Articles | Volume 16, issue 1
https://doi.org/10.5194/tc-16-103-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-16-103-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
An empirical algorithm to map perennial firn aquifers and ice slabs within the Greenland Ice Sheet using satellite L-band microwave radiometry
Julie Z. Miller
CORRESPONDING AUTHOR
Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, Colorado, USA
Earth Science and Observation Center, University of Colorado Boulder, Boulder, Colorado, USA
Riley Culberg
Department of Electrical Engineering, Stanford University, Stanford, California, USA
David G. Long
Department of Electrical and Computer Engineering, Brigham Young University, Provo, Utah, USA
Christopher A. Shuman
Joint Center for Earth Systems Technology at Code 615, Cryospheric Sciences Laboratory, NASA Goddard Space Flight Center, University of Maryland, Baltimore County, Greenbelt, Maryland, USA
Dustin M. Schroeder
Department of Electrical Engineering, Stanford University, Stanford, California, USA
Department of Geophysics, Stanford University, Stanford, CA, USA
Mary J. Brodzik
Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, Colorado, USA
National Snow and Ice Data Center, University of Colorado Boulder, Boulder, Colorado, USA
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Seyedmohammad Mousavi, Andreas Colliander, Julie Z. Miller, and John S. Kimball
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Julie Z. Miller, David G. Long, Kenneth C. Jezek, Joel T. Johnson, Mary J. Brodzik, Christopher A. Shuman, Lora S. Koenig, and Ted A. Scambos
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Short summary
We use L-band brightness temperature imagery from NASA's Soil Moisture Active Passive (SMAP) satellite to map the extent of perennial firn aquifer and ice slab areas within the Greenland Ice Sheet. As Greenland's climate continues to warm and seasonal surface melting increases in extent, intensity, and duration, quantifying the possible rapid expansion of perennial firn aquifers and ice slab areas has significant implications for understanding the stability of the Greenland Ice Sheet.
We use L-band brightness temperature imagery from NASA's Soil Moisture Active Passive (SMAP)...