TIDE OBSERVATION USING GNSS REFLECTOMETRY METHOD

In defining the vertical datum, tide observation is used to obtain height by referring to mean sea level. Hitherto, tide observation can be carried out using two methods: 1) in-situ using tide gauge; and 2) satellite-based using altimeter satellite. However, implementation of these two methods in...

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Main Author: Syetiawan, Agung
Format: Theses
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/70754
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:70754
spelling id-itb.:707542023-01-20T09:46:43ZTIDE OBSERVATION USING GNSS REFLECTOMETRY METHOD Syetiawan, Agung Indonesia Theses sea level, multipath, GNSS Reflectometry, quality control INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/70754 In defining the vertical datum, tide observation is used to obtain height by referring to mean sea level. Hitherto, tide observation can be carried out using two methods: 1) in-situ using tide gauge; and 2) satellite-based using altimeter satellite. However, implementation of these two methods in coastal areas is still considered not optimal. This is due to the inadequate resolutions, both spatial and temporal, for complex and rapidly changing sea level observation. Currently, another alternative method is being developed to observe the sea level by utilizing the GNSS multipath signal. This method is known as GNSS Reflectometry. Unfortunately, there are still problems related to the accuracy and temporal resolution of the tides produced. Implementing quality control and adding satellite segments can improve accuracy and temporal resolution. The purpose of this research is to observe the sea level height from the reflected GNSS signal. GNSS Reflectometry technique utilizes multipath signals that have been considered as noise in precise GNSS measurements. The signal reflected by the sea is then analyzed using the Lomb- Scargle Periodogram (LSP) method. LSP calculates the vertical distance of the reflected plane surface based on the dominant frequency of the multipath signal from the peak value of the wave. Statistically, the estimated peak from one LSP shall not be considered as the accurate value. Therefore, the quality control process is used to increase the quality of the estimated reflector height. The results showed that the sensitivity of quality control greatly determines the final result of the tidal signal. Furthermore, the combination of GPS and GLONASS at the L1 and L2 frequencies produces a tide with an RMSe value of 8cm and a correlation of up to 97% when compared using tide gauge observations. Finally, the use of GNSS iii antenna installation at tidal stations provides another alternative in sea level monitoring. The GNSS-Reflectometry technique can be used as a complement to tide observations at the Geospatial Information Agency. text
institution Institut Teknologi Bandung
building Institut Teknologi Bandung Library
continent Asia
country Indonesia
Indonesia
content_provider Institut Teknologi Bandung
collection Digital ITB
language Indonesia
description In defining the vertical datum, tide observation is used to obtain height by referring to mean sea level. Hitherto, tide observation can be carried out using two methods: 1) in-situ using tide gauge; and 2) satellite-based using altimeter satellite. However, implementation of these two methods in coastal areas is still considered not optimal. This is due to the inadequate resolutions, both spatial and temporal, for complex and rapidly changing sea level observation. Currently, another alternative method is being developed to observe the sea level by utilizing the GNSS multipath signal. This method is known as GNSS Reflectometry. Unfortunately, there are still problems related to the accuracy and temporal resolution of the tides produced. Implementing quality control and adding satellite segments can improve accuracy and temporal resolution. The purpose of this research is to observe the sea level height from the reflected GNSS signal. GNSS Reflectometry technique utilizes multipath signals that have been considered as noise in precise GNSS measurements. The signal reflected by the sea is then analyzed using the Lomb- Scargle Periodogram (LSP) method. LSP calculates the vertical distance of the reflected plane surface based on the dominant frequency of the multipath signal from the peak value of the wave. Statistically, the estimated peak from one LSP shall not be considered as the accurate value. Therefore, the quality control process is used to increase the quality of the estimated reflector height. The results showed that the sensitivity of quality control greatly determines the final result of the tidal signal. Furthermore, the combination of GPS and GLONASS at the L1 and L2 frequencies produces a tide with an RMSe value of 8cm and a correlation of up to 97% when compared using tide gauge observations. Finally, the use of GNSS iii antenna installation at tidal stations provides another alternative in sea level monitoring. The GNSS-Reflectometry technique can be used as a complement to tide observations at the Geospatial Information Agency.
format Theses
author Syetiawan, Agung
spellingShingle Syetiawan, Agung
TIDE OBSERVATION USING GNSS REFLECTOMETRY METHOD
author_facet Syetiawan, Agung
author_sort Syetiawan, Agung
title TIDE OBSERVATION USING GNSS REFLECTOMETRY METHOD
title_short TIDE OBSERVATION USING GNSS REFLECTOMETRY METHOD
title_full TIDE OBSERVATION USING GNSS REFLECTOMETRY METHOD
title_fullStr TIDE OBSERVATION USING GNSS REFLECTOMETRY METHOD
title_full_unstemmed TIDE OBSERVATION USING GNSS REFLECTOMETRY METHOD
title_sort tide observation using gnss reflectometry method
url https://digilib.itb.ac.id/gdl/view/70754
_version_ 1822278856481964032