Award Abstract # 0632310
Collaborative Research: IPY: POLENET/Greenland: Using Bedrock Geodesy to Constrain Past and Present Day Changes in Greenland Ice Mass

NSF Org: OPP
Office of Polar Programs (OPP)
Recipient: THE RESEARCH FOUNDATION FOR THE STATE UNIVERSITY OF NEW YORK
Initial Amendment Date: June 21, 2007
Latest Amendment Date: July 9, 2009
Award Number: 0632310
Award Instrument: Continuing Grant
Program Manager: William J. Wiseman, Jr.
OPP
 Office of Polar Programs (OPP)
GEO
 Directorate for Geosciences
Start Date: July 1, 2007
End Date: June 30, 2011 (Estimated)
Total Intended Award Amount: $204,762.00
Total Awarded Amount to Date: $204,762.00
Funds Obligated to Date: FY 2007 = $58,623.00
FY 2008 = $81,547.00

FY 2009 = $64,592.00
History of Investigator:
  • Beata Csatho (Principal Investigator)
    bcsatho@buffalo.edu
Recipient Sponsored Research Office: SUNY at Buffalo
520 LEE ENTRANCE STE 211
AMHERST
NY  US  14228-2577
(716)645-2634
Sponsor Congressional District: 26
Primary Place of Performance: SUNY at Buffalo
520 LEE ENTRANCE STE 211
AMHERST
NY  US  14228-2577
Primary Place of Performance
Congressional District:
26
Unique Entity Identifier (UEI): LMCJKRFW5R81
Parent UEI: GMZUKXFDJMA9
NSF Program(s): ANS-Arctic Natural Sciences
Primary Program Source: 0100CYXXDB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 0000, 1079, 5295, OTHR
Program Element Code(s): 528000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.078

ABSTRACT

ABSTRACT
Bevis
OPP-0632320
Csatho
OPP-0632310

Intellectual Focus. This is a collaborative proposal from Principal Investigators at Ohio State University and SUNY Buffalo. They will construct a network (GNET) of continuous GPS stations in Greenland as part the U.S. contribution to the International Polar Year (IPY) and the international POLENET consortium. They will use this network to map the steady vertical velocity field associated with postglacial rebound (PGR), which will provide GRACE, and any successor missions, with an accurate 'PGR correction', thereby suppressing by far the largest source of uncertainty in GRACE-based estimates of ice mass changes in Greenland. They intend to use GNET to 'weigh' annual and interannual changes in ice mass, obtaining better spatial resolution than GRACE is capable of, using Earth's instantaneous elastic response to surface load changes. This approach will be calibrated and validated by relating annual or seasonal patterns of loading (the cause) with in-phase seasonal oscillations of adjacent bedrock. Having calibrated a 'weighing machine' in this way, the Principal Investigators will be able to quickly detect and analyze any abrupt increases in long terms rates of ice gain or loss.

Relevance to IPY: POLENET (Polar Earth Observing Network) is a consortium involving 24 nations that will dramatically improve the coverage in geodetic, magnetic, and seismic data across the polar regions during IPY. GNET, which involves three international partners, constitutes the largest component of a POLENET deployment across Greenland, and is the only POLENET component in the northern hemisphere which is focused on a major ice sheet. It will complement GPS initiatives elsewhere in the Arctic to be carried out by more than 12 nations participating in POLENET. POLENET will overcome the scarcity of observational systems in the Earth's polar regions, and will provide a legacy in observational infrastructure and in the technological capability to deploy autonomous operations in extreme environments. The GPS data and metadata will be made available to the global science community as soon as they reach the UNAVCO archive.

Broader Impacts. The POLENET project will bring about the development of new technologies for operating autonomous stations in the Arctic and Antarctic. It will promote one of the most holistic collaborations between glaciologists, geodesists, geophysicists, geologists, meteorologists and oceanographers in the history of these disciplines. This project will leverage NASA's GRACE project to an entirely new level of importance, because providing GRACE with a "PGR correction" will transform it into the single most powerful measurement system ever developed for the direct observation of mass transfer between the ice sheets and the oceans. GNET will be able to detect any rapid acceleration in ice mass gain or loss in Greenland, especially at the critical margins of the ice sheet, in response to changing climatic conditions. Even more broadly, understanding and monitoring the behavior of the Greenland (as well as the Antarctic) ice sheet,
is a matter of tremendous societal importance. It is widely understood that there is serious danger that the West Antarctic or Greenland ice sheets could collapse and so seriously damage the global economy, and degrade the social infrastructure supporting hundreds of millions of people, by inundating large swaths of densely inhabited coastal areas worldwide. While it may be too late to reverse global warming before sea level rise becomes seriously problematic, it is crucial to assess both the possible severity of sea level rise, and the amount of time that our governments have to respond to, or mitigate, developments that they may be powerless to prevent. Given the importance of this agenda, we propose to develop an outreach component using UNAVCO's outreach specialists.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Beata Csatho, Toni Schenk, C.J. van der Veen and William Krabill "Intermittent thinning of Jakobshavn Isbrae, West Greenland since the Little Ice Age" Journal of Glaciology , v.54 , 2008 , p.131
Braun, A; Kim, HR; Csatho, B; von Frese, RRB "Gravity-inferred crustal thickness of Greenland" EARTH AND PLANETARY SCIENCE LETTERS , v.262 , 2007 , p.138 View record at Web of Science 10.1016/j.epsl.2007.07.05
Forman, SL; Marin, L; van der Veen, C; Tremper, C; Csatho, B "Little ice age and neoglacial landforms at the Inland Ice margin, Isunguata Sermia, Kangerlussuaq, west Greenland" BOREAS , v.36 , 2007 , p.341 View record at Web of Science 10.1080/0017313060117330
van der Veen, CJ; Leftwich, T; von Frese, R; Csatho, BM; Li, J "Subglacial topography and geothermal heat flux: Potential interactions with drainage of the Greenland ice sheet" GEOPHYSICAL RESEARCH LETTERS , v.34 , 2007 View record at Web of Science 10.1029/2007GL03004
van der Veen, C.J., Y. Ahn, W.B. Krabill, E. Mosley-Mosley Thompson and B. M. Csatho "Surface roughness over the northern half of the Greenland ice sheet from airborne laser altimetry" Journal of Geophysical Research, Earth Surface , v.114 , 2009 F01001, doi:10.1029/2008JF001067.

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