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International Polar Year
IPY 2007-2008
 
 
Updated on 05/01/2009
 
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Expressions of Intent for IPY 2007-2008 Activities

Expression of Interest Details

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PROPOSAL INFORMATION

(ID No: 882)

PErmafrost and Carbon Emissions (PEACE)  (PEACE)

Outline
The goal is to explore the climate vulnerability to a positive feedback associated with possible release of Carbon containing gases from within and under the thawing permafrost in a warmer climate scenario. Existing estimates of Carbon content in soils within the permafrost regions are of order of 400 PgC. Climate warming by 2oC scenarios and associated possible 25% reduction in the near-surface permafrost may result in a release of up to 100 PgC into the atmosphere, which would exert a large impact on the rate of global warming. The project will examine current distribution of the permafrost and seasonally frozen soils and assess current quality and quantity of Carbon in frozen soils, the near-surface permafrost, and the extensive peatlands within and adjacent to permafrost regions of Planet Earth. This will enable preliminary estimates of current Carbon fluxes from regions of underlain by permafrost and containing seasonally frozen soil. The project will consider several processes which are expected to control Carbon dynamics in thawing permafrost. This will involve biogeochemical modelling and experimentation using data from flux towers and chamber techniques. The scope of the land surface models will be extended to include permafrost dynamics under a warming climate. Where possible, these models will be extended to include hydrological processes. Vegetation change and associated Carbon dynamics will also be considered. The project will conclude with a series of experiments with Earth System models that will more fully represent the climate warming – permafrost - Carbon feedback with best possible account of biogeochemical and hydrological processes. This will reveal warming potential associated with Carbon stocks currently fully or partially isolated from the atmosphere by permafrost and/or frozen soil.Summary of Activities: 1. Spatial Distribution Carbon Stocks Assoicated with Permafrost• Refine existing digital databases of spatial distribution• Re-assessment of current soil carbon content in frozen soils and peatlands (including below 1-2 m depth)• Assessment of southern boundary of permafrost changes 2. Carbon Processes• Development of biogeochemical modeling of C dynamics in thawing permafrost with emission trajectories:– Review of processes controlling carbon emissions in thawing permafrost – Current fluxes and controlling processes (eddy-covariance measurements) 3. Climate Impacts (100 years time frame)• Off-line calculations of carbon emissions impacts on climate change.• Work with Earth System models including permafrost models (eg, GCMs) to bring critical elements of permafrost dynamics, hydrological, and carbon cycle components into model development to explore feedbacks to climate.

Theme(s)   Major Target
The current state of the polar environment
Change in the polar regions
Polar-global linkages and teleconnections
The human dimension in polar regions
  Natural or social sciences research

What significant advance(s) in relation to the IPY themes and targets can be anticipated from this project?
Theme 1: Assessment of current Carbon stocks within the permafrost and seasonally frozen soils.Theme 2: Estimates of additional warming associated with the role of Carbon in permafrost regions.Theme 3: Global climate warming potential associated with Carbon stocks isolated by permafrost and seasonally frozen soils

What international collaboration is involved in this project?
The project will be executed in collaboration between the Global Carbon Project, the World Climate Research Programme Climate and Cryosphere project and the International Permafrost Association. The project will be linked to COSMOS activities.


FIELD ACTIVITY DETAILS

Geographical location(s) for the proposed field activities:
Permafrost (perennially frozen ground) may occur where the mean annual air temperature is less than –1°C and is generally continuous where it is less than –7°C. It is estimated that permafrost regions occupy a quarter of the Earth’s ice free area. Methane emissions from the Arctic continental shelves where relict permafrost exists is another potential source regi

Approximate timeframe(s) for proposed field activities:
Arctic: The activities should commence before the IPY and be concluded during the IPY period.            
Antarctic: n/a

Significant facilities will be required for this project:
No significant logistics envisaged. If existing, new and representative remote sites for flux measurements and aircraft observations are involved, the project may required additional support.

Will the project leave a legacy of infrastructure?
None anticipated. However, field sites from which data are utilized might become part of long-term observatories (Flagship Observatories). For instance in the U.S. Barrow and the Toolik LTER site are currently under consideration, a Canadian network is proposed, and the Abisko Research Station in Sweden has a long tradition of flux studies.

How is it envisaged that the required logistic support will be secured?
Own national polar operator
Another national polar operator
National agency
Own support
Other sources of support

Further details: Flux sites will require logistics

Has the project been "endorsed" at a national or international level?
Yes. The draft proposal was considered and approved by the First Session of the CliC Scientific Steering Group (Hobart, Australia, October 2004). The Global Carbon Project has identified the permafrost-carbon-climate feedback as a critical vulnerability of the Earth System and made it a research priority (GCP 2003. A framework for Internationally Coordinated Research of the Global Carbon Cycle, ESSP Report No. 1).


PROJECT MANAGEMENT AND STRUCTURE

Is the project a short-term expansion (over the IPY 2007-2008 timeframe) of an existing plan, programme or initiative or is it a new autonomous proposal?
Yes
PEACE will be a subproject of the Global Carbon Project, WCRP CliC Project, and several activities of the International Permafrost Association. Coordination with the International Arctic Science Committee (IASC) project C-FATE: Carbon stock, carbon cycling and trace gas flux studies and the IASC ICARP II conference in November 2005 will be developed.

How will the project be organised and managed?
The project will have a leader, a small Steering Committee, links to several research groups and international programmes (GCP, CliC, IPA etc); including peatland projects. The project proposal will be amended and agreed by all the participants.

What are the initial plans of the project for addressing the education, outreach and communication issues outlined in the Framework document?
Results from the project will be published in scientific literature and this information can be used in the learning process. Graduate students and post docs will participate in many project activities

What are the initial plans of the project to address data management issues (as outlined in the Framework document)?
Data management practices will comply with requirements set out by the IPY Framework.

How is it proposed to fund the project?
A request for funding will be prepared and submitted to ICSU. Other sources of funding will be sough

Is there additional information you wish to provide?
Numerical experimentation of PEACE may affect IPCC scenarios. The activities related to stocks will rely on recently completed GIS-based projects from West Siberia (Sheng, Smith, MacDonald et al.) and the Usa Basin (Kuhry and Mazhitova) to update carbon stocks in permafrost and peatland regions of Russia and Canadian estimates by Tarnocai..


PROPOSER DETAILS

Director, Global Carbon Project Pep Canadell
Earth Observation Center
CSIRO Division of Atmospheric Research
GPO Box 4023, Canberra
ACT 2601
Australia

Tel: 61 2 6246 5631
Mobile:
Fax: 61 2 6246 5988
Email:

Other project members and their affiliation

Name   Affiliation
Barry Goodison   Environment Canada; barry.goodison@ec.gc.ca
Douglas Kane   University of Alaska at Fairbanks, USA; ffdlk@uaf.edu
Jerry Brown   International Permafrost Association; jerrybrown@igc.org
Tetsuo Ohato   CliC Project Area 1 and JAMSTEC, Japan; ohata@jamstec.jp
Vladimir Romanovsky   University of Alaska at Fairbanks; ffven@uaf.edu
Charles Tarnocai   Agriculture and Agri-Food, Canada; tarnocaict@agr.gc.ca

Other Information

Sergei Zimov, Pacific Institute of Geography, Russian Academy of Sciences; sazimov@cher.sakha.ru Christopher Field, Carnegie Institute of Washington, Stanford, CA, USA; chris@globalecology.stanford.edu Philippe Ciais, Commissariat a L'Energie Atomique; philippe.ciais@cea.fr Peter Cox, Hadley Center, UK, Peter.Cox@metoffice.com Guy Brasseur, Daniela Jacob,Max-Planck Institute for Meteorology, Germany; brasseur@dkrz.dejacob@dkrz.de Peter Kuhry,University of Stockholm, Sweden; peter.kuhry@natgeo.su.se Glen MacDonald; Univerisity of California, Los Angeles;macdonal@geog.ucla.edu Torben Christensen; Lund University, Sweden; torben.christensen@nateko.lu.se Tatiana Khromova Institute of Geography, Russian Ac. Sci., Russia;glacgis@orc.ru



 
   
   
 
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