Snow Water Equivalent Retrieval Using Active and Passive Microwave Observations
This paper implements a newly developed combined active and passive algorithm for the retrieval of snow water equivalent (SWE) by using three‐channel active and two‐channel passive observations. First, passive microwave observations at 19 and 37 GHz are used to determine the scattering albedo of sno...
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description | This paper implements a newly developed combined active and passive algorithm for the retrieval of snow water equivalent (SWE) by using three‐channel active and two‐channel passive observations. First, passive microwave observations at 19 and 37 GHz are used to determine the scattering albedo of snow. An a priori scattering albedo is obtained by averaging over time series observations. Second, 13.3 GHz is introduced to formulate a three‐channel (9.6, 13.3, and 17.2 GHz) radar algorithm which reduces effects of background scattering from the snow‐soil interface, and improves SWE retrieval. In the algorithm, the bicontinuous dense media radiative transfer (DMRT‐Bic) is used to compute look‐up tables (LUTs) of both radar backscatter and radiometer brightness temperatures (TBs) of the snowpack. To accelerate the retrieval, a parameterized model is derived from LUT by regression training, which links backscatter to the scattering albedo at 9.6 GHz or 13.3 GHz and to SWE. The volume scattering of snow is obtained by subtracting the background scattering from radar observations. SWE is then retrieved through a cost function that is guided by the a priori scattering albedo obtained from the passive microwave observations. The proposed algorithm, along with the active‐only version, is evaluated against the Finnish Nordic Snow Radar Experiment (NoSREx) data set measured in 2009–2013. The combined active‐passive algorithm achieves root mean square errors (RSME) less than 27 mm and correlation coefficients above 0.68 for 2009–2010, RMSE less than 21 mm and correlation above 0.85 for 2010–2011, and RMSE less than 40 mm and correlation above 0.38 for 2012–2013.
Key Points
Snow water equivalent retrieval using X (9.6 GHz) and upper Ku band (17.2 GHz) radar observations is improved by adding lower Ku‐band (13.3 GHz) data
Passive observations are used to obtain scattering albedos, which improves the radar retrieval algorithm performance
The resulting combined active and passive algorithm is validated against the Finnish NoSREx dataset |
doi_str_mv | 10.1029/2020WR027563 |
format | Article |
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Key Points
Snow water equivalent retrieval using X (9.6 GHz) and upper Ku band (17.2 GHz) radar observations is improved by adding lower Ku‐band (13.3 GHz) data
Passive observations are used to obtain scattering albedos, which improves the radar retrieval algorithm performance
The resulting combined active and passive algorithm is validated against the Finnish NoSREx dataset</description><identifier>ISSN: 0043-1397</identifier><identifier>EISSN: 1944-7973</identifier><identifier>DOI: 10.1029/2020WR027563</identifier><language>eng</language><publisher>Washington: John Wiley & Sons, Inc</publisher><subject>Albedo ; Albedo of snow ; Algorithms ; Backscatter ; Backscattering ; Brightness temperature ; Coefficients ; combine active and passive ; Correlation coefficient ; Correlation coefficients ; Cost function ; Equivalence ; Meteorological satellites ; Radar ; Radar backscatter ; Radar data ; Radiative transfer ; Radiometers ; Retrieval ; Scattering ; scattering albedo ; Snow ; snow water equivalent (SWE) ; Snow-water equivalent ; Snowpack ; Soil improvement ; Training</subject><ispartof>Water resources research, 2021-07, Vol.57 (7), p.n/a</ispartof><rights>2021. American Geophysical Union. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a3682-9e88a70ed79c5234bd2f0fd94fc246c4fa84ac2db905c595981f2d5f9c2b5c7e3</citedby><cites>FETCH-LOGICAL-a3682-9e88a70ed79c5234bd2f0fd94fc246c4fa84ac2db905c595981f2d5f9c2b5c7e3</cites><orcidid>0000-0003-0638-8790 ; 0000-0002-8764-8883</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1029%2F2020WR027563$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1029%2F2020WR027563$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,11494,27903,27904,45553,45554,46446,46870</link.rule.ids></links><search><creatorcontrib>Zhu, Jiyue</creatorcontrib><creatorcontrib>Tan, Shurun</creatorcontrib><creatorcontrib>Tsang, Leung</creatorcontrib><creatorcontrib>Kang, Do‐Hyuk</creatorcontrib><creatorcontrib>Kim, Edward</creatorcontrib><title>Snow Water Equivalent Retrieval Using Active and Passive Microwave Observations</title><title>Water resources research</title><description>This paper implements a newly developed combined active and passive algorithm for the retrieval of snow water equivalent (SWE) by using three‐channel active and two‐channel passive observations. First, passive microwave observations at 19 and 37 GHz are used to determine the scattering albedo of snow. An a priori scattering albedo is obtained by averaging over time series observations. Second, 13.3 GHz is introduced to formulate a three‐channel (9.6, 13.3, and 17.2 GHz) radar algorithm which reduces effects of background scattering from the snow‐soil interface, and improves SWE retrieval. In the algorithm, the bicontinuous dense media radiative transfer (DMRT‐Bic) is used to compute look‐up tables (LUTs) of both radar backscatter and radiometer brightness temperatures (TBs) of the snowpack. To accelerate the retrieval, a parameterized model is derived from LUT by regression training, which links backscatter to the scattering albedo at 9.6 GHz or 13.3 GHz and to SWE. The volume scattering of snow is obtained by subtracting the background scattering from radar observations. SWE is then retrieved through a cost function that is guided by the a priori scattering albedo obtained from the passive microwave observations. The proposed algorithm, along with the active‐only version, is evaluated against the Finnish Nordic Snow Radar Experiment (NoSREx) data set measured in 2009–2013. The combined active‐passive algorithm achieves root mean square errors (RSME) less than 27 mm and correlation coefficients above 0.68 for 2009–2010, RMSE less than 21 mm and correlation above 0.85 for 2010–2011, and RMSE less than 40 mm and correlation above 0.38 for 2012–2013.
Key Points
Snow water equivalent retrieval using X (9.6 GHz) and upper Ku band (17.2 GHz) radar observations is improved by adding lower Ku‐band (13.3 GHz) data
Passive observations are used to obtain scattering albedos, which improves the radar retrieval algorithm performance
The resulting combined active and passive algorithm is validated against the Finnish NoSREx dataset</description><subject>Albedo</subject><subject>Albedo of snow</subject><subject>Algorithms</subject><subject>Backscatter</subject><subject>Backscattering</subject><subject>Brightness temperature</subject><subject>Coefficients</subject><subject>combine active and passive</subject><subject>Correlation coefficient</subject><subject>Correlation coefficients</subject><subject>Cost function</subject><subject>Equivalence</subject><subject>Meteorological satellites</subject><subject>Radar</subject><subject>Radar backscatter</subject><subject>Radar data</subject><subject>Radiative transfer</subject><subject>Radiometers</subject><subject>Retrieval</subject><subject>Scattering</subject><subject>scattering albedo</subject><subject>Snow</subject><subject>snow water equivalent (SWE)</subject><subject>Snow-water equivalent</subject><subject>Snowpack</subject><subject>Soil improvement</subject><subject>Training</subject><issn>0043-1397</issn><issn>1944-7973</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><recordid>eNp9kE9LAzEQxYMoWKs3P0DAq6vJJNlsjqXUP1CprJYeQzabSErdbZNtS7-9W-rBk6d5Az_mvXkI3VLyQAmoRyBAFiUBKXJ2hgZUcZ5JJdk5GhDCWUaZkpfoKqUlIZSLXA7Q7KNp93hhOhfxZLMNO7NyTYdL18Xg-gXPU2i-8Mh2YeewaWr8blI66rdgY7s3vZpVycWd6ULbpGt04c0quZvfOUTzp8nn-CWbzp5fx6NpZlheQKZcURhJXC2VFcB4VYMnvlbcW-C55d4U3FioK0WEFUqognqohVcWKmGlY0N0d7q7ju1m61Knl-02Nr2lBiEEU7z_vqfuT1QfNaXovF7H8G3iQVOij5Xpv5X1ODvh-7Byh39ZvSjHJQhWAPsBaoRtfw</recordid><startdate>202107</startdate><enddate>202107</enddate><creator>Zhu, Jiyue</creator><creator>Tan, Shurun</creator><creator>Tsang, Leung</creator><creator>Kang, Do‐Hyuk</creator><creator>Kim, Edward</creator><general>John Wiley & Sons, Inc</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7QH</scope><scope>7QL</scope><scope>7T7</scope><scope>7TG</scope><scope>7U9</scope><scope>7UA</scope><scope>8FD</scope><scope>C1K</scope><scope>F1W</scope><scope>FR3</scope><scope>H94</scope><scope>H96</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>M7N</scope><scope>P64</scope><orcidid>https://orcid.org/0000-0003-0638-8790</orcidid><orcidid>https://orcid.org/0000-0002-8764-8883</orcidid></search><sort><creationdate>202107</creationdate><title>Snow Water Equivalent Retrieval Using Active and Passive Microwave Observations</title><author>Zhu, Jiyue ; Tan, Shurun ; Tsang, Leung ; Kang, Do‐Hyuk ; Kim, Edward</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a3682-9e88a70ed79c5234bd2f0fd94fc246c4fa84ac2db905c595981f2d5f9c2b5c7e3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Albedo</topic><topic>Albedo of snow</topic><topic>Algorithms</topic><topic>Backscatter</topic><topic>Backscattering</topic><topic>Brightness temperature</topic><topic>Coefficients</topic><topic>combine active and passive</topic><topic>Correlation coefficient</topic><topic>Correlation coefficients</topic><topic>Cost function</topic><topic>Equivalence</topic><topic>Meteorological satellites</topic><topic>Radar</topic><topic>Radar backscatter</topic><topic>Radar data</topic><topic>Radiative transfer</topic><topic>Radiometers</topic><topic>Retrieval</topic><topic>Scattering</topic><topic>scattering albedo</topic><topic>Snow</topic><topic>snow water equivalent (SWE)</topic><topic>Snow-water equivalent</topic><topic>Snowpack</topic><topic>Soil improvement</topic><topic>Training</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zhu, Jiyue</creatorcontrib><creatorcontrib>Tan, Shurun</creatorcontrib><creatorcontrib>Tsang, Leung</creatorcontrib><creatorcontrib>Kang, Do‐Hyuk</creatorcontrib><creatorcontrib>Kim, Edward</creatorcontrib><collection>CrossRef</collection><collection>Aqualine</collection><collection>Bacteriology Abstracts (Microbiology B)</collection><collection>Industrial and Applied Microbiology Abstracts (Microbiology A)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Virology and AIDS Abstracts</collection><collection>Water Resources Abstracts</collection><collection>Technology Research Database</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>AIDS and Cancer Research Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Algology Mycology and Protozoology Abstracts (Microbiology C)</collection><collection>Biotechnology and BioEngineering Abstracts</collection><jtitle>Water resources research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zhu, Jiyue</au><au>Tan, Shurun</au><au>Tsang, Leung</au><au>Kang, Do‐Hyuk</au><au>Kim, Edward</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Snow Water Equivalent Retrieval Using Active and Passive Microwave Observations</atitle><jtitle>Water resources research</jtitle><date>2021-07</date><risdate>2021</risdate><volume>57</volume><issue>7</issue><epage>n/a</epage><issn>0043-1397</issn><eissn>1944-7973</eissn><abstract>This paper implements a newly developed combined active and passive algorithm for the retrieval of snow water equivalent (SWE) by using three‐channel active and two‐channel passive observations. First, passive microwave observations at 19 and 37 GHz are used to determine the scattering albedo of snow. An a priori scattering albedo is obtained by averaging over time series observations. Second, 13.3 GHz is introduced to formulate a three‐channel (9.6, 13.3, and 17.2 GHz) radar algorithm which reduces effects of background scattering from the snow‐soil interface, and improves SWE retrieval. In the algorithm, the bicontinuous dense media radiative transfer (DMRT‐Bic) is used to compute look‐up tables (LUTs) of both radar backscatter and radiometer brightness temperatures (TBs) of the snowpack. To accelerate the retrieval, a parameterized model is derived from LUT by regression training, which links backscatter to the scattering albedo at 9.6 GHz or 13.3 GHz and to SWE. The volume scattering of snow is obtained by subtracting the background scattering from radar observations. SWE is then retrieved through a cost function that is guided by the a priori scattering albedo obtained from the passive microwave observations. The proposed algorithm, along with the active‐only version, is evaluated against the Finnish Nordic Snow Radar Experiment (NoSREx) data set measured in 2009–2013. The combined active‐passive algorithm achieves root mean square errors (RSME) less than 27 mm and correlation coefficients above 0.68 for 2009–2010, RMSE less than 21 mm and correlation above 0.85 for 2010–2011, and RMSE less than 40 mm and correlation above 0.38 for 2012–2013.
Key Points
Snow water equivalent retrieval using X (9.6 GHz) and upper Ku band (17.2 GHz) radar observations is improved by adding lower Ku‐band (13.3 GHz) data
Passive observations are used to obtain scattering albedos, which improves the radar retrieval algorithm performance
The resulting combined active and passive algorithm is validated against the Finnish NoSREx dataset</abstract><cop>Washington</cop><pub>John Wiley & Sons, Inc</pub><doi>10.1029/2020WR027563</doi><tpages>21</tpages><orcidid>https://orcid.org/0000-0003-0638-8790</orcidid><orcidid>https://orcid.org/0000-0002-8764-8883</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Albedo Albedo of snow Algorithms Backscatter Backscattering Brightness temperature Coefficients combine active and passive Correlation coefficient Correlation coefficients Cost function Equivalence Meteorological satellites Radar Radar backscatter Radar data Radiative transfer Radiometers Retrieval Scattering scattering albedo Snow snow water equivalent (SWE) Snow-water equivalent Snowpack Soil improvement Training |
title | Snow Water Equivalent Retrieval Using Active and Passive Microwave Observations |
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