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Title: DOE Final Report on Collaborative Research. Quantifying Climate Feedbacks of the Terrestrial Biosphere under Thawing Permafrost Conditions in the Arctic

Technical Report ·
DOI:https://doi.org/10.2172/1224739· OSTI ID:1224739
 [1];  [2];  [3];  [4];  [3];  [2]
  1. Purdue Univ., West Lafayette, IN (United States)
  2. Massachusetts Inst. of Technology (MIT), Cambridge, MA (United States)
  3. Marine Biological Lab. (MBL), Woods Hole, MA (United States)
  4. Univ. of Alaska, Fairbanks, AK (United States)

Our overall goal is to quantify the potential for threshold changes in natural emission rates of trace gases, particularly methane and carbon dioxide, from pan-arctic terrestrial systems under the spectrum of anthropogenically-forced climate warming, and the conditions under which these emissions provide a strong feedback mechanism to global climate warming. This goal is motivated under the premise that polar amplification of global climate warming will induce widespread thaw and degradation of the permafrost, and would thus cause substantial changes to the landscape of wetlands and lakes, especially thermokarst (thaw) lakes, across the Arctic. Through a suite of numerical experiments that encapsulate the fundamental processes governing methane emissions and carbon exchanges – as well as their coupling to the global climate system - we intend to test the following hypothesis in the proposed research: There exists a climate warming threshold beyond which permafrost degradation becomes widespread and stimulates large increases in methane emissions (via thermokarst lakes and poorly-drained wetland areas upon thawing permafrost along with microbial metabolic responses to higher temperatures) and increases in carbon dioxide emissions from well-drained areas. Besides changes in biogeochemistry, this threshold will also influence global energy dynamics through effects on surface albedo, evapotranspiration and water vapor. These changes would outweigh any increased uptake of carbon (e.g. from peatlands and higher plant photosynthesis) and would result in a strong, positive feedback to global climate warming.

Research Organization:
Purdue Univ., West Lafayette, IN (United States)
Sponsoring Organization:
USDOE Office of Science (SC), Biological and Environmental Research (BER)
DOE Contract Number:
SC0007007
OSTI ID:
1224739
Report Number(s):
DOE-Purdue-SC0007007-1
Country of Publication:
United States
Language:
English

References (8)

The impacts of recent permafrost thaw on land–atmosphere greenhouse gas exchange journal April 2014
Potential influence of climate-induced vegetation shifts on future land use and associated land carbon fluxes in Northern Eurasia journal March 2014
Insights and issues with simulating terrestrial DOC loading of Arctic river networks journal December 2013
Contrasting soil thermal responses to fire in Alaskan tundra and boreal forest: Contrasting soil thermal responses journal February 2015
Arctic lakes are continuous methane sources to the atmosphere under warming conditions journal May 2015
Evapotranspiration in Northern Eurasia: Impact of forcing uncertainties on terrestrial ecosystem model estimates journal April 2015
Response of evapotranspiration and water availability to the changing climate in Northern Eurasia journal August 2014
Response of evapotranspiration and water availability to changing climate and land cover on the Mongolian Plateau during the 21st century journal September 2013