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Little change in global drought over the past 60 years
Abstract
Drought is expected to increase in frequency and severity in the future as a result of climate change, mainly as a consequence of decreases in regional precipitation but also because of increasing evaporation driven by global warming. Previous assessments of historic changes in drought over the late twentieth and early twenty-first centuries indicate that this may already be happening globally. In particular, calculations of the Palmer Drought Severity Index (PDSI) show a decrease in moisture globally since the 1970s with a commensurate increase in the area in drought that is attributed, in part, to global warming. The simplicity of the PDSI, which is calculated from a simple water-balance model forced by monthly precipitation and temperature data, makes it an attractive tool in large-scale drought assessments, but may give biased results in the context of climate change. Here we show that the previously reported increase in global drought is overestimated because the PDSI uses a simplified model of potential evaporation that responds only to changes in temperature and thus responds incorrectly to global warming in recent decades. More realistic calculations, based on the underlying physical principles that take into account changes in available energy, humidity and wind speed, suggest that there has been little change in drought over the past 60 years. The results have implications for how we interpret the impact of global warming on the hydrological cycle and its extremes, and may help to explain why palaeoclimate drought reconstructions based on tree-ring data diverge from the PDSI-based drought record in recent years.
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“Two recent studies published in Nature Climate Change 25 and Nature 26 came to opposing conclusions about whether there are noticeable changes in drought trends as a result of climate change.”
From A Big Data Guide to Understanding Climate Change: The Case for Theory-Guided Data Science (2014) · cites this paper as [26]
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“Most of the empirical studies on long-term trends in drought hazard have focused on meteorological drought (e.g. Sheffield et al., 2012; Spinoni et al., 2017) and on hydrological drought (e.g. Stahl et al., 2010; Laaha et al., 2017).”
BackgroundWartenburger, R., Seneviratne, S. I., Hirschi, M., Chang, J., Ciais, P., Deryng, D., Elliott, J. W., Folberth, C., Gosling, S. N., Gudmundsson, L., et al. (2018) · Environmental Research Letters · doi:10.1088/1748-9326/aac4bb · Cited by 88
“…the latter issue: the difficulties of choosing the most appropriate ET scheme for specific applications (e.g. Kay et al 2013, Bormann 2011), which can even translate into ambiguities in the interpretation of the evolution of past global drought conditions (Sheffield et al 2012, Seneviratne 2012).”
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“The 3-h PGF data used in this study are based on the NCEP–NCAR reanalyses (Sheffield et al. 2012), with the precipitation and temperature bias corrected using the Climatic Research Unit (CRU)Time Series, version 3.0 (TS3.”
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“In addition to CCSM4, we also analyzed the simulations from 25 global climate models (Table 1) in phase 5 of the Coupled Model Intercomparison Project (CMIP5) database (Taylor et al. 2012).”
MethodDrought characteristics over China during 1980–2015
Shao, D., Chen, S., Tan, X., & Gu, W. (2018) · International Journal of Climatology · doi:10.1002/joc.5515 · Cited by 83
“Although Thornthwaite method is more concise and easily applicable, inaccuracies are introduced by neglecting the non-temperature components (Hobbins et al., 2008; McVicar et al., 2012; Sheffield et al., 2012).”
MethodThe contribution of internal climate variability to climate change impacts on droughts
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A hydrological perspective on evaporation: historical trends and future projections in Britain
Kay, A. L., Bell, V. A., Blyth, E., Crooks, S. M., Davies, H., & Reynard, N. S. (2013) · Journal of Water and Climate Change · doi:10.2166/wcc.2013.014 · Cited by 82
The dry season intensity as a key driver of NPP trends
Tortarolo, G. N. M., Friedlingstein, P., Sitch, S. A., Seneviratne, S. I., Fletcher, I. N., Mueller, B., Greve, P., Anav, A., Liu, Y., Ahlström, A., et al. (2016) · Geophysical Research Letters · doi:10.1002/2016gl068240 · Cited by 82
“Nonetheless, some regional (or latitudinal) trends can be identified [Sheffield et al., 2012; Zhang et al., 2007], and a global increase in the range between dry versus wet season precipitation has been reported [Chou et al., 2013], particularly over the tropics [Feng et al., 2013].”
BackgroundDisconnection Between Trends of Atmospheric Drying and Continental Runoff
Yang, Y., Zhang, S., McVicar, T. R., Beck, H. E., Zhang, Y., & Liu, B. (2018) · Water Resources Research · doi:10.1029/2018wr022593 · Cited by 81
“This issue has been recently discussed in several studies (Milly & Dunne, 2016, 2017; Roderick et al., 2015; Sheffield et al., 2012) and is again highlighted here (Figures 2 and 4–6).”
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“No longterm-drought-area-change conclusion is also supported by the widely used PDSI dynamics over the past 60 years (Sheffield et al. 2013) and analysis of the 30-year VH data in Ukraine, although the mean Ukrainian temperature increased 1.5 C over the last 50 years (Kogan et al. 2013).”
MethodInfluentialPotopová, V., Boroneant, C., Možný, M., & Soukup, J. (2015) · International Journal of Climatology · doi:10.1002/joc.4588 · Cited by 82
“However, some shortcomings of PDSI/scPDSI are still under debate in the drought researcher community (Vicente-Serrano et al., 2011, 2014; Sheffield et al., 2012; Beguería et al., 2014) mainly because of its simplicity (Wells et al., 2004) owing to the treatment of potential evaporation (the…”
BackgroundSamaniego, L., Kumar, R., Breuer, L., Chamorro, A., Flörke, M., Pechlivanidis, I. G., Schäfer, D., Shah, H. L., Vetter, T., Wortmann, M., et al. (2016) · Climatic Change · doi:10.1007/s10584-016-1778-y · Cited by 81
“Contradictory results have been reported in recent years (e.g., Dai 2013; Sheffield et al. 2013) regarding this topic.”
BackgroundMethodResultNational-scale analysis of simulated hydrological droughts (1891–2015)
Rudd, A. C., Bell, V. A., & Kay, A. L. (2017) · Journal of Hydrology · doi:10.1016/j.jhydrol.2017.05.018 · Cited by 80
“Similarly, Sheffield et al. (2012) find little change in meteorological drought globally over 1950-2010, although this is the subject of debate as there have been a number of studies producing apparently conflicting results (Trenberth et al. 2014).”
ResultThe first global multi-timescale daily SPEI dataset from 1982 to 2021
Liu, X., Yu, S., Yang, Z., Dong, J., & Peng, J. (2024) · Scientific Data · doi:10.1038/s41597-024-03047-z · Cited by 91
“D i were calculated by subtracting PET from precipitation using the following equation at a given day i : The obtained D i were summed at different timescales D kj,i , which represented a given day i and year j depending on the chosen timescale k (days).”
MethodInfluentialAbatzoglou, J. T., & Ficklin, D. L. (2017) · Water Resources Research · doi:10.1002/2017wr020843 · Cited by 80
“These models, however, are subject to uncertainties in hydrological model structure, simplification, and parameterization [Wilby and Harris 2006; Renard et al. 2010], particularly when applied to watersheds without observed data for calibration [Sivapalan et al. 2003].”
BackgroundAssessment of drought impacts on crop yields across Nepal during 1987–2017
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“, 2018) that is aggravated by the changing climate and anthropogenic drivers (Mishra and Singh, 2010; Sheffield et al., 2012).”
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“This result coincides with recent studies reporting little change in global drought since 1950 (Sheffield et al., 2012).”
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“2013), linked strongly with ongoing climate changes (Sheffield et al .”
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“Although PET is usually calculated by means of the Penman–Monteith's approach (Allen et al., 2006; Sheffield et al., 2012; Trenberth et al., 2014), such method is not free from criticism due to specific thresholds and unlimited supply of moisture, that is not realistic in very dry conditions…”
BackgroundMethodHigh-income groups disproportionately contribute to climate extremes worldwide
Schöngart, S., Nicholls, Z., Hoffmann, R., Pelz, S., & Schleussner, C. (2025) · Nature Climate Change · doi:10.1038/s41558-025-02325-x · Cited by 88
“However, PET estimates via the Thornthwaite method are prone to overestimations in terms of magnitude and temporal trends 51 .”
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Global estimation of long-term persistence in annual river runoff
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“Uncertainty in AET estimates is caused by at least (1) the different PET approaches (Sheffield et al., 2012; Peng et al., 2018), (2) the complexity of the parameterization of the biophysical limitations (Chen et al.”
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“Drought is an intermittent disturbance when water supply does not satisfy the demand for a long time [1,2], which can bring profound effects on carbon-water fluxes in terrestrial ecosystems at global and regional scales [3,4].”
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“1 of 17 This behavior has been especially evident since the 1980s (Sheffield et al., 2012), when a relatively rapid increase in global temperature was observed (Hartmann et al., 2013).”
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Quantitative and detailed spatiotemporal patterns of drought in China during 2001–2013
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CMIP5 drought projections in Canada based on the Standardized Precipitation Evapotranspiration Index
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An Enhanced Effective Reconnaissance Drought Index for the Characterisation of Agricultural Drought
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“Additionally, it has been reported that the PDSI may give biased results in the context of climate change (Sheffield et al. 2012).”
BackgroundMathbout, S., Bustins, J. A. L., Royé, D., & Vide, J. M. (2021) · Atmosphere · doi:10.3390/atmos12080941 · Cited by 76
“Although the estimated evapotranspiration using temperature-based models may magnify the impacts of the current global warming [66], it has been indicated that drought indices provide reliable estimates of the true global drought trend when using the temperature-based models [67].”
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Coverage-dependent amplifiers of vegetation change on global water cycle dynamics
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“Potential evapotranspiration (PET) was estimated with the Penman- Monteith formula, which is favored because it does not overestimate drought (Allen et al. 1998, Sheffield et al. 2012).”
MethodYang, T., Ding, J., Liu, D., Wang, X., & Wang, T. (2018) · Journal of Climate · doi:10.1175/jcli-d-18-0261.1 · Cited by 76
“This result is consistent with the observed nonsignificant trend of Penman–Monteith (PM)based PDSI (0.08% 6 0.21% yr21 during the period 1980–2008) reported by Sheffield et al. (2012) when using different combinations of precipitation and radiation datasets to generate an ensemble of sc_PDSI.”
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“This definition has two main reasons; firstly, the consistent low drought intensity could also greatly influence vegetation growth, agricultural production, and the environment (Sheffield et al. 2012; Wang et al. 2014).”
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“…of global warming, extreme climate events have received increasing attention by scientific communities (Aguilar et al. 2005; Lehner et al. 2006; Sheffield et al. 2012; Xu et al. 2009), due to the fact that the variations in extreme climate events are more sensitive to climate change than those…”
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“Temperature based methods tend to overestimate evapotranspiration with increasing temperatures (Sheffield et al., 2012) and more physically based methods might provide more accurate estimations of PET.”
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Spring-summer droughts in the Czech Land in 1805-2012 and their forcings
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“Globally there is currently conflicting evidence (Trenberth et al. 2014) as to whether droughts are changing (Sheffield et al. 2012; Dai 2013; Damberg and AghaKouchak 2014).”
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“An accurately estimated ET can therefore provide a comprehensive contribution to understanding the changes in hydrological cycles and the associated extreme events, such as droughts and floods, as well as their impacts on ecosystem productivity, water-use efficiency, and irrigation (Sheffield et al., 2012; Sun et al.,…”
Vicente-Serrano, S. M., Domínguez‐Castro, F., Reig, F., Tomàs‐Burguera, M., Peña‐Angulo, D., Latorre, B., Beguerı́a, S., Rabanaque, I., Noguera, I., Lorenzo‐Lacruz, J., et al. (2022) · Geoscience Data Journal · doi:10.1002/gdj3.178 · Cited by 76
“Nevertheless, it is widely known that empirical AED approximations based on temperature data alone show limitations under global warming, as is not the case with physically based approaches (Sheffield et al., 2012; Vicente-Serrano et al., 2020).”
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Wang, M., Jiang, S. S., Ren, L., Xu, C.-Y., Yuan, F., Liu, Y., & Yang, X. (2020) · Journal of Hydrology · doi:10.1016/j.jhydrol.2020.125384 · Cited by 71
Consequences of climate change on airborne pollen in Bavaria, Central Europe
Rojo, J., Picornell, A., Oteros, J., Werchan, M., Werchan, B., Bergmann, K., Smith, M., Weichenmeier, I., Schmidt‐Weber, C. B., & Buters, J. (2021) · Regional Environmental Change · doi:10.1007/s10113-020-01729-z · Cited by 70
On observed aridity changes over the semiarid regions of India in a warming climate
Ramarao, M. V. S., Sanjay, J., Krishnan, R., Mujumdar, M., Bazaz, A. B., & Revi, A. (2018) · Theoretical and Applied Climatology · doi:10.1007/s00704-018-2513-6 · Cited by 69
“…of Tropical Meteorology, Pune 411008, India 2 Indian Institute for Human Settlements, Bangalore, India at global and regional scales (Dai 2011; Sheffield et al. 2012; Liu et al. 2013; Cook et al. 2014; Sherwood and Fu 2014; Scheff and Frierson 2015 ; Moral et al. 2017), during past few…”
BackgroundAridity and desertification in the Mediterranean under EURO-CORDEX future climate change scenarios
Carvalho, D., Pereira, S., Silva, R., & Rocha, A. (2022) · Climatic Change · doi:10.1007/s10584-022-03454-4 · Cited by 62
“Several studies have shown that the method chosen to estimate PET strongly influences its results, and that simpler PET estimation formulas may not be accurate in a climate change context (e.g. Lian et al. 2021; Sheffield et al. 2012).”
MethodZhang, Q., Miao, C., Guo, X., Gou, J., & Su, T. (2023) · Journal of Hydrology · doi:10.1016/j.jhydrol.2023.129752 · Cited by 69
Liu, S., Kang, W., & Wang, T. (2016) · Environmental Earth Sciences · doi:10.1007/s12665-015-4996-0 · Cited by 69
“…China 2 Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China overestimated (Sheffield et al. 2012), the role of warminginduced drought stress is evident in recent studies that have analyzed drought impacts on net primary…”
BackgroundInfluentialStisen, S., Koch, J., Sonnenborg, T. O., Refsgaard, J. C., Bircher, S., Ringgaard, R., & Jensen, K. H. (2018) · Hydrological Processes · doi:10.1002/hyp.13177 · Cited by 68
Shi, L., Feng, P., Wang, B., Liu, D. L., Cleverly, J., Fang, Q., & Yu, Q. (2020) · Journal of Hydrology · doi:10.1016/j.jhydrol.2020.124756 · Cited by 68
Drought trend, frequency and extremity across a wide range of climates over Iran
Nouri, M., & Homaee, M. (2020) · Meteorological Applications · doi:10.1002/met.1899 · Cited by 69
“Although inconsistent trend results are obtained for drought severity and frequency mainly due to disparities between datasets, and drought characterizations and definitions, an overall drying pattern has been reported since half a century ago over the globe (Sheffield et al., 2012; Dai, 2013; Trenberth et al., 2013;…”
BackgroundElevation dependence of drought legacy effects on vegetation greenness over the Tibetan Plateau
Li, P., Zhu, D., Wang, Y., & Liu, D. (2020) · Agricultural and Forest Meteorology · doi:10.1016/j.agrformet.2020.108190 · Cited by 69
Projected changes in the Iberian Peninsula drought characteristics
Ojeda, M. G., Gámiz‐Fortis, S. R., Romero-Jiménez, E., Rosa-Cánovas, J. J., Yeste, P., Castro‐Díez, Y., & Esteban‐Parra, M. J. (2020) · The Science of The Total Environment · doi:10.1016/j.scitotenv.2020.143702 · Cited by 71
Wei, W., Zhang, J., Zhou, J., Zhou, L., Xie, B., & Li, C. (2021) · Journal of Environmental Management · doi:10.1016/j.jenvman.2021.112733 · Cited by 67
Zhuang, Y., Fu, R., Lisonbee, J., Sheffield, A., Parker, B.-A. A., & Deheza, G. (2024) · Science Advances · doi:10.1126/sciadv.adn9389 · Cited by 79
“Simpler methods such as Thornthwaite ( 72 ) usually overestimate the PET magnitude and trend ( 73 ).”
Kam, J., Sheffield, J., & Wood, E. F. (2014) · Geophysical Research Letters · doi:10.1002/2014gl060973 · Cited by 68
“Long-term analyses for the southern U.S. [Chen et al., 2012] and the U.S. [Andreadis and Lettenmaier, 2006; Sheffield et al., 2012] show that there is little change or even a decrease in drought, which may be related to the weakening of oceanic controls.”
BackgroundSelf-citationDrought Forecasting Using Stochastic Models in a Hyper-Arid Climate
Mossad, A., & Alazba, A. A. (2015) · Atmosphere · doi:10.3390/atmos6040410 · Cited by 68
“Prominently, the impact of intense long drought on natural ecosystems essentially concerns regional agriculture, water resources and the environment [4].”
BackgroundHankin, L. E., Higuera, P. E., Davis, K. T., & Dobrowski, S. Z. (2019) · Ecosphere · doi:10.1002/ecs2.2679 · Cited by 68
Zhang, Z., Xu, W., Qin, Q., & Long, Z. (2020) · IEEE Transactions on Geoscience and Remote Sensing · doi:10.1109/tgrs.2020.2999371 · Cited by 70
“The global average temperature has been rising, particularly in recent years, which leads to global warming and, thus, requires more water resources for human activities than before [5]–[8].”
BackgroundProbabilistic impacts of compound dry and hot events on global gross primary production
Wu, X., & Jiang, D. (2022) · Environmental Research Letters · doi:10.1088/1748-9326/ac4c5b · Cited by 69
Evaluation of TRMM 3B43 Precipitation Data for Drought Monitoring in Jiangsu Province, China
Tao, H., Fischer, T., Zeng, Y., & Fraedrich, K. (2016) · Water · doi:10.3390/w8060221 · Cited by 67
“Research on droughts has received special attention in recent years due to concerns over global climate change [1–3].”
BackgroundKang, H., & Sridhar, V. (2017) · Journal of Hydrology Regional Studies · doi:10.1016/j.ejrh.2017.06.003 · Cited by 68
“…and soil moisture can occur over many areas in low- and mid-latitudes due to increasing greenhouse gas (GHG) concentrations (Dai, 2013; Rajsekhar et al., 2015; Kumar et al., 2014; Chen and Sun, 2015; Mishra et al., 2014; Dai, 2011; Wang, 2005; Burke et al., 2006; Sheffield et al., 2012).”
BackgroundCopulas-Based Drought Characteristics Analysis and Risk Assessment across the Loess Plateau of China
She, D., & Xia, J. (2017) · Water Resources Management · doi:10.1007/s11269-017-1826-z · Cited by 67
Zhang, C., Filella, I., Liu, D., Ogaya, R., Llusià, J., Asensio, D., & Peñuelas, J. (2017) · Remote Sensing · doi:10.3390/rs9111189 · Cited by 67
“Droughts have occurred frequently under global warming around the world [1,2], prominently disturbing terrestrial ecosystemic services and functioning, such as water cycles [3], terrestrial production [4,5], ecosystemic respiration [4], biodiversity [6] and plant survival and mortality [7,8].”
BackgroundLuce, C. H., Vose, J. M., Pederson, N., Campbell, J. L., Millar, C. I., Kormos, P. R., & Woods, R. A. (2016) · Forest Ecology and Management · doi:10.1016/j.foreco.2016.05.020 · Cited by 67
“The Penman-Monteith potential evaporation formulation (Monteith, 1965), which has been adapted for use in PDSI and as part of more complex water balance models (Sheffield et al., 2012; Cook et al., 2014), implicitly carries a strong temperature dependence in the calculation of the reference evaporation as a function o…”
BackgroundMethodChanging impacts and societal responses to drought in southwestern Germany since 1800
Erfurt, M., Glaser, R., & Blauhut, V. (2019) · Regional Environmental Change · doi:10.1007/s10113-019-01522-7 · Cited by 66
Sippel, S., & Otto, F. E. L. (2014) · Climatic Change · doi:10.1007/s10584-014-1153-9 · Cited by 74
“Also, the applied water balance proxy P − PET does not account for several other factors that determine dryness, for example antecedent soil moisture deficits (Seneviratne 2012; Sheffield et al. 2012).”
BackgroundMethodEffects of different reference periods on drought index (SPEI) estimations from 1901 to 2014
Um, M., Kim, Y., Park, D., & Kim, J. (2017) · Hydrology and earth system sciences · doi:10.5194/hess-21-4989-2017 · Cited by 66
“As different studies have used different meteorological drought indices (Seneviratne, 2012; Sheffield et al., 2012; Trenberth et al., 2014; Nasrollahi et al., 2015; Touma et al., 2015), this study focuses on the SPEI.”
Hydrological Modeling of Climate Change Impacts
Hakala, K., Addor, N., Teutschbein, C., Vis, M. J. P., Dakhlaoui, H., & Seibert, J. (2019) · Wiley eBooks · doi:10.1002/9781119300762.wsts0062 · Cited by 68
Tian, W., Liu, X., Liu, C., & Bai, P. (2018) · Journal of Hydrology · doi:10.1016/j.jhydrol.2018.08.015 · Cited by 65
Metadata
- Authors
- Sheffield, J., Wood, E. F., & Roderick, M. L.
- Affiliations
- Princeton University (US)
- Australian National University (AU)
- Corresponding author
- Sheffield, Justin
- Venue
- Nature
- Published
- 2012-11
- Volume
- 491
- Issue
- 7424
- Pages
- 435-438
- ISSN
- 0028-0836 (ISSN-L)
- 1476-4687
- OpenAlex
- W2015522309
- Cited by
- 1,978
- References
- 50
- Citations by year
- 2026: 97 · 2025: 126 · 2024: 131 · 2023: 162 · 2022: 188 · 2021: 196 · 2020: 174 · 2019: 159 · 2018: 160 · 2017: 139 · 2016: 144 · 2015: 121 · 2014: 110 · 2013: 66 · 2012: 3
- FWCI
- 79.51
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Nature (publishedVersion)
- PubMed (publishedVersion)
- RePEc: Research Papers in Economics (submittedVersion)
- ePrints Soton (University of Southampton) (submittedVersion)
- ANU Open Research (Australian National University) (submittedVersion)
- Topics
- Physical Sciences › Environmental Science › Global and Planetary Change › Hydrology and Drought Analysis
- Physical Sciences › Environmental Science › Global and Planetary Change › Plant Water Relations and Carbon Dynamics
- Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
- Keywords
- global drought, Palmer Drought Severity Index, drought trends, potential evaporation, global warming, water cycle, drought indices, climate change impacts, water balance modeling
- MeSH terms
- Models, Theoretical, Temperature, Time Factors, Droughts, Global Warming
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