Is Accurate Synoptic Altimetry Achievable by Means of Interferometric GNSS-R?

被引:13
作者
Fabra, Fran [1 ,2 ]
Cardellach, Estel [1 ,2 ]
Ribo, Serni [1 ,2 ]
Li, Weiqiang [1 ,2 ]
Rius, Antonio [1 ,2 ]
Carlos Arco-Fernandez, Juan [1 ,2 ,5 ]
Nogues-Correig, Oleguer [1 ,2 ,6 ]
Praks, Jaan [3 ]
Rouhe, Erkka [3 ]
Seppanen, Jaakko [3 ,7 ]
Martin-Neira, Manuel [4 ]
机构
[1] CSIC, ICE, Inst Space Sci, Earth Observat Res Grp, Barcelona 08193, Spain
[2] IEEC, Barcelona 08034, Spain
[3] Aalto Univ, Dept Elect & Nanoengn, Espoo 02150, Finland
[4] European Space Agcy, European Space Res & Technol Ctr, NL-2200 AG Noordwijk, Netherlands
[5] ERNI Consulting Spain, Barcelona 08002, Spain
[6] Spire Global UK Ltd, Glasgow G3 8JU, Lanark, Scotland
[7] Finnish Meteorol Inst, FI-00101 Helsinki, Finland
关键词
GNSS-R; altimetry; interferometry; radar; GPS; Galileo; sea level; OCEAN ALTIMETRY; GPS SIGNALS; REFLECTOMETRY; SCATTERING; PARIS;
D O I
10.3390/rs11050505
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This paper evaluates the capability of interferometric global navigation satellite system reflectometry (GNSS-R) to perform sea surface altimetry in a synoptic scenario. Such purpose, which requires the combination of the results from different GNSS signals, constitutes a unique characteristic of this approach. Interferometric GNSS-R group delay altimetry has been proven to be more precise than conventional GNSS-R. However, the self-consistency and accuracy of their synoptic solutions (simultaneous multi-static results) have never been proved before. In our work, we analyze a dataset of GNSS signals reflected off the Baltic Sea acquired during an airborne campaign using a receiver that was developed for such a purpose. Among other features, it enables beamformer capability in post-processing to get multiple and simultaneous GNSS signals under the interferometric approach's restrictions. In particular, the signals from two GPS and two Galileo satellites, at two frequency bands (L1 and L5), covering an elevation range between 28 degrees and 83 degrees, are processed to retrieve sea surface height estimations. The results obtained are self-consistent among the different GNSS signals and data tracks, with discrepancies between 0.01 and 0.26 m. Overall, they agree with ancillary information at 0.40 m level, following a characteristic height gradient present at the experimental site.
引用
收藏
页数:19
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