Scientific Assembly of the International Association of Geodesy (IAG), Beijing, Çin, 28 Haziran - 02 Temmuz 2021, ss.1
Sea level is a key
component of climate change and plays an important role in the hydrological
cycle. Rising sea levels have significant impacts such as environmental, social,
and economic along with coastal areas. Global Navigation Satellite System
Interferometric Reflectometry (GNSS-IR) enables to retrieve sea level heights
using the reflected signal. Moreover, GNSS-IR is considered a promising alternative
to conventional tide gauges. This study focuses on the determination of
meteorological and tidal effects on GNSS reflected signals from the sea
surface. We used Signal-to-Noise Ratio
(SNR) data from the MERS IGS (International GNSS Service) network station
located on the Mediterranean coast of Turkey. Time series of SNR data were
analyzed to determine sea level variations. The various meteorological
parameters such as temperature, air pressure, and wind speed, which were acquired
from the nearby Erdemli tide gauge operated by the Turkish National Sea Level
Monitoring System (TUDES), were utilized. Furthermore, tidal harmonic analysis
was applied to both MERS station and Erdemli tide gauge to calculate tidal constituents
which are an important parameter for the investigation of sea level variations.
For this stage, tidal constituents were used
including annual constituent, semi-annual term, long-term constituents, diurnal
tides, semi-diurnal tides, third-diurnal tides, sixth-diurnal tides, quarter-diurnal
tides, and third-diurnal tide. We compared the tidal constituents estimated
from GNSS-IR and tide gauge observations. On the other hand, SNR amplitudes
were compared to meteorological and tide parameters to investigate the effect
on GNSS reflected signals from the sea surface. The results of meteorological
parameters have shown that as temperature increases the SNR amplitudes decrease
in the Mediterranean coasts of Turkey. In tidal harmonic analysis, the annual
constituent (SA) is the largest tidal constituent with an amplitude higher than
11 cm.