Antarctic Snowmelt Detected by Diurnal Variations of AMSR-E Brightness Temperature
Antarctic surface snowmelt is sensitive to the polar climate. The ascending and descending passes of the Advanced Microwave Scanning Radiometer for Earth Observing System Sensor (AMSR-E) observed the Antarctic ice sheet in the afternoon (the warmest period) and at midnight (a cold period), enabling...
Published in: | Remote Sensing |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
MDPI AG
2018
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Subjects: | |
Online Access: | https://doi.org/10.3390/rs10091391 https://doaj.org/article/8c0ae060162749e59f856da56500872f |