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Scientific personnel
K. Walter (INE), G. Grosse (GIPL),
M. Edwards (Dep. of Natural Sciences, UAF / University of Southampton,
UK), L. Slater (Rutgers University), L. Plug (Dalhousie University,
Canada)
This project is funded through the International Polar Year Program
of the National Science Foundation (NSF).
Project duration: 2008-2011

Project Summary
The proposed research integrates field studies in a range of disciplines
(geomorphology, geophysics, paleoecology, hydrology, limnology)
with process modeling of permafrost thaw, lake formation, carbon
cycling, and greenhouse gas (GHG) emissions to understand how permafrost
degradation in the Arctic, particularly thermokarst-lake (TKL) evolution,
affects long-term atmospheric trace gas dynamics by releasing ancient
carbon (C) stored in permafrost as carbon dioxide (CO2) and methane
(CH4). The overarching goals of the IPY/NSF solicitation are met
in the short term (2007-2009), by (1) describing comprehensively
the state of thermokarst (permafrost degradation) in Siberia and
Alaska, (2) quantifying its impact on landscape configuration through
the alteration of surface geomorphology and drainage patterns, (3)
estimating its impacts on the C cycle via enhanced GHG (CO2, CH4)
emissions, and (4) examining its potential to influence global climate
-potential C release from thawing permafrost in Siberia alone totals
>50% of the current atmospheric C burden. The IPY goals are met
in the long term by establishing (1) a legacy of geographic, stratigraphic
and process data from permafrost regions and data on thermokarst
dynamics (past, present and future), (2) a working model of thermokarst
processes, (3) scenarios of thermokarst-GHG emissions driven by
climate change from the Last Glacial Maximum (LGM) to the year 2200,
and (4) an enhancement of collaborations within the Arctic Observing
Network at observatories in North Siberia (Cherskii) and Alaska
(Toolik Lake), and work with international collaborators at Bristol
University (UK), the Alfred Wegener Institute for Polar and Marine
Research and the Max Planck Institute for Microbiology (both Germany)
and the Permafrost Institute, Yakutsk (Russia). The project will
be integrated with other IPY certified projects: "Permafrost
Observatories: Thermal State of Permafrost (ID 50)", "Arctic
Circum-Polar Coastal Observatory Network (ID 90)", and "Carbon
Pools in Permafrost Regions (ID 373)".

Fieldwork
We started with fieldwork on the Seward Peninsula, Alaska, in July
2008. We will have extended fieldwork during a second, third, and
a fourth expedition to the Seward Peninsula in August and October
2008 and April 2009. Our fieldwork for this project includes sediment
sampling of thermokarst basin and lakes, geophysical surveys, DGPS
surveys, sedimentological and biogeochemical studies, and paleoenvironmental
analyses.

Publications resulting from this
project
- Schirrmeister L, Meyer H, Wetterich S, Siegert C, Kunitsky VV,
Grosse G, Kuznetsova TV, Derevyagin AYu (2008): The Yedoma Suite
of the Northeastern Siberian Shelf Region: Characteristics and
Concept of Formation. In: 'Ninth International Conference on Permafrost',
Kane DL & Hinkel KM (eds), Institute of Northern Engineering,
University of Alaska Fairbanks, pp. 1595-1600.
- Schirrmeister L, Grosse G, Kunitsky V, Magens D, Meyer H, Derivyagin
A, Kuznetsova T, Andreev A, Kienast F, Grigoriev M, Preusser F
(2008): Periglacial landscape evolution and environmental changes
of Arctic lowland areas during the Late Quaternary (Western Laptev
Sea coast, Cape Mamontov Klyk). Polar Research, 27(2): 249 - 272.

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