be interpreted with local environmental, socio-cultural, and economic factors, and the simple correlation coefficients do not explore nonlinear relationships or interactions.
Model-written summary. Check it against the paper before relying on it.
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Claims the paper makes
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- Findingown data§ AGlobal Index for Mapping the Exposure of Water Resources to Wildfire · p. 1
The GWWEI indicates intermediate exposure in mountain ranges and dry shrublands.
“Intermediate exposure is indicated in mountain ranges and dry shrublands”
- Also stated in: § 3.1. Geography of the GWWEI · p. 7 · plain
“Intermediate scores are shown in dry savannas, dry steppes and dry shrublands on all continents, as well as in the Mediterranean, the northwest of the Eurasian boreal forest and the southern range of the North American boreal forest.”
Quote in the paperNot a substantial claim- The authors state this as an assumption: Areas with higher surface runoff play a prominent role in the amount of available water resources and are more vulnerable to disturbances.
- The authors state this as an assumption: A drop in soil moisture content after a fire is caused by greater inputs of radiative energy, which negatively impact surface runoff levels and amounts of water during the dry season.
- The authors state this as an assumption: Without vegetation interception and respiration, actual evapotranspiration will mainly be converted to runoff.
- Also stated in: § 3.1. Geography of the GWWEI · p. 7 · plain
- Findingown data§ AGlobal Index for Mapping the Exposure of Water Resources to Wildfire · p. 1
The lowest GWWEI scores are mostly associated with high latitudes.
“whereas the lowest index scores are mostly associated with high latitudes.”
- Also stated in: § 3.1. Geography of the GWWEI · p. 7 · plain
“The lowest scores are seen in the temperate prairies of North America, South America and Eurasia, as well as in the northern boreal and the tundra (Figure 3b).”
Quote in the paperNot a substantial claim- The authors state this as an assumption: Areas with higher surface runoff play a prominent role in the amount of available water resources and are more vulnerable to disturbances.
- The authors state this as an assumption: A drop in soil moisture content after a fire is caused by greater inputs of radiative energy, which negatively impact surface runoff levels and amounts of water during the dry season.
- The authors state this as an assumption: Without vegetation interception and respiration, actual evapotranspiration will mainly be converted to runoff.
- Also stated in: § 3.1. Geography of the GWWEI · p. 7 · plain
- Findingown data§ AGlobal Index for Mapping the Exposure of Water Resources to Wildfire · p. 1
The GWWEI shows the greatest exposure risk in the tropical wet and dry forests.
“The resulting index shows the greatest exposure risk in the tropical wet and dry forests.”
- Also stated in: § 3.1. Geography of the GWWEI · p. 7 · plain
“Highest scores are concentrated in the tropical latitudes, more specifically in the forests of the Amazon basin, the Congo basin and Indonesia.”
Quote in the paperSubstantial claim- The authors state this as an assumption: Areas with higher surface runoff play a prominent role in the amount of available water resources and are more vulnerable to disturbances.
- The authors state this as an assumption: A drop in soil moisture content after a fire is caused by greater inputs of radiative energy, which negatively impact surface runoff levels and amounts of water during the dry season.
- The authors state this as an assumption: Without vegetation interception and respiration, actual evapotranspiration will mainly be converted to runoff.
- Also stated in: § 3.1. Geography of the GWWEI · p. 7 · plain
- Findingown data§ 3.1. Geography of the GWWEI · p. 7
Moderately high GWWEI scores are mostly located in subtropical humid forests of southeastern Asia, southeastern North America, Central America, and in fire-prone dry forested savannas of Africa, southeastern South America and southeastern Oceania.
“Moderately high scores are mostly located in the subtropical humid forests of southeastern Asia, southeastern North America, Central America and in fire-prone dry forested savannas of Africa, southeastern South America and southeastern Oceania.”
Quote in the paperNot a substantial claim- The authors state this as an assumption: Areas with higher surface runoff play a prominent role in the amount of available water resources and are more vulnerable to disturbances.
- The authors state this as an assumption: A drop in soil moisture content after a fire is caused by greater inputs of radiative energy, which negatively impact surface runoff levels and amounts of water during the dry season.
- The authors state this as an assumption: Without vegetation interception and respiration, actual evapotranspiration will mainly be converted to runoff.
- Findingown data§ 3.2. Sensitivity of the GWWEI · p. 9
Moderately high to high variability in index scores is also shown in areas of dense human pressure, like Japan, Western Europe and eastern North America.
“Moderately high to high variability in index scores is also shown in areas of dense human pressure, like Japan, Western Europe and eastern North America.”
Quote in the paperNot a substantial claim
- Findingown data§ 3.1. Geography of the GWWEI · p. 7
The lowest GWWEI scores are seen in the temperate prairies of North America, South America and Eurasia, as well as in the northern boreal and the tundra.
“The lowest scores are seen in the temperate prairies of North America, South America and Eurasia, as well as in the northern boreal and the tundra (Figure 3b).”
Quote in the paperNot a substantial claim- The authors state this as an assumption: Areas with higher surface runoff play a prominent role in the amount of available water resources and are more vulnerable to disturbances.
- The authors state this as an assumption: A drop in soil moisture content after a fire is caused by greater inputs of radiative energy, which negatively impact surface runoff levels and amounts of water during the dry season.
- The authors state this as an assumption: Without vegetation interception and respiration, actual evapotranspiration will mainly be converted to runoff.
- Findingnone given§ 3.2. Sensitivity of the GWWEI · p. 9
Moderately low levels of variability cover most of circumboreal, temperate, tropical, and sub-tropical forests and dry shrublands in both hemispheres.
“Moderately low levels of variability cover most of circumboreal, temperate, tropical, and sub -tropical forests and dry shrublands in both hemispheres.”
Quote in the paperNot a substantial claim - Findingown data§ 3.2. Sensitivity of the GWWEI · p. 9
In the stepwise sensitivity analysis, inclusion of AET in the simplest version of the index sets a pattern that is conserved and enforced through all steps.
“This influence of water resource indicators is confirmed by the stepwise approach, where the inclusion of AET in the simplest version of the index (Figure 4a) sets a pattern that is conserved and enforced through all steps (Figure 4b-f)”
Quote in the paperNot a substantial claim - Findingown data§ 3.2. Sensitivity of the GWWEI · p. 9
The highest values of the coefficient of variation (where the index is less robust) are mostly concentrated at northern latitudes (tundra and northern fringe of the circumboreal forest), where water indicators have the most influence on the wildfire water risk exposure pattern.
“The highest values of the coefficient of variation (Figure 5) ( i.e. , where the index is less robust) are mostly concentrated at northern latitudes ( i.e. , the tundra and northern fringe of the circumboreal forest), where water indicators have the most influence on the wildfire water risk exposure pattern (Figure 6).”
Quote in the paperNot a substantial claim - Findingown data§ 3.2. Sensitivity of the GWWEI · p. 9
In the stepwise sensitivity analysis, SM is critical in setting the pattern for mountain ranges, such as the Himalayas or Southern Alaska.
“with SM being critical in setting the pattern for mountain ranges, such as the Himalayas or Southern Alaska”
Quote in the paperNot a substantial claim - Findingown data§ 3.2. Sensitivity of the GWWEI · p. 9
In the stepwise sensitivity analysis, SM increases scores for the southern fringe of the boreal forest.
“as well as increasing scores for the southern fringe of the boreal forest (Figure 4c)”
Quote in the paperNot a substantial claim - Findingown data§ 3.2. Sensitivity of the GWWEI · p. 9
The most influential fire indicators on the GWWEI are NI (0.55) and AB (0.21), based on Spearman correlation coefficients.
“whereas the most influential fire indicators are NI (0.55) and AB (0.21).”
Quote in the paperNot a substantial claim - Findingown data§ 3.1. Geography of the GWWEI · p. 7
Intermediate GWWEI scores are shown in dry savannas, dry steppes and dry shrublands on all continents, as well as in the Mediterranean, the northwest of the Eurasian boreal forest and the southern range of the North American boreal forest.
“Intermediate scores are shown in dry savannas, dry steppes and dry shrublands on all continents, as well as in the Mediterranean, the northwest of the Eurasian boreal forest and the southern range of the North American boreal forest.”
Quote in the paperNot a substantial claim- The authors state this as an assumption: Areas with higher surface runoff play a prominent role in the amount of available water resources and are more vulnerable to disturbances.
- The authors state this as an assumption: A drop in soil moisture content after a fire is caused by greater inputs of radiative energy, which negatively impact surface runoff levels and amounts of water during the dry season.
- The authors state this as an assumption: Without vegetation interception and respiration, actual evapotranspiration will mainly be converted to runoff.
- Findingown data§ 3.2. Sensitivity of the GWWEI · p. 9
The most influential water indicators on the GWWEI are AET (0.76), SM (0.74) and SR (0.66), based on Spearman correlation coefficients.
“The Spearman correlation coefficients (Table 3) between the GWWEI and indicators show that the most influential water indicators are AET (0.76), SM (0.74) and SR (0.66)”
Quote in the paperSubstantial claim - Findingown data§ 3.2. Sensitivity of the GWWEI · p. 9
Several mountain ranges, such as the Andes, the Rocky Mountains, the European and New-Zealand Alps, show moderately high variability values.
“Several mountain ranges, such the Andes, the Rocky Mountains, the European and New -Zealand Alps, also show this range of moderately high values.”
Quote in the paperNot a substantial claim - Findingown data§ 3.4. Limitations and Improvements · p. 12
The sensitivity analysis showed that water resource indicators tend to overwhelm fire-related indicators in the pattern of the GWWEI.
“The sensitivity analysis showed that water resource indicators tend to overwhelm fire-related indicators in the pattern of the GWWEI.”
Quote in the paperSubstantial claim - Premisecitation§ 1. Introduction · p. 2
Global-scale studies or assessments of wildfire effects or risks on water resources are lacking.
“Although a significant number of studies have examined such second-order fire effects on surface freshwater resources [8], most have been conducted at a local or regional scale [8-12], whereas global-scale studies do not exist.”
- Also stated in: § AGlobal Index for Mapping the Exposure of Water Resources to Wildfire · p. 1 · plain
“Although well studied at the local scale, the potential extent of these effects has not been examined at the global scale.”
- Also stated in: § 1. Introduction · p. 2 · plain
“Despite the ubiquitous nature of fire and the potential for adverse consequences on ecosystems and populations [13], large-scale assessments of the risks that fire can pose to water resources are lacking.”
Quote in the paperSubstantial claim0 of 6 sources checked- cites [8] Scott, 2012, Probabilistic assessment of wildfire hazard and municipal watershed exposure, Nat. Hazards source
Not checked in the free run.
- cites [9] Weidner, E., and Todd, A.H. (2011). From the Forest to the Faucet Methods Paper.
Not checked in the free run.
- cites [10] Boerner, C., Coday, B., Noble, J., Roa, P., and Roux, V. (2012). Impacts of Wildfire in Clear Creek Watershed on the City of Golden’s Drinking Water Supply, Colorado School of Mines.
Not checked in the free run.
- cites [11] Moody, J.A., and Martin, D.A. (2004, January 18–21). Wildfire impacts on reservoir sedimentation in the western United States. Proceedings of the Ninth International Symposium on River Sedimentation, Yichang, China.
Not checked in the free run.
- cites [12] Thompson, 2013, Assessing Watershed-Wildfire Risks on National Forest System Lands in the Rocky Mountain Region of the United States, Water source
Not checked in the free run.
- cites [13] Emelko, 2011, Implications of land disturbance on drinking water treatability in a changing climate: Demonstrating the need for “source water supply and protection” strategies, Water Res. source
Not checked in the free run.
- Also stated in: § AGlobal Index for Mapping the Exposure of Water Resources to Wildfire · p. 1 · plain
- Premisecitation§ 1. Introduction · p. 2
Advancements in natural resources global mapping and development of innovative methods and global databases now make it possible to better understand the intersection of wildfire activity and water resource availability at the global scale.
“However, several important advancements in natural resources global mapping [14] and the development of innovative methods and global databases now make it possible to better understand the intersection of wildfire activity [15,16] and water resource availability [17,18] at the scale of the planet.”
Quote in the paperSubstantial claim0 of 5 sources checked- cites [14] Shi, P., and Kasperson, R. (2015). World Atlas of Natural Disaster Risk, Springer. source
Queued — the background check reaches it, usually within a day.
- cites [15] Bowman, 2009, Fire in the Earth System, Science source
Queued — the background check reaches it, usually within a day.
- cites [16] Knorr, 2014, Impact of human population density on fire frequency at the global scale, Biogeosciences source
Not checked in the free run.
- cites [17] Oki, 2006, Global hydrological cycles and world water resources, Science source
Not checked in the free run.
- cites [18] Davies, 2011, Global water resources modeling with an integrated model of the social-economic-environmental system, Adv. Water Resour. source
Not checked in the free run.
- Premisereasoning§ AGlobal Index for Mapping the Exposure of Water Resources to Wildfire · p. 1
Critical surface freshwater resources can be exposed to post-fire effects that disrupt their quantity, quality and regularity.
“Consequently, critical surface freshwater resources can be exposed to post-fire effects disrupting their quantity, quality and regularity.”
Quote in the paperNot a substantial claim - Premisecitation§ 3.3. The GWWEI and Its Implications for Water Resource Protection · p. 11
Regional studies and reports showed that wildfire risk in source watersheds raises concerns for water treatment and supply.
“Regional studies from Thompson et al. [12], Santos et al. [54] and Moody and Martin [11], as well as reports from the U.S. Forest Service [9] and the Water Research Foundation [55] showed that wildfire risk in source watersheds raises concerns for water treatment and supply.”
Quote in the paperSubstantial claim0 of 3 sources checked- cites Thompson et al. [12] Thompson, 2013, Assessing Watershed-Wildfire Risks on National Forest System Lands in the Rocky Mountain Region of the United States, Water source
Not checked in the free run.
- cites Santos et al. [54] Santos, 2015, Water resources planning for a river basin with recurrent wildfires, Sci. Total Environ. source
Not checked in the free run.
- cites Moody and Martin [11] Moody, J.A., and Martin, D.A. (2004, January 18–21). Wildfire impacts on reservoir sedimentation in the western United States. Proceedings of the Ninth International Symposium on River Sedimentation, Yichang, China.
Not checked in the free run.
- Interpretationown data§ 3.2. Sensitivity of the GWWEI · p. 9
The correlation between the GWWEI and water indicators explains the pattern of high index values in tropical areas, which naturally concentrate a very dynamic hydrological cycle.
“The correlation between the index and water indicators explains the pattern of high values in tropical areas, which naturally concentrate a very dynamic hydrological cycle.”
Quote in the paperNot a substantial claim - Premisecitation§ 3.3. The GWWEI and Its Implications for Water Resource Protection · p. 11
78% of large cities on the planet are dependent on surface freshwater.
“as is the case with 78% of large cities on the planet [60].”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites [60] McDonald, 2014, Water on an urban planet: Urbanization and the reach of urban water infrastructure, Glob. Environ. Chang. source
Not checked in the free run.
- Premisecitation§ 2.1. Data Selection and Indicators' Definition · p. 4
The reduction of vegetation cover after a fire might impact actual evapotranspiration levels.
“The reduction of the vegetation cover after a fire might impact actual evapotranspiration (AET) levels [44]”
Quote in the paperSubstantial claim0 of 1 sources checked- cites [44] Nolan, 2014, Changes in evapotranspiration following wildfire in resprouting eucalypt forests, Ecohydrology source
Not checked in the free run.
- Interpretationreasoning§ 3.3. The GWWEI and Its Implications for Water Resource Protection · p. 11
A high level of GWWEI can have potential implications for water security.
“we argue that a high level of GWWEI can have potential implications for water security.”
Quote in the paperNot a substantial claim - Study design and conductreasoning§ 2.3. Sensitivity Analysis · p. 7
Areas showing higher variability in the GWWEI are more sensitive to changes in the indicators' values.
“We averaged those to produce a map of the per-pixel mean variability of the GWWEI scores, where areas showing higher variability are thus more sensitive to changes in the indicators' values.”
Quote in the paperNot a substantial claim - Interpretationcitation§ 3.3. The GWWEI and Its Implications for Water Resource Protection · p. 11
The potential implications of a high GWWEI for water security are especially true in areas that are dependent on surface water coming from a highly fire-prone river basin.
“This is especially true in areas that are dependent on surface water coming from a highly fire-prone river basin.”
Quote in the paperSubstantial claim - Interpretationown data§ 3.3. The GWWEI and Its Implications for Water Resource Protection · p. 11
According to the GWWEI, water resources' exposure to fire activity potentially threatens the water supply of a large portion of the human population.
“According to our index, water resources' exposure to fire activity potentially threatens the water supply of a large portion of the human population, as underlined by several localized events.”
Quote in the paperSubstantial claim - Interpretationreasoning§ 3.3. The GWWEI and Its Implications for Water Resource Protection · p. 11
Large and severe wildfires threaten communities dependent on surface freshwater to ensure daily potable water needs.
“This recent event brought to light the threat induced by large and severe wildfires to communities dependent on surface freshwater to ensure daily potable water needs”
Quote in the paperSubstantial claim - Study design and conductcitation§ 2.1. Data Selection and Indicators' Definition · p. 3
The AB indicator, as an average of monthly area burned for the past 20 years, provides a view of areas experiencing most of the fire activity across the planet.
“Our AB indicator, as an average of the monthly area burned for the past 20 years, provides a view of areas experiencing most of the fire activity across the planet.”
Quote in the paperSubstantial claim - Premisenone given§ 2.1. Data Selection and Indicators' Definition · p. 4
Surface runoff can be greatly increased due to changes in water interception by vegetation and alteration of soil properties caused by wildfires.
“It can be greatly increased due to changes in water interception by vegetation and alteration of soil properties caused by wildfires.”
Quote in the paperNot a substantial claim - Interpretationnone given§ 3.1. Geography of the GWWEI · p. 8
High GWWEI scores in mountain ranges are mostly driven by intermediate to high scores of soil moisture.
“whereas high scores in mountain ranges are mostly driven by intermediate to high scores of SM.”
Quote in the paperNot a substantial claim- The authors state this as an assumption: A drop in soil moisture content after a fire is caused by greater inputs of radiative energy, which negatively impact surface runoff levels and amounts of water during the dry season.
- Premisecitation§ 2.1. Data Selection and Indicators' Definition · p. 4
Soil moisture reserves are critical to sustain surface runoff and dry season river-stream baseflows.
“Soil moisture (SM) reserves are critical to sustain surface runoff and dry season river-stream baseflows.”
Quote in the paperSubstantial claim0 of 1 sources checked- cites [39] Kasischke, 2007, Assessing spatial and temporal variations in surface soil moisture in fire-disturbed black spruce forests in Interior Alaska using spaceborne synthetic aperture radar imagery—Implications for post-fire tree recruitment, Remote Sens. Environ. source
Not checked in the free run.
- Premisecitation§ 3.3. The GWWEI and Its Implications for Water Resource Protection · p. 11
Other major blazes in the past decade had significant impacts on several cities' water supply, such as Melbourne, Denver, Boulder, Santa Fe, San Salvador, Caracas and Istanbul.
“Other major blazes that occurred in the past decade had significant impacts on several cities' water supply, such as Melbourne in Australia and Denver, Boulder and Santa Fe in the United States [61], as well as numerous large cities across the world, such as San Salvador, Caracas and Istanbul, all of which are considered exposed to potential water provision issues in case of a major fire in their”
Quote in the paperNot a substantial claim0 of 2 sources checked- cites [61] Bladon, 2014, Wildfire and the Future of Water Supply, Environ. Sci. Technol. source
Not checked in the free run.
- cites [62] Dudley, N., and Stolton, S. (2003). Running Pure, World Bank/WWF Alliance for Forest Conservation and Sustainable Use.
Not checked in the free run.
- Study design and conductcitation§ 2.1. Data Selection and Indicators' Definition · p. 4
Higher levels of anthropogenic influence are considered an indicator of lower fire activity.
“We thus consider higher levels of AI as an indicator of lower fire activity.”
Quote in the paperSubstantial claim0 of 1 sources checked- cites [16] Knorr, 2014, Impact of human population density on fire frequency at the global scale, Biogeosciences source
Not checked in the free run.
- May combine two claims. 30
- Classified as probably not a substantial claim. 40
May combine two claims.
Findingown data§ 3.2. Sensitivity of the GWWEI · p. 9NI and AB are the fire indicators that add the most to the pattern of the final index, whereas FD and AI show surprisingly low influence.
“NI and AB are the fire indicators that add the most to the pattern of the final index, whereas FD and AI show surprisingly low influence.”
Quote in the paperNot a substantial claimMay combine two claims.
Findingown data§ 3.1. Geography of the GWWEI · p. 7A large part of northeastern North America and many mountain ranges across the globe show moderately high GWWEI scores.
“A large part of northeastern North America, as well as many mountain ranges across the globe, also show moderately high scores.”
Quote in the paperNot a substantial claim- The authors state this as an assumption: Areas with higher surface runoff play a prominent role in the amount of available water resources and are more vulnerable to disturbances.
- The authors state this as an assumption: A drop in soil moisture content after a fire is caused by greater inputs of radiative energy, which negatively impact surface runoff levels and amounts of water during the dry season.
- The authors state this as an assumption: Without vegetation interception and respiration, actual evapotranspiration will mainly be converted to runoff.
May combine two claims.
Findingown data§ 2.3. Sensitivity Analysis · p. 6The GWWEI is most strongly correlated with AET (0.76) and SM (0.74), moderately with SR (0.66) and NI (0.55), and weakly with AB (0.21), FD (0.11), and AI (0.06).
“GWWEI | GWWEI | 1.00 | 0.21 | 0.11 | 0.55 | 0.06 | 0.76 | 0.74 | 0.66”
Quote in the paperNot a substantial claimMay combine two claims.
Findingown data§ 3.2. Sensitivity of the GWWEI · p. 9Robust estimates of the GWWEI (lowest coefficient of variation values) are concentrated in the tropical savannas and the dry temperate steppes, except for the North American prairies, which show a wide range of variability, and northern Australia, which shows a constant high level in all individual indicator scores.
“Robust estimates of the GWWEI, i.e. , the lowest coefficient of variation values, are concentrated in the tropical savannas and the dry temperate steppes, except for the North American prairies, which show a wide range of variability, and for northern Australia, which shows a constant high level in all individual indicator scores.”
Quote in the paperNot a substantial claimMay combine two claims.
Findingnone given§ 4. Conclusions · p. 12The highest exposure scores were mostly clustered in the tropical wet forests, whereas intermediate scores tended to be localized in tropical dry forest and shrublands, as well as in several mountain ranges and boreal forests; the lowest levels were found in the tundra, temperate forests and temperate prairies.
“The highest exposure scores were mostly clustered in the tropical wet forests, whereas intermediate scores tended to be localized in tropical dry forest and shrublands, as well as in several mountain ranges and boreal forests. The lowest levels were found in the tundra, temperate forests and temperate prairies.”
Quote in the paperSubstantial claimMay combine two claims.
Premisecitation§ 1. Introduction · p. 1The water requirements of rapidly growing post-fire vegetation can subsequently limit water quantity, even though water quality may improve.
“The water requirements of rapidly growing post-fire vegetation can subsequently limit water quantity [4], even though water quality may improve [7].”
Quote in the paperNot a substantial claim0 of 2 sources checked- cites [4] Kuczera, 1987, Prediction of water yield reductions following a bushfire in ash-mixed species eucalypt forest, J. Hydrol. source
Not checked in the free run.
- cites [7] Dunnette, 2014, Biogeochemical impacts of wildfires over four millennia in a Rocky Mountain subalpine watershed, New Phytol. source
Not checked in the free run.
Probably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.
Premisecitation§ 1. Introduction · p. 2Several key global studies used this approach to underline issues in water security and riverine biodiversity, ocean vulnerability to human impact, and to identify natural areas of great importance for ecosystem functioning.
“Several key global studies used this approach to underline issues in water security and riverine biodiversity [20], ocean vulnerability to human impact [22] and to identify natural areas of great importance for ecosystem functioning [19].”
Quote in the paperNot a substantial claim0 of 3 sources checked- cites [20] McIntyre, 2010, Global threats to human water security and river biodiversity, Nature source
Not checked in the free run.
- cites [22] Halpern, 2008, A global map of human impact on marine ecosystems, Science source
Not checked in the free run.
- cites [19] Freudenberger, 2012, A global map of the functionality of terrestrial ecosystems, Ecol. Complex. source
Not checked in the free run.
Probably not a substantial claim: may not pass S3 (load-bearing).
Premisecitation§ 1. Introduction · p. 2Resource or risk indices are often created by aggregating proxy variables (indicators) known to play a role in the occurrence of the studied phenomenon.
“Often, resource or risk indices are created by aggregating proxy variables, called indicators, that are known to play a role in the occurrence of the studied phenomenon [19-22].”
Quote in the paperNot a substantial claim0 of 4 sources checked- cites [19] Freudenberger, 2012, A global map of the functionality of terrestrial ecosystems, Ecol. Complex. source
Not checked in the free run.
- cites [20] McIntyre, 2010, Global threats to human water security and river biodiversity, Nature source
Not checked in the free run.
- cites [21] Dickson, B., Blaney, R., Miles, L., Regan, E., van Soesbergen, A., Väänänen, E., Blyth, S., Harfoot, M., Martin, C.S., and McOwen, C. (2014). Towards a Global Map of Natural Capital: KEY Ecosystem Assets, United Nations Environment Program.
Not checked in the free run.
- cites [22] Halpern, 2008, A global map of human impact on marine ecosystems, Science source
Not checked in the free run.
May combine two claims.
Premisecitation§ 1. Introduction · p. 1Wildfires are essential to ecosystem function across the globe and influence a wide spectrum of ecosystem components and natural processes, including the hydrological cycle.
“Wildfires are essential to ecosystem function across the globe [1], influencing a wide spectrum of ecosystem components and natural processes [2], among which is the hydrological cycle.”
- Also stated in: § AGlobal Index for Mapping the Exposure of Water Resources to Wildfire · p. 1 · plain
“Wildfires are keystone components of natural disturbance regimes that maintain ecosystem structure and functions, such as the hydrological cycle, in many parts of the world.”
Quote in the paperSubstantial claim0 of 2 sources checked- cites [1] Bond, 2005, The global distribution of ecosystems in a world without fire, New Phytol. source
Not checked in the free run.
- cites [2] Lavorel, 2007, Vulnerability of land systems to fire: Interactions among humans, climate, the atmosphere, and ecosystems, Mitig. Adapt. Strateg. Glob. Chang. source
Not checked in the free run.
- Also stated in: § AGlobal Index for Mapping the Exposure of Water Resources to Wildfire · p. 1 · plain
Classified as probably not a substantial claim. May combine two claims.
Premisecitation§ 1. Introduction · p. 2In such an approach, raster datasets representing indicators are selected and normalized to assign each pixel a score, each indicator is assigned a weight according to its assumed importance, and numerous indicators are aggregated to create a final raster index.
“In such an approach, raster datasets representing indicators are selected and normalized to assign each pixel a score. Each indicator is then assigned a weight according to its assumed importance to the phenomenon of interest. Numerous indicators can then be aggregated to create a final raster index, whereby pixel values reflect the degree of risk or resource availability.”
Quote in the paperSubstantial claim0 of 4 sources checked- cites [19] Freudenberger, 2012, A global map of the functionality of terrestrial ecosystems, Ecol. Complex. source
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- cites [20] McIntyre, 2010, Global threats to human water security and river biodiversity, Nature source
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- cites [21] Dickson, B., Blaney, R., Miles, L., Regan, E., van Soesbergen, A., Väänänen, E., Blyth, S., Harfoot, M., Martin, C.S., and McOwen, C. (2014). Towards a Global Map of Natural Capital: KEY Ecosystem Assets, United Nations Environment Program.
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- cites [22] Halpern, 2008, A global map of human impact on marine ecosystems, Science source
Not checked in the free run.
May combine two claims.
Premisecitation§ 1. Introduction · p. 1Vegetation cover, litter and soil organic matter can be dramatically reduced by large fires, leading to higher surface runoff and soil erosion, increasing water quantity but decreasing water quality.
“Vegetation cover, litter and soil organic matter can be dramatically reduced by large fires and can lead to higher surface runoff and soil erosion, increasing water quantity, but decreasing water quality.”
Quote in the paperSubstantial claim0 of 4 sources checked- cites [3] USDA (2005). Wildland Fire in Ecosystems: Effects of Fire on Soil and Water, Gen. Tech. Rep. RMRS-GTR-42-vol.4. Ogden.
Not checked in the free run.
- cites [4] Kuczera, 1987, Prediction of water yield reductions following a bushfire in ash-mixed species eucalypt forest, J. Hydrol. source
Not checked in the free run.
- cites [5] DeBano, 2000, The role of fire and soil heating on water repellency in wildland environments: A review, J. Hydrol. source
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- cites [6] Seibert, 2010, Effects of wildfire on catchment runoff response: A modelling approach to detect changes in snow-dominated forested catchments, Hydrol. Res. source
Not checked in the free run.
Probably not a substantial claim: may not pass S3 (load-bearing), S4 (based). May combine two claims.
Premisenone given§ 2.1. Data Selection and Indicators' Definition · p. 4If natural surface runoff increases when vegetation cover is reduced, it becomes more difficult to predict and can lead to greater erosion levels and floods.
“That said, if natural SR increases when vegetation cover is reduced, it becomes more difficult to predict and can lead to greater erosion levels and floods.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S1 (asserted). May combine two claims.
Premisecitation§ 2.1. Data Selection and Indicators' Definition · p. 4A recent study argues that human influence tends to decrease fire activity at the global scale and, consequently, the area burned.
“Nonetheless, a recent study argues that human influence tends to decrease fire activity at the global scale [16] and, consequently, the area burned.”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites [16] Knorr, 2014, Impact of human population density on fire frequency at the global scale, Biogeosciences source
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Probably not a substantial claim: may not pass S2 (checkable).
Interpretationreasoning§ 3.3. The GWWEI and Its Implications for Water Resource Protection · p. 11The GWWEI, as part of a larger WWR framework, can contribute to knowledge improvement, especially in mountainous areas known as 'water towers'.
“The GWWEI, as a part of a larger WWR framework, can contribute to knowledge improvement, especially in mountainous areas, known as 'water towers', across the globe.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
Study design and conductreasoning§ 3.1. Geography of the GWWEI · p. 8Indicators are global-scale proxies that may not be suitable when estimating fire risk or water discharge across small areas.
“It is important to note that indicators are global-scale proxies that may not be suitable when estimating fire risk or water discharge across small areas.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
Study design and conductnone given§ 2.3. Sensitivity Analysis · p. 6The Spearman correlation coefficient table was generated as a measure of dependency, such that indicators highly correlated with the final index have an overall higher influence on final index scores.
“The Spearman correlation coefficient table was generated as a measure of dependency, such that indicators highly correlated with the final index have an overall higher influence on final index scores.”
Quote in the paperNot a substantial claimClassified as probably not a substantial claim. May combine two claims.
Study design and conductnone given§ 3.1. Geography of the GWWEI · p. 8The GWWEI does not describe a quantitative likelihood or probability of impacts on water resources; it depicts the geographic overlay of important drivers of the WWR and identifies areas where quantitative assessments must be carried out.
“At this stage of our framework development, it is important to recall that the GWWEI does not describe a quantitative likelihood or probability of impacts on water resources. It rather depicts the geographic overlay of important drivers of the WWR and identifies areas where such quantitative assessments must be carried out.”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.
Premisecitation§ 3.3. The GWWEI and Its Implications for Water Resource Protection · p. 11Moody and Martin [11] showed the critical exposure of mountainous reservoirs to wildfire impacts, although limited to the western U.S.
“Moody and Martin [11] showed the critical exposure of mountainous reservoirs to wildfire impacts, although limited to the western U.S.”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Moody and Martin [11] Moody, J.A., and Martin, D.A. (2004, January 18–21). Wildfire impacts on reservoir sedimentation in the western United States. Proceedings of the Ninth International Symposium on River Sedimentation, Yichang, China.
Not checked in the free run.
May combine two claims.
Premisecitation§ 2.1. Data Selection and Indicators' Definition · p. 4High levels of soil moisture favor runoff and water availability, but soil moisture is also sensitive to post-fire changes in vegetation cover.
“Although high levels of SM favor runoff and water availability, it is also sensitive to post-fire changes in vegetation cover [39].”
Quote in the paperSubstantial claim0 of 1 sources checked- cites [39] Kasischke, 2007, Assessing spatial and temporal variations in surface soil moisture in fire-disturbed black spruce forests in Interior Alaska using spaceborne synthetic aperture radar imagery—Implications for post-fire tree recruitment, Remote Sens. Environ. source
Not checked in the free run.
Probably not a substantial claim: may not pass S2 (checkable), S3 (load-bearing). May combine two claims.
Study design and conductreasoning§ 3.1. Geography of the GWWEI · p. 8Working at the global scale usually smooths regional differences, so GWWEI scores should be interpreted according to specific environmental, socio-cultural and economic factors.
“Working at the global scale usually smooths regional differences, and in this regard, the scores should be interpreted according to specific environmental, socio-cultural and economic factors.”
Quote in the paperNot a substantial claimMay combine two claims.
Study design and conductreasoning§ 2.2. Data Processing and Aggregation · p. 5The study used the FWI layer as an extraction mask for other layers, thereby avoiding result biases by including arid areas where climatic conditions restrain water availability, vegetation growth and wildfire activity.
“We used the FWI layer, which does not account for desert areas, as an extraction mask for other layers. Therefore, we avoided result biases by including arid areas where climatic conditions restrain water availability, as well as vegetation growth and, consequently, wildfire activity.”
Quote in the paperSubstantial claimClassified as probably not a substantial claim. May combine two claims.
Study design and conductnone given§ 2.1. Data Selection and Indicators' Definition · p. 4The FD indicator, based on the final FWI, provides information about the potential for fire activity, but does not account for actual area burned, vegetation composition or human influence on fire activity.
“Our FD indicator, based on the final FWI, provides information about the potential for fire activity, but does not account for actual area burned, vegetation composition or human influence on fire activity.”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.
Premisecitation§ 2.1. Data Selection and Indicators' Definition · p. 4The anthropogenic influence on fire activity is well known but still a matter of debate, as the nature of this influence is complicated.
“The anthropogenic influence (AI) on fire activity is well known, but is still a matter of debate, as the nature of this influence is complicated [33-35].”
Quote in the paperNot a substantial claim0 of 3 sources checked- cites [33] Aldersley, 2011, Global and regional analysis of climate and human drivers of wildfire, Sci. Total Environ. source
Not checked in the free run.
- cites [34] Bistinas, 2013, Relationships between human population density and burned area at continental and global scales, PLoS ONE source
Not checked in the free run.
- cites [35] Archibald, 2013, Defining pyromes and global syndromes of fire regimes, Proc. Natl. Acad. Sci. USA source
Not checked in the free run.
Probably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.
Study design and conductnone given§ 3.2. Sensitivity of the GWWEI · p. 9Nonlinear relationships and interactions might exist but are not explored with the simple correlation coefficients used.
“Although several nonlinear relationships and interactions might exist, they are not explored with these simple correlation coefficients.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S4 (based).
Interpretationnone given§ 2.1. Data Selection and Indicators' Definition · p. 4Post-fire conversion of AET to runoff would be limited by expected increases in post-fire soil-water evaporation.
“This process would be limited, however, by expected increases in post-fire soil-water evaporation.”
Quote in the paperNot a substantial claim- The authors state this as an assumption: Without vegetation interception and respiration, actual evapotranspiration will mainly be converted to runoff.
May combine two claims.
Study design and conductreasoning§ 2.1. Data Selection and Indicators' Definition · p. 2The data used have some discrepancies in their time period, but they are the product of large-scale long-term monitoring, which substantially smooths spatial and temporal variability, making them suitable for use in a global model.
“Although our data have some discrepancies in their time period, they are the product of large-scale long-term monitoring, which substantially smooths spatial and temporal variability, making them suitable for use in a global model.”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S2 (checkable), S3 (load-bearing).
Premisecitation§ 2.3. Sensitivity Analysis · p. 6It is critical in indexation models to test the robustness of the aggregated index to evaluate the level of confidence in the final score.
“It is critical in indexation models to test the robustness of the aggregated index to evaluate the level of confidence in the final score [48].”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites [48] OECD (2008). Handbook on Constructing Composite Indicators, European Comission.
Not checked in the free run.
Probably not a substantial claim: may not pass S4 (based).
Interpretationnone given§ 3.3. The GWWEI and Its Implications for Water Resource Protection · p. 11Wildfires are rarely considered as a critical threat to water resources by international authorities.
“Surprisingly, wildfires are rarely considered as a critical threat to water resources by international authorities.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
Premisecitation§ 3.3. The GWWEI and Its Implications for Water Resource Protection · p. 11Mori and Johnson [58] demonstrated that mountains might experience significant changes in their fire regime because of climate change.
“Mori and Johnson [58], for instance, demonstrated that mountains might experience significant changes in their fire regime because of climate change”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Mori and Johnson [58] Mori, 2013, Assessing possible shifts in wildfire regimes under a changing climate in mountainous landscapes, For. Ecol. Manag. source
Not checked in the free run.
Classified as probably not a substantial claim.
Study design and conductreasoning§ 2.1. Data Selection and Indicators' Definition · p. 4The NI indicator considers that a higher lightning flash rate is associated with a higher chance for lightning to reach the ground, potentially starting a fire when the strike occurs in a vegetated area.
“We build our NI indicator considering that a higher lightning flash rate is associated with a higher chance for lightning to reach the ground, potentially starting a fire when the strike occurs in a vegetated area.”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S2 (checkable). May combine two claims.
Study design and conductreasoning§ 2.1. Data Selection and Indicators' Definition · p. 2Slight temporal mismatches may be responsible for some inaccuracies, but these would be relatively minor.
“Although slight temporal mismatches may be responsible for some inaccuracies, there is reason to believe that these would be relatively minor.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
Study design and conductreasoning§ 2.1. Data Selection and Indicators' Definition · p. 4Lightning activity should not be considered as an actual fire ignition product because it does not account for individual strikes.
“As it does not account for individual strikes, lightning activity should not be considered as an actual fire ignition product.”
Quote in the paperNot a substantial claimMay combine two claims.
Study design and conductcitation§ 2.1. Data Selection and Indicators' Definition · p. 4HFP scores are scaled per biome and encompass different socio-environmental configurations, which have different effects on fire activity across the globe.
“However, scores are scaled per biome and, thus, encompass different socio-environmental configurations, which, in turn, have different effects on fire activity across the globe [35].”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites [35] Archibald, 2013, Defining pyromes and global syndromes of fire regimes, Proc. Natl. Acad. Sci. USA source
Not checked in the free run.
Probably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.
Premisecitation§ 3.3. The GWWEI and Its Implications for Water Resource Protection · p. 11Nogués-Bravo et al. [57] pointed out the extreme sensitivity of headwaters to natural hazards in the context of climate change, though wildfire was not considered.
“Nogués-Bravo et al. [57] pointed out the extreme sensitivity of headwaters to natural hazards in the context of climate change, though wildfire was not considered.”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Nogués-Bravo et al. [57]
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May combine two claims.
Premisecitation§ 2.1. Data Selection and Indicators' Definition · p. 4In many places, lightning activity is an important factor of fire ignition that can lead to a large area burned when it occurs in remote areas.
“In many places of the world, lightning activity is an important factor of fire ignition [23] that can lead to a large area burned when it occurs in remote areas [29-31].”
Quote in the paperNot a substantial claim0 of 4 sources checked- cites [23] Krawchuk, 2009, Global pyrogeography: The current and future distribution of wildfire, PLoS ONE source
Not checked in the free run.
- cites [29] Stocks, 2002, Large forest fires in Canada, 1959–1997, J. Geophys. Res.
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- cites [30] Bond, 2005, Fire as a global “herbivore”: The ecology and evolution of flammable ecosystems, Trends Ecol. Evol. source
Not checked in the free run.
- cites [31] Pivello, 2000, Lightning fires in a Brazilian Savanna National Park: Rethinking management strategies, Environ. Manag. source
Not checked in the free run.
May combine two claims.
Premisecitation§ 2.1. Data Selection and Indicators' Definition · p. 3Area burned has been found to be a good global proxy for fire activity, especially as fire size is an important factor of post-fire impact to water resources.
“Area burned (AB) has been found to be a good global proxy for fire activity [23], especially as fire size is an important factor of post-fire impact to water resources [3].”
Quote in the paperSubstantial claim0 of 2 sources checked- cites [23] Krawchuk, 2009, Global pyrogeography: The current and future distribution of wildfire, PLoS ONE source
Not checked in the free run.
- cites [3] USDA (2005). Wildland Fire in Ecosystems: Effects of Fire on Soil and Water, Gen. Tech. Rep. RMRS-GTR-42-vol.4. Ogden.
Not checked in the free run.
Probably not a substantial claim: may not pass S3 (load-bearing).
Premisecitation§ 2.2. Data Processing and Aggregation · p. 5The method is inspired by Freudenberger et al. [19].
“This method is inspired by the work of Freudenberger et al. [19].”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites [19] Freudenberger, 2012, A global map of the functionality of terrestrial ecosystems, Ecol. Complex. source
Not checked in the free run.
Classified as probably not a substantial claim. May combine two claims.
Study design and conductreasoning§ 2.2. Data Processing and Aggregation · p. 5The weighting scheme assigns 50% to fire indicators and 50% to water indicators and equally partitions weights within each group, resulting in a theoretical pixel score range of 0 to 100, with higher scores meaning higher concentration of exposure factors.
“Our weighting scheme assigns 50% to fire indicators and 50% to water indicators and equally partitions the weights within each of these groups. Therefore, we assigned a 16.6% weight to each water indicator (3) and a 12.5% weight to each fire indicator (4). As a result, one pixel's final score in the index theoretically ranges from 0 to 100, a higher score meaning a higher concentration of exposure”
Quote in the paperSubstantial claim0 of 1 sources checked- cites [19] Freudenberger, 2012, A global map of the functionality of terrestrial ecosystems, Ecol. Complex. source
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Probably not a substantial claim: may not pass S2 (checkable). May combine two claims.
Premisecitation§ 2.1. Data Selection and Indicators' Definition · p. 3Fire danger is a measure of the potential for a fire to ignite and spread across the landscape and is critical to assess water resources exposure.
“Fire danger (FD) is a measure of the potential for a fire to ignite and spread across the landscape and therefore is critical to assess water resources exposure.”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites [26] Canadian Forestry Servic (1987). Development and Structure of the Canadian Forest Fire Weather Index System.
Not checked in the free run.
Classified as probably not a substantial claim. May combine two claims.
Premisecitation§ 2.1. Data Selection and Indicators' Definition · p. 3An increasing FWI value means lower fuel moisture, higher wind speed and greater fire danger.
“An increasing index value means lower fuel moisture, higher wind speed and, consequently, a greater fire danger.”
Quote in the paperSubstantial claim0 of 1 sources checked- cites [26] Canadian Forestry Servic (1987). Development and Structure of the Canadian Forest Fire Weather Index System.
Not checked in the free run.
Probably not a substantial claim: may not pass S3 (load-bearing).
Premisecitation§ 3.3. The GWWEI and Its Implications for Water Resource Protection · p. 11Viviroli et al. [56] showed that several mountainous regions provide at least a 'supportive' amount of water for downstream supply needs.
“Viviroli et al. [56] indeed showed that several mountainous regions provide at least a 'supportive' amount of water for downstream supply needs”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Viviroli et al. [56] Viviroli, 2007, Mountains of the world, water towers for humanity: Typology, mapping, and global significance, Water Resour. Res. source
Not checked in the free run.
May combine two claims.
Interpretationcitation§ 3.1. Geography of the GWWEI · p. 8High GWWEI scores in African savannas are mostly driven by area burned, as those ecosystems experience most of the fire activity on Earth.
“For instance, high scores in African savannas are mostly driven by the AB, as those ecosystems experience most of fire activity on Earth [24]”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites [24] Giglio, 2013, Analysis of daily, monthly, and annual burned area using the fourth-generation global fire emissions database (GFED4), J. Geophys. Res. Biogeosci. source
Not checked in the free run.
Probably not a substantial claim: may not pass S2 (checkable), S4 (based).
Interpretationreasoning§ 4. Conclusions · p. 12This framework adds an important component to the global water security paradigm in the context of climate change that do not presently encompass global wildfire water risk.
“This framework adds an important component to the global water security paradigm in the context of climate change that do not presently encompass global wildfire water risk.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S3 (load-bearing), S4 (based).
Interpretationreasoning§ 3.4. Limitations and Improvements · p. 12The Build-Up Index of the FWI System may be a better proxy to fire impacts than FWI, because it better reflects burn severity, a critical determinant of post-fire hydrological effects.
“Similarly, the Build-Up Index of the FWI System may be a better proxy to fire impacts than FWI, because it better reflects burn severity, a critical determinant of post-fire hydrological effects.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
Premisecitation§ 3.4. Limitations and Improvements · p. 12The step of surveying scientists to obtain a robust rating of the score for each indicator has been previously used in several studies describing the creation of risk and resource indices.
“This step has been previously used in several studies describing the creation of risk and resource indices [20,22,59].”
Quote in the paperNot a substantial claim0 of 3 sources checked- cites [20] McIntyre, 2010, Global threats to human water security and river biodiversity, Nature source
Not checked in the free run.
- cites [22] Halpern, 2008, A global map of human impact on marine ecosystems, Science source
Not checked in the free run.
- cites [59] Green, 2015, Freshwater ecosystem services supporting humans: Pivoting from water crisis to water solutions, Glob. Environ. Chang. source
Not checked in the free run.
Probably not a substantial claim: may not pass S2 (checkable).
Interpretationcitation§ 3.3. The GWWEI and Its Implications for Water Resource Protection · p. 11The WWR should be viewed primarily as a source of cumulative effects on water resources whose watersheds are exposed, if not already impacted, by forest degradation and human activities.
“We argue that the WWR should be viewed primarily as a source of cumulative effects on water resources whose watersheds are exposed, if not already impacted, by forest degradation and human activities [63].”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites [63] Millar, 2015, Temperate forest health in an era of emerging megadisturbance, Science source
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Probably not a substantial claim: may not pass S3 (load-bearing).
Interpretationown data§ 3.4. Limitations and Improvements · p. 12The variability in the spatial pattern of the index shows that different weighting schemes could improve its robustness.
“the variability in the spatial pattern of the index shows that different weighting schemes could improve its robustness.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S2 (checkable).
Interpretationreasoning§ 4. Conclusions · p. 12The global index presented in this study can help pinpoint regions of potential concern that may require a more detailed assessment of wildfire-induced risk to water resources.
“The global index presented in this study can help us pinpoint regions of potential concern that may require a more detailed assessment of wildfire-induced risk to water resources.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S2 (checkable), S3 (load-bearing), S4 (based).
Interpretationnone given§ 3.4. Limitations and Improvements · p. 12Resulting estimates of GWWEI could be improved if indicator data were averaged for biome-specific fire seasons, rather than annually.
“Moreover, resulting estimates of GWWEI could be improved if indicator data were averaged for biome-specific fire seasons, rather than annually.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
Study design and conductnone given§ 3.4. Limitations and Improvements · p. 12The current version of the framework only considers overlapping additive effects mostly based on long-term indicator averages.
“Our current version of the framework only considers overlapping additive effects mostly based on long-term indicator averages.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S2 (checkable), S4 (based).
Interpretationnone given§ 4. Conclusions · p. 12High exposure levels may reveal the potential for deleterious impacts on water quality and downstream cumulative effects that might in turn affect local to regional water security, especially in river basins serving large populations.
“Indeed, high exposure levels may reveal the potential for deleterious impacts on water quality and downstream cumulative effects that might in turn affect local to regional water security, especially in river basins serving large populations.”
Quote in the paperNot a substantial claim- Rests on an assumption: Fire activity can increase the net quantity of water downstream.
- Rests on an assumption: Potentially severe impacts on water quality and timing/magnitude of event flows (i.e., floods) can impact a wide range of ecological and human water resource uses (i.e., drinking water).
Probably not a substantial claim: may not pass S2 (checkable), S4 (based).
Interpretationnone given§ 4. Conclusions · p. 12The definition of a WWR opens new perspectives in the understanding of the global water and land systems.
“In this regard, the definition of a WWR opens new perspectives in the understanding of the global water and land systems.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
Interpretationreasoning§ 3.4. Limitations and Improvements · p. 12Extending the WWR framework to take into account the induced risk to the downstream water supply implies the integration of a 'spatial transmission' process.
“Extending the WWR framework to take into account the induced risk to the downstream water supply implies the integration of a 'spatial transmission' process”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S2 (checkable), S3 (load-bearing).
Interpretationreasoning§ 3.4. Limitations and Improvements · p. 12Improvement of the index depends on the creation of and enhancements to global datasets, especially regarding water-related indicators.
“It is important to underline that we were dependent on data availability; the improvement of our index will therefore depend on the creation of and enhancements to global datasets, especially regarding water-related indicators, given that several wildfire indicators already exist.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S2 (checkable).
Interpretationown data§ 4. Conclusions · p. 12The overwhelming influence of water resource indicators indicates the need for several modifications in the weighting scheme, such as incorporating expert opinion or including a larger set of variables.
“Notably, the sensitivity analysis showed an overwhelming influence of water resource indicators on the final index scores, which indicates the need for several modifications in the weighting scheme, such as incorporating expert opinion or including a larger set of variables.”
Quote in the paperNot a substantial claim
The authors state this as an assumption.
Areas with higher surface runoff play a prominent role in the amount of available water resources and are more vulnerable to disturbances.
“For this study, our indicator assumes that areas showing higher levels of SR play a prominent role in the amount of available water resources and are thus more vulnerable to disturbances.”
The authors state this as an assumption.
A drop in soil moisture content after a fire is caused by greater inputs of radiative energy, which negatively impact surface runoff levels and amounts of water during the dry season.
“Our indicator assumes that a drop in soil moisture content after a fire is caused by greater inputs of radiative energy [43], which, in turn, negatively impact SR levels and amounts of water during the dry season.”
The authors state this as an assumption.
Without vegetation interception and respiration, actual evapotranspiration will mainly be converted to runoff.
“Our indicator is used as a proxy for post-fire water-balance change, based on the reasonable assumption that without vegetation interception and respiration, AET will mainly be converted to runoff.”
The authors state this as an assumption.
The strong pattern shown by water indicators may mask information contained in fire indicators, thus showing lower levels of correlation in them.
“We assume that the strong pattern shown by water indicators may mask information contained in fire indicators, thus showing lower levels of correlation in them.”
The authors state this as an assumption.
Equal weight is used in the aggregation process of the GWWEI.
“This raises a question about the assumption of equal weight used in the aggregation process. While we considered this assumption acceptable to create our framework”
The paper relies on this without support.
Fire activity can increase the net quantity of water downstream.
“Although fire activity can increase the net quantity of water downstream”
The paper relies on this without support.
Potentially severe impacts on water quality and timing/magnitude of event flows (i.e., floods) can impact a wide range of ecological and human water resource uses (i.e., drinking water).
“potentially severe impacts on water quality and timing/magnitude of event flows ( i.e. , floods) can impact a wide range of ecological and human water resource uses ( i.e. , drinking water).”
The paper relies on this without support.
Wildfires can impair water provision services from ecosystems.
“Although wildfires can impair water provision services from ecosystems”
The paper relies on this without support.
Wildfires are a natural and essential ecosystem process.
“they are a natural and essential ecosystem process.”
Claims other papers make about this one
Each is checked against this paper’s own text: does it say what the citing paper says it does?
Recent studies have focused on determining the sensitivity to post-fire contamination and range from relatively simple spatial indices to more complex assessments based on the probability of occurrence of both fire and post-fire contamination events.
“Recent studies have focused on determining the sensitivity to post-fire contamination and range from relatively simple spatial indices (e.g., Robinne et al., 2016 at the global scale) to more complex assessments based on the probability of occurrence of both fire and the post-fire contamination events (Langhans et al., 2016;Santos et al., 2015a;Thompson et al., 2013).”
From Assessing water contamination risk from vegetation fires: Challenges, opportunities and a framework for progress (2018) · cites this paper as Robinne et al., 2016
Self-check
Percentages, sums and reported differences re-computed from the paper’s own numbers.
Each contradiction between two passages listed here was confirmed by an independent check.
SM is attributed to the wrong stepwise map
MinorThe text cites Figure 4c for SM's effect, but the caption shows no SM in 4c. SM first appears in 4e.
“with SM being critical in setting the pattern for mountain ranges, such as the Himalayas or Southern Alaska, as well as increasing scores for the southern fringe of the boreal forest (Figure 4c).”
“( c ) AB + SR + NI + AET; ( d ) AB + SR + NI + AET + AI; ( e ) AB + SR + NI + AET + AI + SM”
Jackknifing count conflicts with the number of indicators
MinorRemoving each of seven indicators once produces seven modified indices, not eight. The stated total of 51 modified indices also uses seven jackknife indices: 7 + 2 + 14 + 28 = 51.
“jackknifing produced eight modified indices; in other words, one for each missing indicator.”
“As this process removes our seven indicators successively to create a new index each time”
Fire-danger dataset has conflicting end years
MinorTable 1 lists fire-danger coverage through 2014, but the dataset description says it was compiled through 2012.
“Fire Danger (FD) | of datasets used to NASA | develop the GWWEI indicators. unitless | NASA: National Aeronautic 0.5 2/3 | 1980-2014”
“compiled for 1980-2012 at a resolution of 0.5 latitude 2/3 longitude”
Anthropogenic-influence dataset has conflicting coverage years
MinorTable 1 gives 1960-2004 for anthropogenic influence, whereas its description says the Human Footprint Index data were computed from 1995 to 2004.
“Anthropogenic Influence (AI) SEDAC Unitless (0-100) 0.08° 1960-2004”
“we used the Human Footprint Index (HFP) V2 data from the Socioeconomic Data and Applications Center from NASA, computed from 1995 to 2004”
Area-burned dataset has conflicting coverage years
MinorTable 1 lists 1997-2013 for area burned, while the accompanying description says the data span 1995-2014.
“inaccuracies, there Area Burned (AB) | is reason to believe that Giglio et al. | these would be relatively Ha/month | minor. 0.25 | 1997-2013”
“Data span 1995-2014, and are spatially aggregated at a 0.25 pixel resolution [24,25].”
AET is attributed to the wrong stepwise map
MinorThe text says Figure 4a shows the inclusion of AET, but the figure caption identifies 4a as AB + SR; AET first appears in 4c.
“the inclusion of AET in the simplest version of the index (Figure 4a)”
“( a ) AB + SR; ( b ) AB + SR + NI; ( c ) AB + SR + NI + AET”
Cites
Terrestrial ecoregions of the world: a new map of life on Earth
Olson, D. M., Dinerstein, E., Wikramanayake, E. D., Burgess, N. D., Powell, G. V. N., Underwood, E. C., D'amico, J. A., Itoua, I., Strand, H. E., Morrison, J. C., et al. (2001) · BioScience · doi:10.1641/0006-3568(2001)051[0933:teotwa]2.0.co;2 · Cited by 8,488 · see citing works
Global threats to human water security and river biodiversity
Vörösmarty, C. J., McIntyre, P. B., Gessner, M. O., Dudgeon, D., Prusevich, A., Green, P., Glidden, S., Bunn, S. E., Sullivan, C. A., Liermann, C. R., et al. (2010) · Nature · doi:10.1038/nature09440 · Cited by 7,582 · see citing works
A global map of human impact on marine ecosystems
Halpern, B. S., Walbridge, S., Selkoe, K. A., Kappel, C. V., Micheli, F., D'Agrosa, C., Bruno, J. F., Casey, K. S., Ebert, C., Fox, H. E., et al. (2008) · Science · doi:10.1126/science.1149345 · Cited by 6,627 · see citing works
Global hydrological cycles and world water resources
Oki, T., & Kanae, S. (2006) · Science · doi:10.1126/science.1128845 · Cited by 4,392 · see citing works
Bowman, D. M. J. S., Balch, J. K., Artaxo, P., Bond, W. J., Carlson, J. M., Cochrane, M. A., D’Antonio, C. M., DeFries, R. S., Doyle, J. C., Harrison, S. P., et al. (2009) · Science · doi:10.1126/science.1163886 · Cited by 3,351 · see citing works
Fire as a global ‘herbivore’: the ecology and evolution of flammable ecosystems
BOND, W., & KEELEY, J. (2005) · Trends in Ecology & Evolution · doi:10.1016/j.tree.2005.04.025 · Cited by 2,484 · see citing works
The Human Footprint and the Last of the Wild
Sanderson, E. W., Jaiteh, M., Levy, M. A., Redford, K. H., Wannebo, A., & Woolmer, G. (2002) · BioScience · doi:10.1641/0006-3568(2002)052[0891:thfatl]2.0.co;2 · Cited by 2,472 · see citing works
The global distribution of ecosystems in a world without fire
Bond, W. J., Woodward, F. I., & Midgley, G. F. (2005) · New Phytologist · doi:10.1111/j.1469-8137.2004.01252.x · Cited by 1,942 · see citing works
Giglio, L., Randerson, J. T., & van der Werf, G. R. (2013) · Journal of Geophysical Research: Biogeosciences · doi:10.1002/jgrg.20042 · Cited by 1,605 · see citing works
Mean seasonal and spatial variability in gauge‐corrected, global precipitation
Legates, D. R., & Willmott, C. J. (1990) · International Journal of Climatology · doi:10.1002/joc.3370100202 · Cited by 1,512 · see citing works
Human Appropriation of Renewable Fresh Water
Postel, S. L., Daily, G. C., & Ehrlich, P. R. (1996) · Science · doi:10.1126/science.271.5250.785 · Cited by 1,477 · see citing works
Mountains of the world, water towers for humanity: Typology, mapping, and global significance
Viviroli, D., Dürr, H. H., Messerli, B., Meybeck, M., & Weingartner, R. (2007) · Water Resources Research · doi:10.1029/2006wr005653 · Cited by 1,376 · see citing works
Assessing objective techniques for gauge‐based analyses of global daily precipitation
Chen, M., Shi, W., Xie, P., Silva, V. B. S., Kousky, V. E., Higgins, R. W., & Janowiak, J. E. (2008) · Journal of Geophysical Research Atmospheres · doi:10.1029/2007jd009132 · Cited by 1,253 · see citing works
The role of fire and soil heating on water repellency in wildland environments: a review
DeBano, L. F. (2000) · Journal of Hydrology · doi:10.1016/s0022-1694(00)00194-3 · Cited by 1,244 · see citing works
Global Pyrogeography: the Current and Future Distribution of Wildfire
Krawchuk, M. A., Moritz, M. A., Parisien, M.-A., Van Dorn, J., & Hayhoe, K. (2009) · PLoS ONE · doi:10.1371/journal.pone.0005102 · Cited by 1,000 · see citing works
Self-citationLarge forest fires in Canada, 1959–1997
Stocks, B. J., Mason, J. A., Todd, J. B., Bosch, E. M., Wotton, B. M., Amiro, B. D., Flannigan, M., Hirsch, K. G., Logan, K. A., Martell, D. L., et al. (2002) · Journal of Geophysical Research Atmospheres · doi:10.1029/2001jd000484 · Cited by 970 · see citing works
Self-citationTemperate forest health in an era of emerging megadisturbance
Millar, C. I., & Stephenson, N. L. (2015) · Science · doi:10.1126/science.aaa9933 · Cited by 968 · see citing works
Future long-term changes in global water resources driven by socio-economic and climatic changes
Alcamo, J., Flörke, M., & Maerker, M. (2007) · Hydrological Sciences Journal · doi:10.1623/hysj.52.2.247 · Cited by 966 · see citing works
Climate change and disruptions to global fire activity
Moritz, M. A., Parisien, M.-A., Batllori, E., Krawchuk, M. A., Van Dorn, J., Ganz, D. J., & Hayhoe, K. (2012) · Ecosphere · doi:10.1890/es11-00345.1 · Cited by 959 · see citing works
Self-citationDefining pyromes and global syndromes of fire regimes
Archibald, S., Lehmann, C. E. R., Gómez-Dans, J. L., & Bradstock, R. A. (2013) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1211466110 · Cited by 845 · see citing works
Development and Structure of the Canadian Forest FireWeather Index System
Wagner, C. E. V., Forest, P., Station, E., Ontario, C. R., Fran�ais, R. U. E., & Davis, H. J. (1987) · Cited by 830 · see citing works
Water on an urban planet: Urbanization and the reach of urban water infrastructure
McDonald, R. I., Weber, K., Padowski, J., Flörke, M., Schneider, C., Green, P. A., Gleeson, T., Eckman, S., Lehner, B., Balk, D., et al. (2014) · Global Environmental Change · doi:10.1016/j.gloenvcha.2014.04.022 · Cited by 786 · see citing works
Fekete, B. M., Vörösmarty, C. J., & Grabs, W. (2002) · Global Biogeochemical Cycles · doi:10.1029/1999gb001254 · Cited by 742 · see citing works
Exposure of global mountain systems to climate warming during the 21st Century
Nogués‐Bravo, D., Araújo, M. B., Abad, M. P. E., & Martínez-Rica, J. P. (2007) · Global Environmental Change · doi:10.1016/j.gloenvcha.2006.11.007 · Cited by 711 · see citing works
Gridded lightning climatology from TRMM-LIS and OTD: Dataset description
Cecil, D. J., Buechler, D. E., & Blakeslee, R. J. (2012) · Atmospheric Research · doi:10.1016/j.atmosres.2012.06.028 · Cited by 698 · see citing works
An active-fire based burned area mapping algorithm for the MODIS sensor
Giglio, L., Loboda, T., Roy, D., Quayle, B., & Justice, C. (2009) · Remote Sensing of Environment · doi:10.1016/j.rse.2008.10.006 · Cited by 671 · see citing works
Mean seasonal and spatial variability in global surface air temperature
Legates, D. R., & Willmott, C. J. (1990) · Theoretical and Applied Climatology · doi:10.1007/bf00866198 · Cited by 633 · see citing works
Assessing global exposure and vulnerability towards natural hazards: the Disaster Risk Index
Peduzzi, P., Dao, H., Herold, C., & Mouton, F. (2009) · Natural hazards and earth system sciences · doi:10.5194/nhess-9-1149-2009 · Cited by 555 · see citing works
Lightning Fires in a Brazilian Savanna National Park: Rethinking Management Strategies
Neto, M. B. R., & Pivello, V. R. (2000) · Environmental Management · doi:10.1007/s002670010124 · Cited by 389 · see citing works
Emelko, M. B., Silins, U., Bladon, K. D., & Stone, M. (2011) · Water Research · doi:10.1016/j.watres.2010.08.051 · Cited by 357 · see citing works
Self-citationWildfire and the Future of Water Supply
Bladon, K. D., Emelko, M. B., Silins, U., & Stone, M. (2014) · Environmental Science & Technology · doi:10.1021/es500130g · Cited by 354 · see citing works
Self-citationGeospatial Indicators of Emerging Water Stress: An Application to Africa
Vörösmarty, C. J., Douglas, E., Green, P., & Revenga, C. (2005) · AMBIO · doi:10.1579/0044-7447-34.3.230 · Cited by 336 · see citing works
Global and regional analysis of climate and human drivers of wildfire
Aldersley, A., Murray, S. J., & Cornell, S. E. (2011) · Science of The Total Environment · doi:10.1016/j.scitotenv.2011.05.032 · Cited by 311 · see citing works
Prediction of water yield reductions following a bushfire in ash-mixed species eucalypt forest
Kuczera, G. A. (1987) · Journal of Hydrology · doi:10.1016/0022-1694(87)90054-0 · Cited by 280 · see citing works
A review of recent advances in risk analysis for wildfire management
Miller, C., & Ager, A. A. (2013) · International Journal of Wildland Fire · doi:10.1071/wf11114 · Cited by 277 · see citing works
Self-citationGlobal water resources modeling with an integrated model of the social-economic-environmental system
Davies, E. G. R., & Simonovic, S. P. (2011) · Advances in Water Resources · doi:10.1016/j.advwatres.2011.02.010 · Cited by 262 · see citing works
Lavorel, S., Flannigan, M. D., Lambin, E. F., & Scholes, M. C. (2006) · Mitigation and Adaptation Strategies for Global Change · doi:10.1007/s11027-006-9046-5 · Cited by 220 · see citing works
Self-citationFreshwater ecosystem services supporting humans: Pivoting from water crisis to water solutions
Green, P., Vörösmarty, C., Harrison, I., Farrell, T., Sáenz, L., & Fekete, B. (2015) · Global Environmental Change · doi:10.1016/j.gloenvcha.2015.06.007 · Cited by 193 · see citing works
Present and future water requirements for feeding humanity
Falkenmark, M., Rockström, J., & Karlberg, L. (2009) · Food Security · doi:10.1007/s12571-008-0003-x · Cited by 192 · see citing works
Impact of human population density on fire frequency at the global scale
Knorr, W., Kaminski, T., Arneth, A., & Weber, U. (2014) · Biogeosciences · doi:10.5194/bg-11-1085-2014 · Cited by 189 · see citing works
Effects of Urbanization on Organic Carbon Loads in the Sacramento River, California
Sickman, J. O., Zanoli, M. J., & Mann, H. L. (2007) · Water Resources Research · doi:10.1029/2007wr005954 · Cited by 182 · see citing works
Development of a Global Fire Weather Database
Field, R. D., Spessa, A. C., Aziz, N. A., Camia, A., Cantin, A. S., Carr, R., de Groot, W. J., Dowdy, A. J., Flannigan, M., Manomaiphiboon, K., et al. (2015) · Natural hazards and earth system sciences · doi:10.5194/nhess-15-1407-2015 · Cited by 161 · see citing works
Self-citationSeibert, J., McDonnell, J. J., & Woodsmith, R. D. (2010) · Hydrology research · doi:10.2166/nh.2010.036 · Cited by 135 · see citing works
Falkenmark, M. (2001) · International Journal of Water Resources Development · doi:10.1080/07900620120094073 · Cited by 130 · see citing works
Relations between soil hydraulic properties and burn severity
Moody, J. A., Ebel, B. A., Nyman, P., Martin, D. A., Stoof, C., & McKinley, R. (2016) · International Journal of Wildland Fire · doi:10.1071/wf14062 · Cited by 122 · see citing works
Dunnette, P. V., Higuera, P. E., McLauchlan, K. K., Derr, K. M., Briles, C. E., & Keefe, M. H. (2014) · New Phytologist · doi:10.1111/nph.12828 · Cited by 116 · see citing works
Relationships between Human Population Density and Burned Area at Continental and Global Scales
Bistinas, I., Oom, D., Sá, A. C. L., Harrison, S. P., Prentice, I. C., & Pereira, J. M. C. (2013) · PLoS ONE · doi:10.1371/journal.pone.0081188 · Cited by 110 · see citing works
World Atlas of Natural Disaster Risk
(2015) · IHDP/Future Earth-Integrated Risk Governance Project Series · doi:10.1007/978-3-662-45430-5 · Cited by 98 · cited 1× · see citing works
“However, several important advancements in natural resources global mapping [14] and the development of innovative methods and global databases now make it possible to better understand the intersection of wildfire activity [15,16] and water resource availability [17,18] at the scale of the planet.”
BackgroundChanges in evapotranspiration following wildfire in resprouting eucalypt forests
Nolan, R. H., Lane, P. N. J., Benyon, R. G., Bradstock, R. A., & Mitchell, P. J. (2014) · Ecohydrology · doi:10.1002/eco.1463 · Cited by 92 · see citing works
Kasischke, E. S., Bourgeau-Chavez, L. L., & Johnstone, J. F. (2007) · Remote Sensing of Environment · doi:10.1016/j.rse.2006.10.020 · Cited by 82 · see citing works
Water resources planning for a river basin with recurrent wildfires
Santos, R. M. B., Fernandes, L. F. S., Pereira, M., Cortes, R., & Pacheco, F. A. L. (2015) · The Science of The Total Environment · doi:10.1016/j.scitotenv.2015.04.058 · Cited by 72 · see citing works
World Atlas of Natural Disaster Risk
Shi, P., Wang, J., Xu, W., Ye, T., Yang, S., Liu, L., Fang, W., Liu, K., Li, N., & Wang, M. (2015) · IHDP/Future earth-integrated risk governance project series · doi:10.1007/978-3-662-45430-5_17 · Cited by 67 · see citing works
Probabilistic assessment of wildfire hazard and municipal watershed exposure
Scott, J., Helmbrecht, D., Thompson, M. P., Calkin, D. E., & Marcille, K. (2012) · Natural Hazards · doi:10.1007/s11069-012-0265-7 · Cited by 66 · see citing works
Assessing global exposure to natural hazards: Progress and future trends
Lerner‐Lam, A. L. (2007) · Environmental Hazards · doi:10.1016/j.envhaz.2007.04.007 · Cited by 64 · see citing works
A global map of the functionality of terrestrial ecosystems
Biber‐Freudenberger, L., Hobson, P. R., Schluck, M., & Ibisch, P. L. (2012) · Ecological Complexity · doi:10.1016/j.ecocom.2012.08.002 · Cited by 49 · see citing works
Thompson, M., Scott, J., Langowski, P., Gilbertson-Day, J., Haas, J., & Bowne, E. (2013) · Water · doi:10.3390/w5030945 · Cited by 45 · see citing works
Assessing possible shifts in wildfire regimes under a changing climate in mountainous landscapes
Mori, A. S., & Johnson, E. A. (2013) · Forest Ecology and Management · doi:10.1016/j.foreco.2013.09.036 · Cited by 25 · see citing works
Flagged first, then by citations
1 of the 58 references couldn’t be matched to a known paper.
Research works printed but not linked: 2
- USDA (2005). Wildland Fire in Ecosystems: Effects of Fire on Soil and Water, Gen. Tech. Rep. RMRS-GTR-42-vol.4. Ogden.
- Moody, J.A., and Martin, D.A. (2004, January 18–21). Wildfire impacts on reservoir sedimentation in the western United States. Proceedings of the Ninth International Symposium on River Sedimentation, Yichang, China.
Cited by
Sorted by citations
Climate, wildfire, and erosion ensemble foretells more sediment in western USA watersheds
Sankey, J. B., Kreitler, J. R., Hawbaker, T. J., McVay, J. L., Miller, M. E., Mueller, E. R., Vaillant, N. M., Lowe, S. E., & Sankey, T. T. (2017) · Geophysical Research Letters · doi:10.1002/2017gl073979 · Cited by 161 · see citing works
Wildland fire risk research in Canada
Johnston, L. M., Wang, X., Erni, S., Taylor, S. W., McFayden, C. B., Oliver, J. A., Stockdale, C., Christianson, A. C., Boulanger, Y., Gauthier, S., et al. (2020) · Environmental Reviews · doi:10.1139/er-2019-0046 · Cited by 132 · see citing works
Self-citationA spatial evaluation of global wildfire-water risks to human and natural systems
Robinne, F.-N., Bladon, K. D., Miller, C., Parisien, M.-A., Mathieu, J., & Flannigan, M. D. (2018) · Science of The Total Environment · doi:10.1016/j.scitotenv.2017.08.112 · Cited by 122 · see citing works
Self-citationAt the nexus of fire, water and society
Martin, D. A. (2016) · Philosophical Transactions of the Royal Society B: Biological Sciences · doi:10.1098/rstb.2015.0172 · Cited by 106 · see citing works
Molecular insights and impacts of wildfire-induced soil chemical changes
Lopez, A. M., Avila, C. C. E., VanderRoest, J. P., Roth, H. K., Fendorf, S. E., & Borch, T. (2024) · Nature Reviews Earth & Environment · doi:10.1038/s43017-024-00548-8 · Cited by 105 · see citing works
Nunes, J. P., Doerr, S. H., Sheridan, G., Neris, J., Santín, C., Emelko, M. B., Silins, U., Robichaud, P. R., Elliot, W. J., & Keizer, J. (2018) · Hydrological Processes · doi:10.1002/hyp.11434 · Cited by 97 · see citing works
Self-citationEbel, B. A. (2020) · Journal of Hydrology · doi:10.1016/j.jhydrol.2020.124765 · Cited by 95 · see citing works
Murphy, B. P., Czuba, J. A., & Belmont, P. (2019) · Earth Surface Processes and Landforms · doi:10.1002/esp.4635 · Cited by 86 · see citing works
Wagenbrenner, J. W., Ebel, B. A., Bladon, K. D., & Kinoshita, A. M. (2021) · Journal of Hydrology · doi:10.1016/j.jhydrol.2021.126772 · Cited by 84 · see citing works
Self-citationRengers, F. K., McGuire, L. A., Kean, J. W., Staley, D. M., Dobre, M., Robichaud, P. R., & Swetnam, T. L. (2021) · Journal of Geophysical Research Earth Surface · doi:10.1029/2020jf006053 · Cited by 82 · see citing works
Reframing the Challenge of Global Wildfire Threats to Water Supplies
Hallema, D. W., Robinne, F., & Bladon, K. D. (2018) · Earth's Future · doi:10.1029/2018ef000867 · Cited by 78 · see citing works
Self-citationA Regional-Scale Index for Assessing the Exposure of Drinking-Water Sources to Wildfires
Robinne, F., Bladon, K. D., Silins, U., Emelko, M. B., Flannigan, M., Parisien, M., Wang, X., Kienzle, S. W., & Dupont, D. (2019) · Forests · doi:10.3390/f10050384 · Cited by 40 · see citing works
Self-citationWildfires as a Source of PAHs in Surface Waters of Background Areas (Lake Baikal, Russia)
Горшков, А. Г., Izosimova, O. N., Kustova, O. V., Marinaite, I. I., Galachyants, Y., Николаевич, С. В., & Khodzher, T. V. (2021) · Water · doi:10.3390/w13192636 · Cited by 38 · see citing works
Wall, S., Murphy, B. P., Belmont, P., & Yocom, L. L. (2022) · Earth Surface Processes and Landforms · doi:10.1002/esp.5480 · Cited by 34 · see citing works
Strategic application of wildland fire suppression in the southwestern United States
Young, J. D., Thode, A. E., Huang, C.-H., Ager, A. A., & Fulé, P. Z. (2019) · Journal of Environmental Management · doi:10.1016/j.jenvman.2019.01.003 · Cited by 30 · see citing works
Johnston, L. M., Blanchi, R., & Jappiot, M. (2019) · Springer eBooks · doi:10.1007/978-3-319-51727-8_130-1 · Cited by 24 · see citing works
Atmospheric change as a driver of change in the Canadian boreal zone1
Yeung, A. C. Y., Paltsev, A., Daigle, A., Duinker, P. N., & Creed, I. F. (2018) · Environmental Reviews · doi:10.1139/er-2018-0055 · Cited by 23 · see citing works
Economic drivers of global fire activity: A critical review using the DPSIR framework
Kim, Y., Rodrígues, M., & Robinne, F. (2021) · Forest Policy and Economics · doi:10.1016/j.forpol.2021.102563 · Cited by 23 · see citing works
Self-citationForest fire risk indices and zoning of hazardous areas in Sorocaba, São Paulo state, Brazil
Ziccardi, L. G., Thiersch, C. R., Yanai, A. M., Fearnside, P. M., & Ferreira-Filho, P. J. (2019) · Journal of Forestry Research · doi:10.1007/s11676-019-00889-x · Cited by 19 · see citing works
Economic Analysis of Wildfire Impacts to Water Quality: A Review
Wibbenmeyer, M. J., Sloggy, M. R., & Sánchez, J. J. (2023) · Journal of Forestry · doi:10.1093/jofore/fvad012 · Cited by 15 · see citing works
Climate change unevenly affects the dependence of multiple climate-related hazards in China
Zong, X., Yin, Y., & Yin, M. (2024) · npj Climate and Atmospheric Science · doi:10.1038/s41612-024-00614-4 · Cited by 14 · see citing works
Freeze–thaw processes degrade post‐fire water repellency in wet soils
Rakhmatulina, E., & Thompson, S. (2020) · Hydrological Processes · doi:10.1002/hyp.13931 · Cited by 12 · see citing works
Callegary, J. B., Norman, L. M., Eastoe, C. J., Sankey, J. B., & Youberg, A. (2021) · Air Soil and Water Research · doi:10.1177/11786221211001768 · Cited by 12 · see citing works
Wildland fire impacts on water yield across the contiguous United States
Hallema, D. W., Sun, G., Caldwell, P. V., Robinne, F., Bladon, K. D., Norman, S. P., Liu, Y., Cohen, E. C., & McNulty, S. G. (2019) · doi:10.2737/srs-gtr-238 · Cited by 12 · see citing works
Self-citationBlackburn, E. A. J., Dickson‐Anderson, S. E., Anderson, W. B., & Emelko, M. B. (2023) · ACS ES&T Water · doi:10.1021/acsestwater.2c00209 · Cited by 11 · see citing works
Self-citationBrucker, C. P., Livneh, B., Minear, J. T., & Rosario‐Ortiz, F. L. (2022) · Environmental Science Processes & Impacts · doi:10.1039/d2em00045h · Cited by 13 · see citing works
Sanin, F. A. M., Alias, N. E., Kanniah, K. D., Kadir, M. A. A., Mohamad, I. I., & Paramasivam, R. (2022) · Journal of Hydrology and Hydromechanics · doi:10.2478/johh-2022-0029 · Cited by 8 · see citing works
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Кузнецов, Г. В., Zhdanova, A. O., Strizhak, P. A., & Atroshenko, Y. K. (2020) · Journal of Engineering Physics and Thermophysics · doi:10.1007/s10891-020-02251-z · Cited by 7 · see citing works
Assessing the Vulnerability of California Water Utilities to Wildfires
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Forest Fires and Climate Change Impacts on Water Resources
Verma, M., & Sati, M. (2025) · Springer eBooks · doi:10.1007/978-3-031-89967-6_9 · Cited by 3 · see citing works
Análise multitemporal de incêndios florestais ocorridos no Estado de Minas Gerais entre 2001 e 2020
Latuf, M. D. O., Rios, G. D. S., & Pereira, R. C. (2022) · Revista Cerrados · doi:10.46551/rc24482692202206 · Cited by 3 · see citing works
Evaporation of Promising Fire Extinguishing Agent Droplets
Zhdanova, A. O., Islamova, A. G., Kurapov, R., & Волков, Р. С. (2023) · Forests · doi:10.3390/f14020301 · Cited by 3 · see citing works
Johnston, L. M., Blanchi, R., & Jappiot, M. (2020) · Springer eBooks · doi:10.1007/978-3-319-52090-2_130 · Cited by 3 · see citing works
Development of Performance Evaluation Indicators for Table Grape Packaging Units. 2. Global Indexes
Kogachi, E., Ferreira, A. M. S., Cavalcante, C., & Embiruçu, M. (2021) · Sustainability · doi:10.3390/su13116367 · Cited by 2 · see citing works
Forest Fires and Forest Degradations: Approaches to Mitigation
Shaji, A., Chandel, S., Antony, N., Santhosh, V., Jisha, E. D., & Kamalolbhavan, B. N. (2025) · Forestry sciences · doi:10.1007/978-3-031-84055-5_15 · Cited by 1 · see citing works
Wildfire Impacts on Water Quality and Treatability
Geng, X. (2018) · UWSpace (University of Waterloo) · Cited by 1 · see citing works
Review of fire effects on soil properties
(2019) · CSIRO Publishing eBooks · doi:10.1071/9781486308149.bk07743_pt01
Overview of Wildland-Urban Interface (WUI) Fires
Blanchi, R., & Alessio, A. (2026) · The Society of fire protection engineers series · doi:10.1007/978-3-031-59212-6_98
- Authors
- Robinne, F.-N., Miller, C., Parisien, M.-A., Emelko, M., Bladon, K., Silins, U., & Flannigan, M.
- Affiliations
- University of Alberta (CA)
- Aldo Leopold Wilderness Research Institute, Missoula, MT 59801, USA
- Canadian Forest Service (CA)
- University of Waterloo (CA)
- Oregon State University (US)
- Corresponding author
- Robinne, François-Nicolas
- ORCID
- Venue
- Forests
- Publisher
- MDPI AG
- Published
- 2016-01-13
- Volume
- 7
- Issue
- 1
- Pages
- 22
- ISSN
- 1999-4907 (ISSN-L)
- OpenAlex
- W2237347042
- Cited by
- 41
- References
- 58
- Citations by year
- 2026: 1 · 2025: 2 · 2024: 3 · 2023: 4 · 2022: 5 · 2021: 6 · 2020: 5 · 2019: 7 · 2018: 4 · 2017: 2 · 2016: 2
- FWCI
- 3.71
- Type
- journal article
- Language
- en
- Open access
- gold
- doi.org
- Licence
- Locations
- Forests (publishedVersion, cc-by)
- DOAJ (DOAJ: Directory of Open Access Journals) (submittedVersion, cc-by-sa)
- Funders
- Global Foundation for Eating Disorders
- Topics
- Physical Sciences › Environmental Science › Global and Planetary Change › Fire effects on ecosystems
- Physical Sciences › Engineering › Ocean Engineering › Water resources management and optimization
- Physical Sciences › Environmental Science › Water Science and Technology › Hydrology and Watershed Management Studies
- Keywords
- forest fires, water resources, exposure index, post-fire effects, freshwater quality, water availability, mountain ranges, water security, global assessment
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