Remote Sensing | |
Remotely Sensed Active Layer Thickness (ReSALT) at Barrow, Alaska Using Interferometric Synthetic Aperture Radar | |
Kevin Schaefer3  Lin Liu7  Andrew Parsekian6  Elchin Jafarov3  Albert Chen1  Tingjun Zhang3  Alessio Gusmeroli2  Santosh Panda2  Howard A. Zebker1  Tim Schaefer4  Santonu Goswami5  Daniel J. Hayes5  Guido Grosse5  Benjamin Jones5  | |
[1] Department of Geophysics, Stanford University, Stanford, CA 94305, USA; E-Mails:;International Arctic Research Center, University of Alaska, Fairbanks, 99775 AK, USA; E-Mails:;National Snow and Ice Data Center, Cooperative Institute for Research in Environmental Sciences, University of Colorado at Boulder, Boulder, CO 80309, USA; E-Mails:;Galmont Consulting, Chicago, 60602 IL, USA; E-Mail:National Snow and Ice Data Center, Cooperative Institute for Research in Environmental Sciences, University of Colorado at Boulder, Boulder, CO 80309, USA;;Department of Geology and Geophysics, University of Wyoming, Laramie, WY 82070, USA; E-Mail:;Earth System Science Programme, Faculty of Science, The Chinese University of Hong Kong, Hong Kong, China; E-Mail: | |
关键词: permafrost; permafrost dynamics; active layer thickness; barrow; interferometric synthetic aperture radar; ground penetrating radar; | |
DOI : 10.3390/rs70403735 | |
来源: mdpi | |
【 摘 要 】
Active layer thickness (ALT) is a critical parameter for monitoring the status of permafrost that is typically measured at specific locations using probing,
【 授权许可】
CC BY
© 2015 by the authors; licensee MDPI, Basel, Switzerland.
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