Award Abstract # 0943799
Impact of Recent Climate Warming on Active-Layer Dynamics, Permafrost, and Soil Properties on the Western Antarctic Peninsula

NSF Org: OPP
Office of Polar Programs (OPP)
Recipient: UNIVERSITY OF WISCONSIN SYSTEM
Initial Amendment Date: September 15, 2010
Latest Amendment Date: August 8, 2014
Award Number: 0943799
Award Instrument: Continuing Grant
Program Manager: Michael E. Jackson
OPP
 Office of Polar Programs (OPP)
GEO
 Directorate for Geosciences
Start Date: September 15, 2010
End Date: August 31, 2015 (Estimated)
Total Intended Award Amount: $592,315.00
Total Awarded Amount to Date: $592,315.00
Funds Obligated to Date: FY 2010 = $301,305.00
FY 2011 = $291,010.00
History of Investigator:
  • James Bockheim (Principal Investigator)
    bockheim@wisc.edu
Recipient Sponsored Research Office: University of Wisconsin-Madison
21 N PARK ST STE 6301
MADISON
WI  US  53715-1218
(608)262-3822
Sponsor Congressional District: 02
Primary Place of Performance: University of Wisconsin-Madison
21 N PARK ST STE 6301
MADISON
WI  US  53715-1218
Primary Place of Performance
Congressional District:
02
Unique Entity Identifier (UEI): LCLSJAGTNZQ7
Parent UEI:
NSF Program(s): ANT Earth Sciences
Primary Program Source: 0100CYXXDB NSF RESEARCH & RELATED ACTIVIT
0100XXXXDB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 0000, OTHR
Program Element Code(s): 511200
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.078

ABSTRACT

Intellectual Merit:
The seasonal thaw layer, permafrost distribution and temperature, and soil properties are key indicators of climate change that have been under-utilized in Antarctica. The PI proposes to install two Circumpolar Active Layer Monitoring (CALM-S) stations and permafrost boreholes on Anvers (64.7°S) and Brabant Islands (64.25°S) to link with existing stations maintained by Portugal, Spain, and Italy on Adelaide (67.57°S), Deception (63.0°S), Livingston (62.50°S), King George (62.18°S), and Signy (60.70°S) Islands. In addition, they propose to examine soils along this latitudinal/climatic gradient to construct a carbon budget for the Antarctic Peninsula. The working hypothesis is that permafrost distribution and temperatures on the West Antarctic Peninsula are strongly influenced by the spatial extent of sea ice in the Southern Ocean, and that the active-layer thickness and permafrost temperatures are increasing at a measurable rate in the study areas. The PIs predict that although soils of the Antarctic Peninsula and offshore islands comprise only 20% of the ice-free area of Antarctica, they will account for more than 80% of the soil organic carbon. Continued warming could stimulate a positive feedback mechanism whereby additional CO2 will be released to the atmosphere as soil organic carbon exposed by thickening of the active layer decomposes. The project will construct and test a mechanistic model that includes ground temperature and climate data, snow cover, a digital elevation model in conjunction with the multi-national PERMANTAR group, slope angle and aspect, and net radiation for predicting the occurrence and the fate of permafrost along the WAP.

Broader impacts:
This project will foster international research among six countries. The project has direct links with the pole-to-pole CALM network, the Global Terrestrial Network for Permafrost (GTN-P), and the SCAR- supported Antarctic Permafrost and Periglacial Environments (ANTPAS) group, and WILL formalize a latitudinal gradient in the most climatically sensitive zone of Antarctica. The research could provide information to help better understand potential rapid climatic changes. The study not only will provide baseline terrestrial data in an area where the focus of U.S. activities has been predominantly on marine ecosystems, but will also take advantage of the extensive Palmer LTER dataset on sea-ice dynamics. The study will train two graduate students and several undergraduates. Outreach activities will focus on school children and will include ?Diary from Antarctic Permafrost Scientists? on the Internet, videoconferencing from the field, and a ?scientist goes to school? initiative for Dane County, WI.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Bockheim, James "Distribution, properties and origin of viscous-flow features in the McMurdo Dry Valleys, Antarctica" Geomorphology , v.204 , 2014 , p.114
Bockheim, James "Soil formation in the Transantarctic Mountains from the middle Paleozoic to the Anthropocene" Palaeogeography, Palaeoclimatology, Palaeoecology , v.382 , 2013 , p.98
Bockheim, James, and McLeod, Malcom "Glacial geomorphology of the Victoria Valley system, Ross Sea Region, Antarctica" Geomorphology , v.193 , 2013 , p.14
Bockheim, J.G. "Paleosols in the Transantarctic Mountains: indicators of environmental change" EGU Solid Earth , v.5 , 2013 , p.1007 doi:10.5194/sed-5-1007-2013
Bockheim, J.G. "Soil formation in the Transantarctic Mountains from the middle Paleozoic to the Anthropocene." Palaeogeography, Palaeoclimatology, Palaeoecology , v.381-382 , 2013 , p.98 doi.org/10.1016/j.palaeo.2013.04.019
Bockheim, J.G., McLeod, M. "Glacial geomorphology of the Victoria Valley system, Ross Sea Region, Antarctica." Geomorphology , v.183 , 2013 , p.14 doi.org/10.1016/j.geomorph.2013.03.020
Bockheim, J.G., Vieira, G., et al. "Climate warming and permafrost dynamics on the Antarctic Peninsula." Global & Planetary Change , v.100 , 2013 , p.215

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

The mean annual air temperature is warmer (-1.7 to -3.2C) along the western Antarctic Pensinsula in 2011-2014 than in the more northerly latitudes of the South Shetland Islands. The shallow boreholes at Amsler Island near Palmer Station and Cierva Point show no permafrost in the upper 1-2 m but soil temperatures vary considerably based on aspect, elevation, and vegetation. Deep boreholes suggest that permafrost begins at about 6-7 m at Cierva Point (64.15?S, 60.95?W) but is at 9-10 m at Amsler Island near Palmer Station (64.76?S, 64.07?W), much deeper than in the South Shetland Islands, where it is 0.8 to 3.0 m. The soils at the two sites are very young, having been formed following recent deglaciation. They can be classifed into four groups: (1) non-acidic mineral, (2) strongly acidic mineral, (3) abundant soil organic matter under mosses, and (4) strongly influenced by penguins and other avians. The non-acidic mineral soils are nearest the glacial margin and have undergone the least amount of development. The strongly acidic soils have undergone acidification from avian occupation. The soils under mosses have the greatest amount of soil carbon. Soils in group 4 show considerable weathering based on acidity, accumulation of phosphorus and organic matter, and depletion of base cations (Ca, Mg).

 


Last Modified: 09/04/2015
Modified by: James G Bockheim