Japan Geoscience Union Meeting 2018

Presentation information

[JJ] Poster

A (Atmospheric and Hydrospheric Sciences) » A-TT Technology &Techniques

[A-TT32] Brand-new geoscientific observations by GNSS-Reflectometry

Mon. May 21, 2018 1:45 PM - 3:15 PM Poster Hall (International Exhibition Hall7, Makuhari Messe)

convener:Kaoru Ichikawa(Research Institute for Applied Mechanics, Kyushu University), Kosuke Heki(Department of Earth and Planetary Sciences, Faculty of Science, Hokkaido University)

[ATT32-P03] Wind-independent periodic variations of signal intensity of a geostationary GNSS satellite observed at an ocean observation tower

*Tatsuki Okumura1, Kaoru Ichikawa1, Takuji Ebinuma2, Ziyuan Li3, Masanori Konda4, Yutaka Yoshikawa4, Yasuyuki Baba5 (1.Research Institute for Applied Mechanics, Kyushu University, 2.College of Engineering, Chubu University, 3.Shenzhen Marine Monitoring and Forecast Center, 4.Graduate School of science, Kyoto University, 5.Disaster Prevention Research Institute, Kyoto University)

Keywords:geostationary GNSS satellite, GNSS-R, wind-independent periodic variation, interferometric intensity variation, path length change, tide

GNSS-R receivers were deployed to the Shirahama Oceanographic Observatory Tower owned by Kyoto University (33deg 42’32”N, 135deg 19’58”E) at the height of 20 m. The signal intensity, measured as signal-to-noise ratio (SNR), of a geostationary GNSS satellite (Beidou #2) was observed every second for both directly-received signals and signals reflected at the sea surface. In general, the SNR of the reflected signal fluctuates larger than that of the direct signal. Even after removal of high-frequency fluctuations by 3-minute smoothing, the SNR of the reflected signal shows larger changes, and these changes tend to be inversely correlated with the wind speed, which are consistent with less reflection by rougher sea surface. However, the SNR of the reflected signal intermittently shows significant periodic variations whose cycle is about one hour. These variations are not synchronized with variations of the wind speed, and they are observed only when the wind is weaker than 4m/s. Furthermore, similar variations were commonly found even in the direct signal. Therefore, they are considered mutual effects between direct and reflected signals, or interferometric intensity variations. Since the phase of the reflected signal depends on the path length, the tidal sea level changes would cause the path length, and thus interferometric SNR intensity. The path length change calculated from the sea level observed by a tide gauge at the tower provides consistent interferometric variation as the observed SNR.