Coastal GNSS-R phase altimetry based on the combination of L1 and L5 signals under high sea states
High-precision sea surface heights retrieved from the Global Navigation Satellite System Reflectometry (GNSS-R) measurements will be valuable in the fields of geodesy and oceanography studies. Due to the short wavelengths and low power of GNSS signals, the continuously tracked carrier phase measurem...
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description | High-precision sea surface heights retrieved from the Global Navigation Satellite System Reflectometry (GNSS-R) measurements will be valuable in the fields of geodesy and oceanography studies. Due to the short wavelengths and low power of GNSS signals, the continuously tracked carrier phase measurements of reflected signals are usually unavailable for sea surfaces with big roughness, varying over space and time. In coastal conditions, persisting spatial coherence assumption can be made within the antenna coverage when the waves are not greatly breaking. To deal with temporal incoherence, we propose an improved algorithm to extract the combined interferometric phase difference measurements between direct and reflected signals under high sea states. After initial tracking the direct signals, dual-frequency observations are combined in the complex domain and the resulting interferometric signal is refined through open-loop tracking with 60-s coherent integration before the phase difference measurements are extracted, without tracking their respective carrier phase measurements in advance. In order to verify our method, a coastal experiment under different sea conditions was conducted and raw intermediate frequency data were collected. The raw data were then processed by a GNSS-R software-defined receiver to compute the path delay measurements of Quasi-Zenith Satellite System signals, which had good visibility during our experiment. For high sea states, that is, when the Rayleigh criterion is not fulfilled for the individual wavelengths, the phase delay measurements of L1 and L5 were random over time, while phase delay can still be well recovered for their combination. Also, the phase delay combination can be well extracted with a higher elevation angle than the previous studies. Finally, the altimetry solutions derived from the carrier phase delay measurements combination were compared with the in situ observations from a 26-GHz radar altimeter. The results show that centimeter-level altimetry accuracy using the combined measurements of L1 and L5 can be achieved under high sea states. |
doi_str_mv | 10.1007/s00190-023-01712-6 |
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Due to the short wavelengths and low power of GNSS signals, the continuously tracked carrier phase measurements of reflected signals are usually unavailable for sea surfaces with big roughness, varying over space and time. In coastal conditions, persisting spatial coherence assumption can be made within the antenna coverage when the waves are not greatly breaking. To deal with temporal incoherence, we propose an improved algorithm to extract the combined interferometric phase difference measurements between direct and reflected signals under high sea states. After initial tracking the direct signals, dual-frequency observations are combined in the complex domain and the resulting interferometric signal is refined through open-loop tracking with 60-s coherent integration before the phase difference measurements are extracted, without tracking their respective carrier phase measurements in advance. In order to verify our method, a coastal experiment under different sea conditions was conducted and raw intermediate frequency data were collected. The raw data were then processed by a GNSS-R software-defined receiver to compute the path delay measurements of Quasi-Zenith Satellite System signals, which had good visibility during our experiment. For high sea states, that is, when the Rayleigh criterion is not fulfilled for the individual wavelengths, the phase delay measurements of L1 and L5 were random over time, while phase delay can still be well recovered for their combination. Also, the phase delay combination can be well extracted with a higher elevation angle than the previous studies. Finally, the altimetry solutions derived from the carrier phase delay measurements combination were compared with the in situ observations from a 26-GHz radar altimeter. The results show that centimeter-level altimetry accuracy using the combined measurements of L1 and L5 can be achieved under high sea states.</description><identifier>ISSN: 0949-7714</identifier><identifier>EISSN: 1432-1394</identifier><identifier>DOI: 10.1007/s00190-023-01712-6</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Altimeters ; Altimetry ; Earth and Environmental Science ; Earth Sciences ; Geodesy ; Geodetics ; Geophysics/Geodesy ; High seas ; Navigation ; Navigation satellites ; Navigation systems ; Navigational satellites ; Oceanography ; Original Article ; Radar ; Radar altimeters ; Radio altimeters ; Roughness ; Sea state ; Sea surface ; Tracking ; Wavelengths</subject><ispartof>Journal of geodesy, 2023-02, Vol.97 (2), Article 19</ispartof><rights>Springer-Verlag GmbH Germany, part of Springer Nature 2023. Springer Nature or its licensor (e.g. a society or other partner) holds exclusive rights to this article under a publishing agreement with the author(s) or other rightsholder(s); author self-archiving of the accepted manuscript version of this article is solely governed by the terms of such publishing agreement and applicable law.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c249t-dff4e11db254440e808223583bf4327c5c5d8c2633ea514f1829fef68208c0243</citedby><cites>FETCH-LOGICAL-c249t-dff4e11db254440e808223583bf4327c5c5d8c2633ea514f1829fef68208c0243</cites><orcidid>0000-0001-5818-6264</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s00190-023-01712-6$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00190-023-01712-6$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27901,27902,41464,42533,51294</link.rule.ids></links><search><creatorcontrib>He, Yunqiao</creatorcontrib><creatorcontrib>Gao, Fan</creatorcontrib><creatorcontrib>Xu, Tianhe</creatorcontrib><creatorcontrib>Meng, Xinyue</creatorcontrib><creatorcontrib>Wang, Nazi</creatorcontrib><creatorcontrib>Ning, Baojiao</creatorcontrib><title>Coastal GNSS-R phase altimetry based on the combination of L1 and L5 signals under high sea states</title><title>Journal of geodesy</title><addtitle>J Geod</addtitle><description>High-precision sea surface heights retrieved from the Global Navigation Satellite System Reflectometry (GNSS-R) measurements will be valuable in the fields of geodesy and oceanography studies. Due to the short wavelengths and low power of GNSS signals, the continuously tracked carrier phase measurements of reflected signals are usually unavailable for sea surfaces with big roughness, varying over space and time. In coastal conditions, persisting spatial coherence assumption can be made within the antenna coverage when the waves are not greatly breaking. To deal with temporal incoherence, we propose an improved algorithm to extract the combined interferometric phase difference measurements between direct and reflected signals under high sea states. After initial tracking the direct signals, dual-frequency observations are combined in the complex domain and the resulting interferometric signal is refined through open-loop tracking with 60-s coherent integration before the phase difference measurements are extracted, without tracking their respective carrier phase measurements in advance. In order to verify our method, a coastal experiment under different sea conditions was conducted and raw intermediate frequency data were collected. The raw data were then processed by a GNSS-R software-defined receiver to compute the path delay measurements of Quasi-Zenith Satellite System signals, which had good visibility during our experiment. For high sea states, that is, when the Rayleigh criterion is not fulfilled for the individual wavelengths, the phase delay measurements of L1 and L5 were random over time, while phase delay can still be well recovered for their combination. Also, the phase delay combination can be well extracted with a higher elevation angle than the previous studies. Finally, the altimetry solutions derived from the carrier phase delay measurements combination were compared with the in situ observations from a 26-GHz radar altimeter. The results show that centimeter-level altimetry accuracy using the combined measurements of L1 and L5 can be achieved under high sea states.</description><subject>Altimeters</subject><subject>Altimetry</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Geodesy</subject><subject>Geodetics</subject><subject>Geophysics/Geodesy</subject><subject>High seas</subject><subject>Navigation</subject><subject>Navigation satellites</subject><subject>Navigation systems</subject><subject>Navigational satellites</subject><subject>Oceanography</subject><subject>Original Article</subject><subject>Radar</subject><subject>Radar altimeters</subject><subject>Radio altimeters</subject><subject>Roughness</subject><subject>Sea state</subject><subject>Sea surface</subject><subject>Tracking</subject><subject>Wavelengths</subject><issn>0949-7714</issn><issn>1432-1394</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2023</creationdate><recordtype>article</recordtype><recordid>eNp9kEtPwzAQhC0EEqXwBzhZ4mxYv2LniCpeUgQShbPlJHaTqk2K7R7673EJEjdOq9F-M9odhK4p3FIAdRcBaAkEGCdAFWWkOEEzKjgjlJfiFM2gFCVRiopzdBHjOuNK6mKG6sVoY7Ib_PS6XJJ3vOtsdNhuUr91KRxwnWWLxwGnzuFm3Nb9YFOf9ehxRbEdWlxJHPvVYDcR74fWBdz1qw5HZ3EOTi5eojOfl-7qd87R5-PDx-KZVG9PL4v7ijRMlIm03gtHaVszKYQAp0EzxqXmtc9_qEY2stUNKzh3VlLhqWald77QDHQDTPA5uplyd2H82ruYzHrch-NdhikNgmsuZKbYRDVhjDE4b3ah39pwMBTMsUszdWlyl-anS1NkE59MMcPDyoW_6H9c3-2YdMY</recordid><startdate>20230201</startdate><enddate>20230201</enddate><creator>He, Yunqiao</creator><creator>Gao, Fan</creator><creator>Xu, Tianhe</creator><creator>Meng, Xinyue</creator><creator>Wang, Nazi</creator><creator>Ning, Baojiao</creator><general>Springer Berlin Heidelberg</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><orcidid>https://orcid.org/0000-0001-5818-6264</orcidid></search><sort><creationdate>20230201</creationdate><title>Coastal GNSS-R phase altimetry based on the combination of L1 and L5 signals under high sea states</title><author>He, Yunqiao ; Gao, Fan ; Xu, Tianhe ; Meng, Xinyue ; Wang, Nazi ; Ning, Baojiao</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c249t-dff4e11db254440e808223583bf4327c5c5d8c2633ea514f1829fef68208c0243</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2023</creationdate><topic>Altimeters</topic><topic>Altimetry</topic><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Geodesy</topic><topic>Geodetics</topic><topic>Geophysics/Geodesy</topic><topic>High seas</topic><topic>Navigation</topic><topic>Navigation satellites</topic><topic>Navigation systems</topic><topic>Navigational satellites</topic><topic>Oceanography</topic><topic>Original Article</topic><topic>Radar</topic><topic>Radar altimeters</topic><topic>Radio altimeters</topic><topic>Roughness</topic><topic>Sea state</topic><topic>Sea surface</topic><topic>Tracking</topic><topic>Wavelengths</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>He, Yunqiao</creatorcontrib><creatorcontrib>Gao, Fan</creatorcontrib><creatorcontrib>Xu, Tianhe</creatorcontrib><creatorcontrib>Meng, Xinyue</creatorcontrib><creatorcontrib>Wang, Nazi</creatorcontrib><creatorcontrib>Ning, Baojiao</creatorcontrib><collection>CrossRef</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Journal of geodesy</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>He, Yunqiao</au><au>Gao, Fan</au><au>Xu, Tianhe</au><au>Meng, Xinyue</au><au>Wang, Nazi</au><au>Ning, Baojiao</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Coastal GNSS-R phase altimetry based on the combination of L1 and L5 signals under high sea states</atitle><jtitle>Journal of geodesy</jtitle><stitle>J Geod</stitle><date>2023-02-01</date><risdate>2023</risdate><volume>97</volume><issue>2</issue><artnum>19</artnum><issn>0949-7714</issn><eissn>1432-1394</eissn><abstract>High-precision sea surface heights retrieved from the Global Navigation Satellite System Reflectometry (GNSS-R) measurements will be valuable in the fields of geodesy and oceanography studies. Due to the short wavelengths and low power of GNSS signals, the continuously tracked carrier phase measurements of reflected signals are usually unavailable for sea surfaces with big roughness, varying over space and time. In coastal conditions, persisting spatial coherence assumption can be made within the antenna coverage when the waves are not greatly breaking. To deal with temporal incoherence, we propose an improved algorithm to extract the combined interferometric phase difference measurements between direct and reflected signals under high sea states. After initial tracking the direct signals, dual-frequency observations are combined in the complex domain and the resulting interferometric signal is refined through open-loop tracking with 60-s coherent integration before the phase difference measurements are extracted, without tracking their respective carrier phase measurements in advance. In order to verify our method, a coastal experiment under different sea conditions was conducted and raw intermediate frequency data were collected. The raw data were then processed by a GNSS-R software-defined receiver to compute the path delay measurements of Quasi-Zenith Satellite System signals, which had good visibility during our experiment. For high sea states, that is, when the Rayleigh criterion is not fulfilled for the individual wavelengths, the phase delay measurements of L1 and L5 were random over time, while phase delay can still be well recovered for their combination. Also, the phase delay combination can be well extracted with a higher elevation angle than the previous studies. Finally, the altimetry solutions derived from the carrier phase delay measurements combination were compared with the in situ observations from a 26-GHz radar altimeter. The results show that centimeter-level altimetry accuracy using the combined measurements of L1 and L5 can be achieved under high sea states.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s00190-023-01712-6</doi><orcidid>https://orcid.org/0000-0001-5818-6264</orcidid></addata></record> |
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subjects | Altimeters Altimetry Earth and Environmental Science Earth Sciences Geodesy Geodetics Geophysics/Geodesy High seas Navigation Navigation satellites Navigation systems Navigational satellites Oceanography Original Article Radar Radar altimeters Radio altimeters Roughness Sea state Sea surface Tracking Wavelengths |
title | Coastal GNSS-R phase altimetry based on the combination of L1 and L5 signals under high sea states |
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