Snow depth product over Antarctic sea ice from 2002 to 2020 using multisource passive microwave radiometers
Snow over sea ice controls energy budgets and affects sea ice growth and melting and thus has essential effects on the climate. Passive microwave radiometers can be used for basin-scale snow depth estimation at a daily scale; however, previously published methods applied to the Antarctic clearly und...
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ftdoajarticles:oai:doaj.org/article:a6d50d10274e4193bed38f145ed40316 2023-05-15T13:52:27+02:00 Snow depth product over Antarctic sea ice from 2002 to 2020 using multisource passive microwave radiometers X. Shen C.-Q. Ke H. Li 2022-02-01T00:00:00Z https://doi.org/10.5194/essd-14-619-2022 https://doaj.org/article/a6d50d10274e4193bed38f145ed40316 EN eng Copernicus Publications https://essd.copernicus.org/articles/14/619/2022/essd-14-619-2022.pdf https://doaj.org/toc/1866-3508 https://doaj.org/toc/1866-3516 doi:10.5194/essd-14-619-2022 1866-3508 1866-3516 https://doaj.org/article/a6d50d10274e4193bed38f145ed40316 Earth System Science Data, Vol 14, Pp 619-636 (2022) Environmental sciences GE1-350 Geology QE1-996.5 article 2022 ftdoajarticles https://doi.org/10.5194/essd-14-619-2022 2022-12-31T07:15:10Z Snow over sea ice controls energy budgets and affects sea ice growth and melting and thus has essential effects on the climate. Passive microwave radiometers can be used for basin-scale snow depth estimation at a daily scale; however, previously published methods applied to the Antarctic clearly underestimated snow depth, limiting their further application. Here, we estimated snow depth using passive microwave radiometers and a newly constructed, robust method by incorporating lower frequencies, which have been available from AMSR-E and AMSR-2 since 2002. A regression analysis using 7 years of Operation IceBridge (OIB) airborne snow depth measurements showed that the gradient ratio (GR) calculated using brightness temperatures in vertically polarized 37 and 7 GHz, i.e. GR(37 <math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mo>/</mo></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="1b4178c77ca0d4bfee6c9ddd864f3a43"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="essd-14-619-2022-ie00001.svg" width="8pt" height="14pt" src="essd-14-619-2022-ie00001.png"/></svg:svg> 7), was optimal for deriving Antarctic snow depth, with a correlation coefficient of − 0.64. We hence derived new coefficients based on GR(37 <math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mo>/</mo></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="e653eaf840568ee76bb20ba3bf368ae0"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="essd-14-619-2022-ie00002.svg" width="8pt" height="14pt" src="essd-14-619-2022-ie00002.png"/></svg:svg> 7) to improve the current snow depth estimation from passive microwave radiometers. Comparing the new retrieval with in situ ... Article in Journal/Newspaper Antarc* Antarctic Sea ice Directory of Open Access Journals: DOAJ Articles Antarctic The Antarctic Earth System Science Data 14 2 619 636 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Environmental sciences GE1-350 Geology QE1-996.5 |
spellingShingle |
Environmental sciences GE1-350 Geology QE1-996.5 X. Shen C.-Q. Ke H. Li Snow depth product over Antarctic sea ice from 2002 to 2020 using multisource passive microwave radiometers |
topic_facet |
Environmental sciences GE1-350 Geology QE1-996.5 |
description |
Snow over sea ice controls energy budgets and affects sea ice growth and melting and thus has essential effects on the climate. Passive microwave radiometers can be used for basin-scale snow depth estimation at a daily scale; however, previously published methods applied to the Antarctic clearly underestimated snow depth, limiting their further application. Here, we estimated snow depth using passive microwave radiometers and a newly constructed, robust method by incorporating lower frequencies, which have been available from AMSR-E and AMSR-2 since 2002. A regression analysis using 7 years of Operation IceBridge (OIB) airborne snow depth measurements showed that the gradient ratio (GR) calculated using brightness temperatures in vertically polarized 37 and 7 GHz, i.e. GR(37 <math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mo>/</mo></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="1b4178c77ca0d4bfee6c9ddd864f3a43"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="essd-14-619-2022-ie00001.svg" width="8pt" height="14pt" src="essd-14-619-2022-ie00001.png"/></svg:svg> 7), was optimal for deriving Antarctic snow depth, with a correlation coefficient of − 0.64. We hence derived new coefficients based on GR(37 <math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mo>/</mo></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="e653eaf840568ee76bb20ba3bf368ae0"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="essd-14-619-2022-ie00002.svg" width="8pt" height="14pt" src="essd-14-619-2022-ie00002.png"/></svg:svg> 7) to improve the current snow depth estimation from passive microwave radiometers. Comparing the new retrieval with in situ ... |
format |
Article in Journal/Newspaper |
author |
X. Shen C.-Q. Ke H. Li |
author_facet |
X. Shen C.-Q. Ke H. Li |
author_sort |
X. Shen |
title |
Snow depth product over Antarctic sea ice from 2002 to 2020 using multisource passive microwave radiometers |
title_short |
Snow depth product over Antarctic sea ice from 2002 to 2020 using multisource passive microwave radiometers |
title_full |
Snow depth product over Antarctic sea ice from 2002 to 2020 using multisource passive microwave radiometers |
title_fullStr |
Snow depth product over Antarctic sea ice from 2002 to 2020 using multisource passive microwave radiometers |
title_full_unstemmed |
Snow depth product over Antarctic sea ice from 2002 to 2020 using multisource passive microwave radiometers |
title_sort |
snow depth product over antarctic sea ice from 2002 to 2020 using multisource passive microwave radiometers |
publisher |
Copernicus Publications |
publishDate |
2022 |
url |
https://doi.org/10.5194/essd-14-619-2022 https://doaj.org/article/a6d50d10274e4193bed38f145ed40316 |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic Sea ice |
genre_facet |
Antarc* Antarctic Sea ice |
op_source |
Earth System Science Data, Vol 14, Pp 619-636 (2022) |
op_relation |
https://essd.copernicus.org/articles/14/619/2022/essd-14-619-2022.pdf https://doaj.org/toc/1866-3508 https://doaj.org/toc/1866-3516 doi:10.5194/essd-14-619-2022 1866-3508 1866-3516 https://doaj.org/article/a6d50d10274e4193bed38f145ed40316 |
op_doi |
https://doi.org/10.5194/essd-14-619-2022 |
container_title |
Earth System Science Data |
container_volume |
14 |
container_issue |
2 |
container_start_page |
619 |
op_container_end_page |
636 |
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1766256735949946880 |