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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Format: | Theses |
Language: | Indonesia |
Online Access: | https://digilib.itb.ac.id/gdl/view/70754 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |
Summary: | 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
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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. |
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