Award Abstract # 2113392
Collaborative Research: Arctic Observing Network For Observing Transformation of the Greenland Ice Sheet Firn Layer

NSF Org: OPP
Office of Polar Programs (OPP)
Recipient: UNIVERSITY OF WYOMING
Initial Amendment Date: July 30, 2021
Latest Amendment Date: July 30, 2021
Award Number: 2113392
Award Instrument: Standard Grant
Program Manager: Lauren Culler
lculler@nsf.gov
 (703)292-8057
OPP
 Office of Polar Programs (OPP)
GEO
 Directorate for Geosciences
Start Date: November 1, 2021
End Date: October 31, 2026 (Estimated)
Total Intended Award Amount: $297,116.00
Total Awarded Amount to Date: $297,116.00
Funds Obligated to Date: FY 2021 = $297,116.00
History of Investigator:
  • Neil Humphrey (Principal Investigator)
    neil@uwyo.edu
Recipient Sponsored Research Office: University of Wyoming
1000 E UNIVERSITY AVE
LARAMIE
WY  US  82071-2000
(307)766-5320
Sponsor Congressional District: 00
Primary Place of Performance: University of Wyoming
1000 E. University Avenue
Laramie
WY  US  82071-2000
Primary Place of Performance
Congressional District:
00
Unique Entity Identifier (UEI): FDR5YF2K32X5
Parent UEI: FDR5YF2K32X5
NSF Program(s): AON-Arctic Observing Network
Primary Program Source: 010V2122DB R&RA ARP Act DEFC V
Program Reference Code(s): 102Z, 1079, 5294
Program Element Code(s): 529300
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.078

ABSTRACT

This award is funded in whole or in part under the American Rescue Plan Act of 2021 (Public Law 117-2)

As the Arctic warms two-to-three times faster than the global average, the duration and intensity of melting is generally increasing on the surface of the Greenland ice sheet. About 90% of ice sheet is covered by compacted snow that is slowly transitioning into glacier ice. This aged and dense snow is called ?firn? and forms a porous layer that is many tens of meters thick. Much of the meltwater generated from the surface of the firn layer infiltrates into the underlying open pore space of the firn and refreezes. However, as this porous layer absorbs more melt it becomes warmer, denser, and filled with ice layers, which reduces its ability to absorb additional melt. Therefore, the thermal and structural transformation that Greenland's firn layer is presently undergoing has important implications for the ice sheet's capacity to retain future melt. This project is directly observing firn evolution with a network of instruments installed within the firn layer and with ice cores sampling the firn. The observational data collected by this project provides on-the-ground documentation of firn conditions needed to develop and test models and remote sensing tools for large-scale investigations of changes to the Greenland ice sheet. Future transformation of the firn layer will govern how much surface melt is retained locally on the ice sheet and how much runs off, thereby impacting hydrologic conditions of the ice sheet and surrounding regions, ocean salinity, and sea level rise.

The researchers will install and maintain an observation network along a transect of the Greenland ice sheet to directly measure the state and transformation of firn properties. Repeat sampling of firn cores and instrumentation extending from the surface to 25 meters depth will yield the observational datasets needed by multiple scientific communities: firn temperature, density and ice content, densification rate, surface boundary processes (radiation, snow accumulation, temperature), and ice velocity. The network will yield 4-5 full-year records in this five-year Arctic Observing Network project. The project will provide comprehensive datasets for process-level investigations, testing climate model simulations of firn processes, and interpreting satellite-based measurement of surface elevation change. The project will engage and support a relatively large number of undergraduate and graduate students at R2 institutions with field research experiences and real-world classroom learning. Outreach activities will target three groups poorly represented in cryospheric science: 1) local and Indigenous residents of Greenland; 2) American Indian undergraduate students; and 3) economically disadvantaged school children.

This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Harper, J. and Saito, J. and Humphrey, N. "Cold Season Rain Event Has Impact on Greenland's Firn Layer Comparable to Entire Summer Melt Season" Geophysical Research Letters , v.50 , 2023 https://doi.org/10.1029/2023GL103654 Citation Details
Saito, Jun and Harper, Joel and Humphrey, Neil "Uptake and Transfer of Heat Within the Firn Layer of Greenland Ice Sheet's Percolation Zone" Journal of Geophysical Research: Earth Surface , v.129 , 2024 https://doi.org/10.1029/2024JF007667 Citation Details

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