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Multi-decadal changes in tundra environments and ecosystems: synthesis of the International Polar Year-Back to the Future project (IPY-BTF)
Authors:Callaghan Terry V  Tweedie Craig E  Akerman Jonas  Andrews Christopher  Bergstedt Johan  Butler Malcolm G  Christensen Torben R  Cooley Dorothy  Dahlberg Ulrika  Danby Ryan K  Daniëls Fred J A  de Molenaar Johannes G  Dick Jan  Mortensen Christian Ebbe  Ebert-May Diane  Emanuelsson Urban  Eriksson Håkan  Hedenås Henrik  Henry H R Greg  Hik David S  Hobbie John E  Jantze Elin J  Jaspers Cornelia  Johansson Cecilia  Johansson Margareta  Johnson David R  Johnstone Jill F  Jonasson Christer  Kennedy Catherine  Kenney Alice J  Keuper Frida  Koh Saewan  Krebs Charles J  Lantuit Hugues  Lara Mark J  Lin David  Lougheed Vanessa L
Affiliation:Royal Swedish Academy of Sciences, Stockholm. terry_callaghan@btinternet.com
Abstract:Understanding the responses of tundra systems to global change has global implications. Most tundra regions lack sustained environmental monitoring and one of the only ways to document multi-decadal change is to resample historic research sites. The International Polar Year (IPY) provided a unique opportunity for such research through the Back to the Future (BTF) project (IPY project #512). This article synthesizes the results from 13 papers within this Ambio Special Issue. Abiotic changes include glacial recession in the Altai Mountains, Russia; increased snow depth and hardness, permafrost warming, and increased growing season length in sub-arctic Sweden; drying of ponds in Greenland; increased nutrient availability in Alaskan tundra ponds, and warming at most locations studied. Biotic changes ranged from relatively minor plant community change at two sites in Greenland to moderate change in the Yukon, and to dramatic increases in shrub and tree density on Herschel Island, and in subarctic Sweden. The population of geese tripled at one site in northeast Greenland where biomass in non-grazed plots doubled. A model parameterized using results from a BTF study forecasts substantial declines in all snowbeds and increases in shrub tundra on Niwot Ridge, Colorado over the next century. In general, results support and provide improved capacities for validating experimental manipulation, remote sensing, and modeling studies.
Keywords:IPY   Glaciers   Permafrost   Snow stratigraphy   Tundra vegetation   Limnology   Shrubs   Treeline
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