Altimetric Algorithm and Errors of Ocean Altimetry Using GNSS Reflection Signals
As a new remote sensing technology, the global navigation satellite system(GNSS) reflection signals can be used to collect the information of ocean surface wind, surface roughness and sea surface height. Ocean altimetry based on GNSS reflection technique is of low cost and it is easy to obtain large...
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Published in | China ocean engineering Vol. 29; no. 6; pp. 933 - 944 |
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Main Author | |
Format | Journal Article |
Language | English |
Published |
Nanjing
Chinese Ocean Engineering Society
01.12.2015
Key Laboratory of Surveying and Mapping Technology on lsland and Reef of NASMG,Qingdao 266590,China%College of Geodesy and Geomatics,Shandong University of Science and Technology,Qingdao 266590,China%Key Laboratory of Surveying and Mapping Technology on lsland and Reef of NASMG,Qingdao 266590,China College of Geodesy and Geomatics,Shandong University of Science and Technology,Qingdao 266590,China Satellite Surveying and Mapping Application Center of NASMG,Beijing 101300,China |
Subjects | |
Online Access | Get full text |
ISSN | 0890-5487 2191-8945 |
DOI | 10.1007/s13344-015-0066-3 |
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Summary: | As a new remote sensing technology, the global navigation satellite system(GNSS) reflection signals can be used to collect the information of ocean surface wind, surface roughness and sea surface height. Ocean altimetry based on GNSS reflection technique is of low cost and it is easy to obtain large amounts of data thanks to the global navigation satellite constellation. We can estimate the sea surface height as well as the position of the specular reflection point. This paper focuses on the study of the algorithm to determine the specular reflection point and altimetry equations to estimate the sea surface height over the reflection region. We derive the error equation of sea surface height based on the error propagation theory. Effects of the Doppler shift and the size of the glistening zone on the altimetry are discussed and analyzed at the same time. Finally, we calculate the sea surface height based on the simulated GNSS data within the whole day and verify the sea surface height errors according to the satellite elevation angles. The results show that the sea surface height can reach the precision of 6 cm for elevation angles of 55° to 90°, and the theoretical error and the calculated error are in good agreement. |
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Bibliography: | GNSS refection technique; sea surface height; specular reflection point; error propagation; ocean altimetry As a new remote sensing technology, the global navigation satellite system(GNSS) reflection signals can be used to collect the information of ocean surface wind, surface roughness and sea surface height. Ocean altimetry based on GNSS reflection technique is of low cost and it is easy to obtain large amounts of data thanks to the global navigation satellite constellation. We can estimate the sea surface height as well as the position of the specular reflection point. This paper focuses on the study of the algorithm to determine the specular reflection point and altimetry equations to estimate the sea surface height over the reflection region. We derive the error equation of sea surface height based on the error propagation theory. Effects of the Doppler shift and the size of the glistening zone on the altimetry are discussed and analyzed at the same time. Finally, we calculate the sea surface height based on the simulated GNSS data within the whole day and verify the sea surface height errors according to the satellite elevation angles. The results show that the sea surface height can reach the precision of 6 cm for elevation angles of 55° to 90°, and the theoretical error and the calculated error are in good agreement. 32-1441/P GUO Jin-yun , WANG Shu-yang , LIU Xin , WANG Jian-bo and CHANG Xiao-tao (a College of Geodesy and Geomatics, Shandong University of Science and Technology, Qingdao 266590, China b Key Laboratory of Surveying and Mapping Technology on Island and ReefofNASMG, Qingdao 266590, China Satellite Surveying and Mapping Application Center of NASMG, Beijing 101300, China) |
ISSN: | 0890-5487 2191-8945 |
DOI: | 10.1007/s13344-015-0066-3 |