Conjoint Inversion of Snow Temperature Profiles from Microwave and Infrared Brightness Temperature in Antarctica

The snow temperature above the ice sheet is one of the basic characteristic parameters of the ice sheet, which plays an important role in the study of the global climate. Because infrared and microwaves with different frequencies have different penetration depths in snow, it is possible to retrieve...

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Published in:Remote Sensing
Main Authors: Zhiwei Chen, Rong Jin, Liqiang Zhang, Ke Chen, Qingxia Li
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2023
Subjects:
Online Access:https://doi.org/10.3390/rs15051396
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spelling ftmdpi:oai:mdpi.com:/2072-4292/15/5/1396/ 2023-08-20T04:00:19+02:00 Conjoint Inversion of Snow Temperature Profiles from Microwave and Infrared Brightness Temperature in Antarctica Zhiwei Chen Rong Jin Liqiang Zhang Ke Chen Qingxia Li agris 2023-03-01 application/pdf https://doi.org/10.3390/rs15051396 EN eng Multidisciplinary Digital Publishing Institute Remote Sensing in Geology, Geomorphology and Hydrology https://dx.doi.org/10.3390/rs15051396 https://creativecommons.org/licenses/by/4.0/ Remote Sensing; Volume 15; Issue 5; Pages: 1396 conjoint inversion algorithm snow temperature profiles microwave brightness temperature infrared brightness temperature Text 2023 ftmdpi https://doi.org/10.3390/rs15051396 2023-08-01T09:04:12Z The snow temperature above the ice sheet is one of the basic characteristic parameters of the ice sheet, which plays an important role in the study of the global climate. Because infrared and microwaves with different frequencies have different penetration depths in snow, it is possible to retrieve the snow temperature profiles by combining microwave and infrared brightness temperatures. This paper proposes a conjoint inversion algorithm to retrieve snow temperature profiles by combining multi-frequency microwave brightness temperature (BT) with infrared BT, in which different weight functions of microwave BT at different frequencies are adopted, and the atmosphere influence has also been corrected. The snow temperature profile data are retrieved based on AMSR2 microwave BT data and MODIS infrared BT data in 2017 and 2018, which are evaluated by comparing with the measured snow temperature at Dome-C station. The results confirm that the inverted snow temperature profiles are consistent with the field observation data from the Dome-C station. Multi-frequency microwave brightness temperature can be used to invert the snow temperature profiles; however, the inverted snow surface temperature is more accurate by combining the infrared BT with the microwave BT in the conjoint inversion algorithm. Text Antarc* Antarctica Ice Sheet MDPI Open Access Publishing Remote Sensing 15 5 1396
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic conjoint inversion algorithm
snow temperature profiles
microwave brightness temperature
infrared brightness temperature
spellingShingle conjoint inversion algorithm
snow temperature profiles
microwave brightness temperature
infrared brightness temperature
Zhiwei Chen
Rong Jin
Liqiang Zhang
Ke Chen
Qingxia Li
Conjoint Inversion of Snow Temperature Profiles from Microwave and Infrared Brightness Temperature in Antarctica
topic_facet conjoint inversion algorithm
snow temperature profiles
microwave brightness temperature
infrared brightness temperature
description The snow temperature above the ice sheet is one of the basic characteristic parameters of the ice sheet, which plays an important role in the study of the global climate. Because infrared and microwaves with different frequencies have different penetration depths in snow, it is possible to retrieve the snow temperature profiles by combining microwave and infrared brightness temperatures. This paper proposes a conjoint inversion algorithm to retrieve snow temperature profiles by combining multi-frequency microwave brightness temperature (BT) with infrared BT, in which different weight functions of microwave BT at different frequencies are adopted, and the atmosphere influence has also been corrected. The snow temperature profile data are retrieved based on AMSR2 microwave BT data and MODIS infrared BT data in 2017 and 2018, which are evaluated by comparing with the measured snow temperature at Dome-C station. The results confirm that the inverted snow temperature profiles are consistent with the field observation data from the Dome-C station. Multi-frequency microwave brightness temperature can be used to invert the snow temperature profiles; however, the inverted snow surface temperature is more accurate by combining the infrared BT with the microwave BT in the conjoint inversion algorithm.
format Text
author Zhiwei Chen
Rong Jin
Liqiang Zhang
Ke Chen
Qingxia Li
author_facet Zhiwei Chen
Rong Jin
Liqiang Zhang
Ke Chen
Qingxia Li
author_sort Zhiwei Chen
title Conjoint Inversion of Snow Temperature Profiles from Microwave and Infrared Brightness Temperature in Antarctica
title_short Conjoint Inversion of Snow Temperature Profiles from Microwave and Infrared Brightness Temperature in Antarctica
title_full Conjoint Inversion of Snow Temperature Profiles from Microwave and Infrared Brightness Temperature in Antarctica
title_fullStr Conjoint Inversion of Snow Temperature Profiles from Microwave and Infrared Brightness Temperature in Antarctica
title_full_unstemmed Conjoint Inversion of Snow Temperature Profiles from Microwave and Infrared Brightness Temperature in Antarctica
title_sort conjoint inversion of snow temperature profiles from microwave and infrared brightness temperature in antarctica
publisher Multidisciplinary Digital Publishing Institute
publishDate 2023
url https://doi.org/10.3390/rs15051396
op_coverage agris
genre Antarc*
Antarctica
Ice Sheet
genre_facet Antarc*
Antarctica
Ice Sheet
op_source Remote Sensing; Volume 15; Issue 5; Pages: 1396
op_relation Remote Sensing in Geology, Geomorphology and Hydrology
https://dx.doi.org/10.3390/rs15051396
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/rs15051396
container_title Remote Sensing
container_volume 15
container_issue 5
container_start_page 1396
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