Changes in vegetation in northern Alaska under scenarios of climate change, 2003-2100: implications for climate feedbacks
Abstract
Assessing potential future changes in arctic and boreal plant species productivity, ecosystem composition, and canopy complexity is essential for understanding environmental responses under expected altered climate forcing. We examined potential changes in the dominant plant functional types (PFTs) of the sedge tundra, shrub tundra, and boreal forest ecosystems in ecotonal northern Alaska, USA, for the years 2003–2100. We compared energy feedbacks associated with increases in biomass to energy feedbacks associated with changes in the duration of the snow‐free season. We based our simulations on nine input climate scenarios from the Intergovernmental Panel on Climate Change (IPCC) and a new version of the Terrestrial Ecosystem Model (TEM) that incorporates biogeochemistry, vegetation dynamics for multiple PFTs (e.g., trees, shrubs, grasses, sedges, mosses), multiple vegetation pools, and soil thermal regimes. We found mean increases in net primary productivity (NPP) in all PFTs. Most notably, birch (Betula spp.) in the shrub tundra showed increases that were at least three times larger than any other PFT. Increases in NPP were positively related to increases in growing‐season length in the sedge tundra, but PFTs in boreal forest and shrub tundra showed a significant response to changes in light availability as well as growing‐season length. Significant NPP responses to changes in vegetation uptake of nitrogen by PFT indicated that some PFTs were better competitors for nitrogen than other PFTs. While NPP increased, heterotrophic respiration (RH) also increased, resulting in decreases or no change in net ecosystem carbon uptake. Greater aboveground biomass from increased NPP produced a decrease in summer albedo, greater regional heat absorption (0.34 ± 0.23 W·m−2·10 yr−1[mean ± SD]), and a positive feedback to climate warming. However, the decrease in albedo due to a shorter snow season (−5.1 ± 1.6 d/10 yr) resulted in much greater regional heat absorption (3.3 ± 1.24 W·m−2·10 yr−1) than that associated with increases in vegetation. Through quantifying feedbacks associated with changes in vegetation and those associated with changes in the snow season length, we can reach a more integrated understanding of the manner in which climate change may impact interactions between high‐latitude ecosystems and the climate system.
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Fire could slow regional warming through alteration of ecosystem energy balances by changing albedo.
“Alternatively, fire could slow regional warming through the alteration of ecosystem energy balances by changing albedo; for example, reduced tree cover exposes proportionally more snow, thus increasing reflectance (Randerson et al., 2006; Euskirchen et al., 2009).”
From The human dimension of fire regimes on Earth (2011) · cites this paper as Euskirchen et al., 2009
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BackgroundInfluentialSelf-citationWhat are the main climate drivers for shrub growth in Northeastern Siberian tundra
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UAV photogrammetry for mapping vegetation in the low-Arctic
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Evidence and implications of recent and projected climate change in Alaska's forest ecosystems
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Longer growing seasons do not increase net carbon uptake in the northeastern Siberian tundra
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Is Alaska's Boreal Forest Now Crossing a Major Ecological Threshold?
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Self-citationTemperature modulates intra-plant growth of Salix polaris from a high Arctic site (Svalbard)
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“…(Sturm et al. 2001; Tape et al. 2006; Forbes et al. 2010; Myers-Smith et al. 2011a; Natali et al. 2012), leading eventually to changes in the composition and structure of the arctic tundra (Chapin et al. 2005; Euskirchen et al. 2009; Elmendorf et al. 2012a) and increased carbon sequestration.”
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Missing pieces to modeling the Arctic-Boreal puzzle
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“Dwarf birch is predicted to increase in abundance and distribution under climate warming scenarios (de Groot & Wein, 1999; Bret-Harte et al., 2001; Euskirchen et al., 2009) and could enhance a positive feedback mechanism that would further increase wildfire in tundra ecosystems (Higuera et al.”
BackgroundSelf-citationRising plant‐mediated methane emissions from arctic wetlands
Andresen, C., Lara, M., Tweedie, C., & Lougheed, V. (2017) · Global Change Biology · doi:10.1111/gcb.13469 · Cited by 83
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“The length of the © 2015 John Wiley & Sons Ltd, Global Change Biology, 22, 208–219 snow season and opposing growing season is an important control on green-up, vegetation productivity, and carbon feedbacks to the climate system (Euskirchen et al., 2006, 2009).”
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Tundra vegetation change near Barrow, Alaska (1972–2010)
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An invasive wetland grass primes deep soil carbon pools
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“…temperatures are increasing the microbially active root zone in boreal and high-altitude peatlands (Updegraff et al., 2001; Pastor et al., 2003; Euskirchen et al., 2009; Koven et al., 2015), and higher levels of atmospheric CO2 are known to increase root growth at depth in shrubs and trees…”
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“In contrast, Euskirchen et al. (2009) chose to use 39 different PFTs to test predictions regarding the migration of arctic plant Global distributions of plant functional types are derived from remotely sensed land-cover data sets (DeFries et al., 1995, 2000; Jung et al., 2006).”
BackgroundIdentification of unrecognized tundra fire events on the north slope of Alaska
Jones, B. M., Breen, A. L., Gaglioti, B. V., Mann, D. H., Rocha, A. V., Grosse, G., Arp, C. D., Kunz, M. L., & Walker, D. A. (2013) · Journal of Geophysical Research Biogeosciences · doi:10.1002/jgrg.20113 · Cited by 81 · see citing works
“The apparent shift from sedge-dominated tundra to shrub-dominated tundra that we documented in the older burn sites could also have a positive feedback on climate warming due to the combination of a decrease in albedo and an increase in evapotranspiration associated with this transition [Euskirchen et al., 2009; Bonfi…”
BackgroundQin, Y., Yi, S., Ren, S., Li, N., & Chen, J.-J. (2014) · Environmental Earth Sciences · doi:10.1007/s12665-013-2547-0 · Cited by 74
“While climate warming benefits vegetation growth in high altitude areas (Yi et al. 2011b), it results in decreases or no change to the net ecosystem carbon uptake (Euskirchen et al. 2009).”
BackgroundSelf-citationHarms, T., Edmonds, J., Genet, H., Creed, I. F., Aldred, D., Balser, A., & Jones, J. B. (2016) · doi:10.1002/2015jg003201 · Cited by 71
“Large fluxes of dissolved materials link high-latitude catchments to coasts [Holmes et al., 2012; McGuire et al., 2009], where dissolved organic C (DOC) and N may fuel microbial respiration or stimulate productivity in the Arctic Ocean [Carmack et al., 2004; Holmes et al., 2008; Le Fouest et al.,…”
Ueyama, M., Ichii, K., Iwata, H., Euskirchen, E. S., Zona, D., Rocha, A. V., Harazono, Y., Iwama, C., NAKAI, T., & Oechel, W. C. (2013) · Journal of Geophysical Research Biogeosciences · doi:10.1002/jgrg.20095 · Cited by 81 · see citing works
“While the warming climate has increased vegetation productivity due to an increase in the length of the growing season in some areas [Euskirchen et al., 2006, 2009], warming has also stimulated respiration in other areas [Oechel et al., 1993, 2000; Ueyama et al., 2009; Hayes et al., 2011].”
BackgroundSelf-citationRosa, R. K., Oberbauer, S., Starr, G., Puma, I. P. L., Pop, E. W., Ahlquist, L., & Baldwin, T. A. (2015) · Global Change Biology · doi:10.1111/gcb.13040 · Cited by 69 · see citing works
Jiang, Y.-Y., Zhuang, Q., Schaphoff, S., Sitch, S., Sokolov, A., Kicklighter, D., & Melillo, J. (2012) · Ecology and Evolution · doi:10.1002/ece3.85 · Cited by 69
“Many other studies (Wilmking et al. 2004; Walker et al. 2006; Euskirchen et al. 2009) also emphasize the complexity of plant feedbacks to climate change, however the uncertainty is considerably high (Cox et al.”
BackgroundResultInfluentialEuskirchen, E. S., McGuire, A. D., Rupp, T. S., Chapin, F. S., & Walsh, J. E. (2009) · Journal of Geophysical Research Atmospheres · doi:10.1029/2009jg001095 · Cited by 59 · see citing works
“Recent work building on the study of Chapin et al. [2005] provides a transient analysis of how changes in vegetation and snow cover of northern Alaska are likely to influence atmospheric heating during the 21st century [Euskirchen et al., 2009].”
BackgroundResultInfluentialSelf-citationThe Holocene thermal maximum and late-Holocene cooling in the tundra of NE European Russia
Salonen, J. S., Seppä, H., Väliranta, M., Jones, V. J., Self, A. E., Heikkilä, M., Kultti, S., & Yang, H. (2011) · Quaternary Research · doi:10.1016/j.yqres.2011.01.007 · Cited by 68 · see citing works
“Tmjja was chosen as climate parameter as it roughly represents the temperature conditions during the growing season, including late spring, generally the most important single climate factor influencing the distribution, reproduction and growth of the plants in the arctic region (Hinzman et al., 2005; Euskirchen et al…”
BackgroundMethodFoster, A. C., Armstrong, A. H., Shuman, J. K., Shugart, H. H., Rogers, B. M., Mack, M. C., Goetz, S. J., & Ranson, K. J. (2019) · Ecological Modelling · doi:10.1016/j.ecolmodel.2019.108765 · Cited by 67 · see citing works
“Ecosystem modeling has been used across Alaska to investigate the response of vegetation to climate and fire using models such as ALFRESCO, TEM, and ecosys (Rupp et al., 2007; Euskirchen et al., 2009; Genet et al., 2013; Mekonnen et al., 2019).”
BackgroundMethodvan der Kolk, H., Heijmans, M., van Huissteden, J., Pullens, J. W. M., & Berendse, F. (2016) · Biogeosciences · doi:10.5194/bg-13-6229-2016 · Cited by 66 · see citing works
“Although several tundra vegetation models exist, these models do not take into account hydrological feedbacks, the formation of thaw ponds and vegetation–permafrost feedbacks or do not include mosses as separate plant functional type (e.g. Epstein et al., 2000; Wolf et al., 2008; Euskirchen et al., 2009).”
Alder Distribution and Expansion Across a Tundra Hillslope: Implications for Local N Cycling
Salmon, V., Breen, A., Kumar, J., Lara, M., Thornton, P., Wullschleger, S., & Iversen, C. (2019) · Frontiers in Plant Science · doi:10.3389/fpls.2019.01099 · Cited by 64 · see citing works
Shrub-tree interactions and environmental changes drive treeline dynamics in the Subarctic.
Grau, O., Ninot, J., Blanco-Moreno, J., van Logtestijn, R. V., Cornelissen, J., & Callaghan, T. (2012) · Oikos · doi:10.1111/j.1600-0706.2011.20032.x · Cited by 64 · see citing works
Fan, Z.-S., McGuire, A. D., Turetsky, M., Harden, J., Waddington, J. M., & Kane, E. S. (2013) · Global Change Biology · doi:10.1111/gcb.12041 · Cited by 61 · see citing works
“…of boreal SOC horizons play a critical role in regulating soil temperature and moisture dynamics as well as permafrost dynamics and net primary productivity (NPP), all of which, in turn, affect the dynamics of SOC and its physical properties (Euskirchen et al., 2009; Yi et al., 2009b, 2010).”
BackgroundSelf-citationDraining the Pool? Carbon Storage and Fluxes in Three Alpine Plant Communities
Sørensen, M. V., Strimbeck, R., Nystuen, K. O., Kapás, R. E., Enquist, B., & Graae, B. (2018) · Ecosystems · doi:10.1007/s10021-017-0158-4 · Cited by 60 · see citing works
Idiosyncratic Responses of High Arctic Plants to Changing Snow Regimes
Rumpf, S., Semenchuk, P., Dullinger, S., & Cooper, E. (2014) · PLoS ONE · doi:10.1371/journal.pone.0086281 · Cited by 58 · see citing works
“In contrast to the assumption for arctic ecosystems [12,26] a naturally earlier snowmelt and thus a longer growing season (Shallow) only resulted in an increased biomass for Stellaria in terms of average but for not for peak plant sizes.”
Feng, S., Ho, C.-H., Hu, Q., Oglesby, R., Jeong, S., & Kim, B.-M. (2012) · Climate Dynamics · doi:10.1007/s00382-011-1020-6 · Cited by 58 · see citing works
“2007), the Terrestrial Ecosystem Model (TEM, McGuire et al. 2000; Thompson et al. 2005; Euskirchen et al. 2009), the BIOME-BGC model (Engstrom et al.”
MethodClimate and Conservation: Landscape and Seascape Science, Planning, and Action
Hilty, J., Chester, C. C., & Cross, M. S. (2012) · Island Press/Center for Resource Economics eBooks · doi:10.5822/978-1-61091-203-7 · Cited by 57 · see citing works
“Finally, there is increasing evidence of the “invasion” of boreal fauna and flora into the Arctic environs (Euskirchen et al. 2009; Martin et al. 2009; Post et al. 2009).”
BackgroundInfluentialBarrio, I., Lindén, E., Beest, M. T., Olofsson, J., Rocha, A., Soininen, E., Alatalo, J., Andersson, T., Asmus, A. L., Boike, J., et al. (2017) · Polar Biology · doi:10.1007/s00300-017-2139-7 · Cited by 56 · see citing works
“2016); further, the range and abundance of dwarf birch are 172 predicted to expand in response to warming (Euskirchen et al. 2009; Myers-Smith et al. 2011).”
BackgroundClimate change risk to forests in China associated with warming
Yin, Y.-H., Ma, D., & Wu, S.-H. (2018) · Scientific Reports · doi:10.1038/s41598-017-18798-6 · Cited by 54 · see citing works
Salonen, J. S., Ilvonen, L., Seppä, H., Holmström, L., Telford, R., Gaidamavičius, A., Stančikaitė, M., & Subetto, D. (2012) · doi:10.1177/0959683611425548 · Cited by 54
“Tmjja was chosen as the climate parameter as it roughly represents the temperature conditions during the growing season, including late spring, generally the most important single climate factor influencing the distribution, reproduction and growth of the plants in the arctic region (Euskirchen et al., 2009; Hinzman e…”
BackgroundMethodAbove‐ and below‐ground plant biomass response to experimental warming in northern Alaska
Hollister, R. D., & Flaherty, K. J. (2010) · Applied Vegetation Science · doi:10.1111/j.1654-109x.2010.01079.x · Cited by 54 · see citing works
Self‐Amplifying Feedbacks Accelerate Greening and Warming of the Arctic
Zhang, W.-X., Miller, P., Jansson, C., Samuelsson, P., Mao, J., & Smith, B. (2018) · Geophysical Research Letters · doi:10.1029/2018gl077830 · Cited by 50
“Euskirchen et al. (2009) used a terrestrial ecosystem model driven with climate fields generated from three GCMs (CSIRO2, HadCM3, and PCM) following the IPCC Special Report: Emissions Scenarios (SRES) A2 scenario to estimate the maximum decline in summer albedo, which was approximately 0.02 in…”
MethodInfluentialLeaf and fine root carbon stocks and turnover are coupled across Arctic ecosystems
Sloan, V., Fletcher, B. J., Press, M., Williams, M., & Phoenix, G. (2013) · Global Change Biology · doi:10.1111/gcb.12322 · Cited by 50 · see citing works
“There is considerable need to quantify the stocks of carbon held within plant communities and the rates at which those stocks are cycled, both for predicting and modelling Arctic ecosystem responses to climate change, and for determining ecosystem feedbacks to climate (Euskirchen et al., 2009).”
BackgroundFeedbacks and Interactions: From the Arctic Cryosphere to the Climate System
Callaghan, T., Johansson, M., Key, J., Prowse, T., Ananicheva, M., & Klepikov, A. (2011) · Ambio · doi:10.1007/s13280-011-0215-8 · Cited by 50 · see citing works
“Furthermore, a decrease in albedo resulting from a decrease in snow cover over land may result in a further change in albedo through a change in the vegetation in response to surface warming (Chapin et al. 2005; Euskirchen et al. 2009).”
BackgroundHistorical and projected trends in landscape drivers affecting carbon dynamics in Alaska.
Pastick, N., Duffy, P., Genet, H., Rupp, T., Wylie, B., Johnson, K., Jorgenson, M., Bliss, N., McGuire, A., Jafarov, E. E., et al. (2017) · Ecological Applications · doi:10.1002/eap.1538 · Cited by 48
Self-citationPark, H., Launiainen, S., Konstantinov, P., Iijima, Y., & Fedorov, A. (2018) · Journal of Geophysical Research - Biogeosciences · doi:10.1029/2018jg004491 · Cited by 47
Euskirchen, E., Bennett, A., Breen, A., Genet, H., Lindgren, M. A., Kurkowski, T. A., McGuire, A., & Rupp, T. S. (2016) · doi:10.1088/1748-9326/11/10/105003 · Cited by 47
“We use the environmental module of DOS-TEM to estimate the changes in the timing of snowmelt, snow return, and the duration of the snow season with methodology previously implemented in Euskirchen et al (2006, 2007, 2009a, 2009b).”
BackgroundMethodInfluentialSelf-citationFang, O.-Y., Wang, Y., & Shao, X. (2016) · Trees · doi:10.1007/s00468-015-1300-6 · Cited by 47
“1996), model simulations (Euskirchen et al. 2009; Stinson et al. 2011; Tian et al. 2010), and remote sensingbased estimation (Running et al.”
Williamson, S., Barrio, I., Hik, D., & Gamon, J. (2016) · Global Change Biology · doi:10.1111/gcb.13297 · Cited by 46 · see citing works
“in particular are likely to thrive in a warmer Arctic (Euskirchen et al., 2009; Heskel et al., 2013).”
BackgroundInfluentialGamon, J., Kershaw, G., Williamson, S., & Hik, D. (2012) · doi:10.1088/1748-9326/7/1/015502 · Cited by 46
“…on larger ecosystem, landscape and atmospheric processes through altered energy balance and gas exchange (Callaghan et al 2004, Cutler 2011, Euskirchen et al 2009, Sturm et al 2005, Swann et al 2010), so an additional hypothesis is that vegetation change or stability can, in itself, lead…”
BackgroundFour decades of plant community change in the Alpine tundra of southwest Yukon, Canada
Danby, R. K., Koh, S., Hik, D. S., & Price, L. W. (2011) · AMBIO · doi:10.1007/s13280-011-0172-2 · Cited by 45 · see citing works
“Significant changes in both diversity and above-ground biomass have been associated with recent warming of both high Arctic (e.g., Hudson et al. 2010) and low Arctic (e.g., Euskirchen et al. 2009) sites.”
BackgroundLin, D., Johnson, D., Andresen, C., & Tweedie, C. (2012) · Environmental Research Letters · doi:10.1088/1748-9326/7/2/025502 · Cited by 45 · see citing works
“…(e.g. Villarreal et al 2012), experimental manipulations (Hollister et al 2005, Johnson et al 2011b), remote sensing (Bhatt et al 2010, Jia et al 2003), and modeling (Euskirchen et al 2009), it is not surprising that land cover change was documented in all of the landscapes investigated.”
BackgroundTwenty-Five Year Record of Changes in Plant Cover on Tundra of Northeastern Alaska
Jorgenson, J., Raynolds, M., Reynolds, J., & Benson, A.-M. (2015) · Arctic Antarctic and Alpine Research · doi:10.1657/aaar0014-097 · Cited by 44 · see citing works
“…unexpected because of the exuberance with which that species sometimes responds to tundra warming experiments (BretHarte et al., 2001) and the large shrub birch increases predicted to occur with climate change in northern Alaska by integrated ecosystem models, such as in Euskirchen et al. (2009).”
BackgroundSulman, B., Salmon, V., Iversen, C., Breen, A., Yuan, F., & Thornton, P. (2021) · Journal of Advances in Modeling Earth Systems · doi:10.1029/2020ms002396 · Cited by 43 · see citing works
“For example, the TEM model (Euskirchen et al., 2009) was designed specifically for improved representation of high-latitude processes.”
BackgroundMethodZhu, X.-D., Zhuang, Q.-L., Gao, X., Sokolov, A., & Schlosser, C. (2013) · Environmental Research Letters · doi:10.1088/1748-9326/8/4/045003 · Cited by 43 · see citing works
Grant, R., Humphreys, E., Lafleur, P., & Dimitrov, D. D. (2011) · doi:10.1029/2010jg001555 · Cited by 43
“…some earlier modeling studies indicate that rises in NPP from warmer and longer growing seasons under higher Ca will be offset by rises in Rh from warmer soils, causing little change or small declines in NEP from current values [Euskirchen et al., 2009; Grant et al., 2003; Zhuang et al., 2006].”
BackgroundResultVariability in the expansion of trees and shrubs in boreal Alaska.
Brodie, J., Roland, C., Stehn, S., & Smirnova, E. (2019) · Ecology · doi:10.1002/ecy.2660 · Cited by 42
Trugman, A., Fenton, N., Bergeron, Y., Xu, X.-T., Welp, L., & Medvigy, D. (2016) · doi:10.1002/2015ms000576 · Cited by 42
“Models of forests in Alaska and central Canada have incorporated dynamic organic layer accumulation [Bona et al., 2016; Carrasco et al., 2006; Yi et al., 2010; Zhuang et al., 2002], NA boreal-specific tree types, and dynamic vegetation [Euskirchen et al., 2014; Euskirchen et al., 2009].”
BackgroundPlant and Vegetation Dynamics on Disko Island, West Greenland: Snapshots Separated by Over 40 Years
Callaghan, T., Christensen, T., & Jantze, E. (2011) · Ambio · doi:10.1007/s13280-011-0169-x · Cited by 42 · see citing works
“…more important future changes that will reinforce modern trends of major loss of biodiversity (Butchart et al. 2010) and projections of plant community change in the Arctic (Kaplan et al. 2003; Sitch et al. 2003; Callaghan et al. 2005; Kaplan and New 2006; Wolf et al. 2008; Euskirchen et al. 2009).”
Background
- Authors
- Euskirchen, E. S., McGuire, A. D., Chapin, F. S., Yi, S., & Thompson, C. C.
- Affiliations
- University of Alaska Fairbanks (US)
- United States Geological Survey (US)
- National Park Service (US)
- Corresponding author
- Euskirchen, E. S.
- Venue
- Ecological Applications
- Publisher
- Wiley
- Published
- 2009-06
- Volume
- 19
- Issue
- 4
- Pages
- 1022-1043
- ISSN
- 1051-0761 (ISSN-L)
- 1939-5582
- OpenAlex
- W2168947040
- Cited by
- 237
- References
- 0
- Citations by year
- 2026: 3 · 2025: 9 · 2024: 8 · 2023: 19 · 2022: 7 · 2021: 22 · 2020: 5 · 2019: 9 · 2018: 10 · 2017: 13 · 2016: 19 · 2015: 15 · 2014: 15 · 2013: 22 · 2012: 21
- FWCI
- 12.58
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Ecological Applications (publishedVersion)
- PubMed (publishedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Climate change and permafrost
- Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil Carbon and Nitrogen Dynamics
- Physical Sciences › Environmental Science › Global and Planetary Change › Plant Water Relations and Carbon Dynamics
- Keywords
- climate change scenarios, plant functional types, net primary productivity, shrub tundra, boreal forest, Betula, albedo feedback, heat absorption, heterotrophic respiration, nitrogen uptake, climate feedbacks, northern Alaska, Terrestrial Ecosystem Model, growing season length, light availability, aboveground biomass
- MeSH terms
- Alaska, Arctic Regions, Carbon, Nitrogen, Plants, Seasons, Snow, Soil, Sunlight, Greenhouse Effect, Ecosystem, Cell Respiration, Plant Development
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