High-Frequency Sea Level Variations Observed by GPS Buoys Using Precise Point Positioning Technique

In this study, sea level variation observed by a 1-Hz Global Positioning System (GPS) buoy system is verified by comparing with tide gauge records and is decomposed to reveal high-frequency signals that cannot be detected from 6-minute tide gauge records. Compared to tide gauges traditionally used t...

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Main Authors: Chung-Yen Kuo, Kuan-Wei Chiu, Kai-Wei Chiang, Kai-Chien Cheng, Li-Ching Lin, Hong-Zeng Tseng, Feng-Yu Chu, Wen-Hau Lan, Hsiang-Tseng Lin
Format: Article
Language:English
Published: Springer 2012-01-01
Series:Terrestrial, Atmospheric and Oceanic Sciences
Subjects:
Online Access: http://tao.cgu.org.tw/images/attachments/v232p209.pdf
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author Chung-Yen Kuo
Kuan-Wei Chiu
Kai-Wei Chiang
Kai-Chien Cheng
Li-Ching Lin
Hong-Zeng Tseng
Feng-Yu Chu
Wen-Hau Lan
Hsiang-Tseng Lin
author_facet Chung-Yen Kuo
Kuan-Wei Chiu
Kai-Wei Chiang
Kai-Chien Cheng
Li-Ching Lin
Hong-Zeng Tseng
Feng-Yu Chu
Wen-Hau Lan
Hsiang-Tseng Lin
author_sort Chung-Yen Kuo
collection DOAJ
description In this study, sea level variation observed by a 1-Hz Global Positioning System (GPS) buoy system is verified by comparing with tide gauge records and is decomposed to reveal high-frequency signals that cannot be detected from 6-minute tide gauge records. Compared to tide gauges traditionally used to monitor sea level changes and affected by land motion, GPS buoys provide high-frequency geocentric measurements of sea level variations. Data from five GPS buoy campaigns near a tide gauge at Anping, Tainan, Taiwan, were processed using the Precise Point Positioning (PPP) technique with four different satellite orbit products from the International GNSS Service (IGS). The GPS buoy data were also processed by a differential GPS (DGPS) method that needs an additional GPS receiver as a reference station and the accuracy of the solution depends on the baseline length. The computation shows the average Root Mean Square Error (RMSE) difference of the GPS buoy using DGPS and tide gauge records is around 3 - 5 cm. When using the aforementioned IGS orbit products for the buoy derived by PPP, its average RMSE differences are 5 - 8 cm, 8 - 13 cm, decimeter level, and decimeter-meter level, respectively, so the accuracy of the solution derived by PPP highly depends on the accuracy of IGS orbit products. Therefore, the result indicates that the accuracy of a GPS buoy using PPP has the potential to measure the sea surface variations to several cm. Finally, high-frequency sea level signals with periods of a few seconds to a day can be successfully detected in GPS buoy observations using the Ensemble Empirical Mode Decomposition (EMD) method and are identified as waves, meteotsunamis, and tides.
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spelling doaj.art-a425dc7f6c544f2f9064e2c05afb43312022-12-22T02:57:03ZengSpringerTerrestrial, Atmospheric and Oceanic Sciences1017-08392311-76802012-01-0123220910.3319/TAO.2011.10.05.01(Oc)1063High-Frequency Sea Level Variations Observed by GPS Buoys Using Precise Point Positioning TechniqueChung-Yen KuoKuan-Wei ChiuKai-Wei ChiangKai-Chien ChengLi-Ching LinHong-Zeng TsengFeng-Yu ChuWen-Hau LanHsiang-Tseng LinIn this study, sea level variation observed by a 1-Hz Global Positioning System (GPS) buoy system is verified by comparing with tide gauge records and is decomposed to reveal high-frequency signals that cannot be detected from 6-minute tide gauge records. Compared to tide gauges traditionally used to monitor sea level changes and affected by land motion, GPS buoys provide high-frequency geocentric measurements of sea level variations. Data from five GPS buoy campaigns near a tide gauge at Anping, Tainan, Taiwan, were processed using the Precise Point Positioning (PPP) technique with four different satellite orbit products from the International GNSS Service (IGS). The GPS buoy data were also processed by a differential GPS (DGPS) method that needs an additional GPS receiver as a reference station and the accuracy of the solution depends on the baseline length. The computation shows the average Root Mean Square Error (RMSE) difference of the GPS buoy using DGPS and tide gauge records is around 3 - 5 cm. When using the aforementioned IGS orbit products for the buoy derived by PPP, its average RMSE differences are 5 - 8 cm, 8 - 13 cm, decimeter level, and decimeter-meter level, respectively, so the accuracy of the solution derived by PPP highly depends on the accuracy of IGS orbit products. Therefore, the result indicates that the accuracy of a GPS buoy using PPP has the potential to measure the sea surface variations to several cm. Finally, high-frequency sea level signals with periods of a few seconds to a day can be successfully detected in GPS buoy observations using the Ensemble Empirical Mode Decomposition (EMD) method and are identified as waves, meteotsunamis, and tides. http://tao.cgu.org.tw/images/attachments/v232p209.pdf GPS buoyPrecise point positioningTide gaugeHigh-frequency sea level variation
spellingShingle Chung-Yen Kuo
Kuan-Wei Chiu
Kai-Wei Chiang
Kai-Chien Cheng
Li-Ching Lin
Hong-Zeng Tseng
Feng-Yu Chu
Wen-Hau Lan
Hsiang-Tseng Lin
High-Frequency Sea Level Variations Observed by GPS Buoys Using Precise Point Positioning Technique
Terrestrial, Atmospheric and Oceanic Sciences
GPS buoy
Precise point positioning
Tide gauge
High-frequency sea level variation
title High-Frequency Sea Level Variations Observed by GPS Buoys Using Precise Point Positioning Technique
title_full High-Frequency Sea Level Variations Observed by GPS Buoys Using Precise Point Positioning Technique
title_fullStr High-Frequency Sea Level Variations Observed by GPS Buoys Using Precise Point Positioning Technique
title_full_unstemmed High-Frequency Sea Level Variations Observed by GPS Buoys Using Precise Point Positioning Technique
title_short High-Frequency Sea Level Variations Observed by GPS Buoys Using Precise Point Positioning Technique
title_sort high frequency sea level variations observed by gps buoys using precise point positioning technique
topic GPS buoy
Precise point positioning
Tide gauge
High-frequency sea level variation
url http://tao.cgu.org.tw/images/attachments/v232p209.pdf
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