Application of GNSS interferometric reflectometry for detecting storm surges
A single geodetic GNSS station placed at the coast has the capability of a traditional tide gauge for sea-level measurements, with the additional advantage of simultaneously obtaining vertical land motions. The sea-level measurements are obtained using GNSS signals that have reflected off the water,...
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sg-ntu-dr.10356-813772020-09-26T21:25:22Z Application of GNSS interferometric reflectometry for detecting storm surges Peng, Dongju Hill, Emma M. Li, Linlin Switzer, Adam D. Larson, Kristine M. Asian School of the Environment Earth Observatory of Singapore GNSS-IR Super Typhoon Hato Science::Geology A single geodetic GNSS station placed at the coast has the capability of a traditional tide gauge for sea-level measurements, with the additional advantage of simultaneously obtaining vertical land motions. The sea-level measurements are obtained using GNSS signals that have reflected off the water, using analysis of the signal-to-noise ratio (SNR) data. For the first time, we apply this technique to detect extreme weather-induced sea-level fluctuations, i.e., storm surges. We first derive 1-year sea-level measurements under normal weather conditions, for a GNSS station located in Hong Kong, and compare them with traditional tide-gauge data to validate its performance. Our results show that the RMS difference between the individual GNSS sea-level measurements and tide-gauge records is about 12.6 cm. Second, we focus on the two recent extreme events, Typhoon Hato of 2017 and Typhoon Mangkhut of 2018, that are ranked the third and second most powerful typhoons hitting Hong Kong since 1954 in terms of maximum sea level. We use GNSS SNR data from two coastal stations to produce sea-level measurements during the two typhoon events. Referenced to predicted astronomical tides, the storm surges caused by the two events are evident in the sea-level time series generated from the SNR data, and the results also agree with tide-gauge records. Our results demonstrate that this technique has the potential to provide a new approach to monitor storm surges that complement existing tide-gauge networks. NRF (Natl Research Foundation, S’pore) MOE (Min. of Education, S’pore) Published version 2019-07-09T01:09:46Z 2019-12-06T14:29:35Z 2019-07-09T01:09:46Z 2019-12-06T14:29:35Z 2019 Journal Article Peng, D., Hill, E. M., Li, L., Switzer, A. D., & Larson, K. M. (2019). Application of GNSS interferometric reflectometry for detecting storm surges. GPS Solutions, 23(2). doi:10.1007/s10291-019-0838-y 1080-5370 https://hdl.handle.net/10356/81377 http://hdl.handle.net/10220/49184 10.1007/s10291-019-0838-y en GPS Solutions © 2019 The Author(s). This article is distributed under the terms of the Creative Commons Attribution 4.0 International License http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution, and reproduction in any medium, provided you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. 11p. application/pdf |
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GNSS-IR Super Typhoon Hato Science::Geology Peng, Dongju Hill, Emma M. Li, Linlin Switzer, Adam D. Larson, Kristine M. Application of GNSS interferometric reflectometry for detecting storm surges |
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A single geodetic GNSS station placed at the coast has the capability of a traditional tide gauge for sea-level measurements, with the additional advantage of simultaneously obtaining vertical land motions. The sea-level measurements are obtained using GNSS signals that have reflected off the water, using analysis of the signal-to-noise ratio (SNR) data. For the first time, we apply this technique to detect extreme weather-induced sea-level fluctuations, i.e., storm surges. We first derive 1-year sea-level measurements under normal weather conditions, for a GNSS station located in Hong Kong, and compare them with traditional tide-gauge data to validate its performance. Our results show that the RMS difference between the individual GNSS sea-level measurements and tide-gauge records is about 12.6 cm. Second, we focus on the two recent extreme events, Typhoon Hato of 2017 and Typhoon Mangkhut of 2018, that are ranked the third and second most powerful typhoons hitting Hong Kong since 1954 in terms of maximum sea level. We use GNSS SNR data from two coastal stations to produce sea-level measurements during the two typhoon events. Referenced to predicted astronomical tides, the storm surges caused by the two events are evident in the sea-level time series generated from the SNR data, and the results also agree with tide-gauge records. Our results demonstrate that this technique has the potential to provide a new approach to monitor storm surges that complement existing tide-gauge networks. |
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Asian School of the Environment |
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Asian School of the Environment Peng, Dongju Hill, Emma M. Li, Linlin Switzer, Adam D. Larson, Kristine M. |
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Article |
author |
Peng, Dongju Hill, Emma M. Li, Linlin Switzer, Adam D. Larson, Kristine M. |
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Peng, Dongju |
title |
Application of GNSS interferometric reflectometry for detecting storm surges |
title_short |
Application of GNSS interferometric reflectometry for detecting storm surges |
title_full |
Application of GNSS interferometric reflectometry for detecting storm surges |
title_fullStr |
Application of GNSS interferometric reflectometry for detecting storm surges |
title_full_unstemmed |
Application of GNSS interferometric reflectometry for detecting storm surges |
title_sort |
application of gnss interferometric reflectometry for detecting storm surges |
publishDate |
2019 |
url |
https://hdl.handle.net/10356/81377 http://hdl.handle.net/10220/49184 |
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1681056336504160256 |