Thermometers in the DONET seafloor cable seismic observation network detect synchronous ocean waves over more than 100 km
The Nankai Trough seafloor cable seismic observation network DONET is used for earthquake early warning and tsunami prediction. A thermometer is attached to each of these ocean bottom seismometers to measure the temperature near the seafloor. In this study, by investigating long-term ocean bottom temperature data, a research group of Yusuke Yokota (Associate Professor at #UTokyo_IIS), Tomohiro Inoue and Tatsuya Kubota (National Research Institute for Earth Science and Disaster Resilience) detected for the first time ocean waves fluctuating synchronously over an area of more than 100 km along the Nankai Trough. In oceanography, this may be a "Coastal Trapped Wave (CTW)" , and this is a rare observation case that shows the possibility of new oceanographic observations using the ocean bottom seismic observation network. The temperature change is very small, a phenomenon that cannot be detected by ocean bottom pressure gauges, and the signal is of a size that does not affect earthquake observations or slow slip observations in the Nankai Trough. In the future, if more accurate slow slip detection is implemented, it may become noise.