qnishida.bsky.social
@qnishida.bsky.social
地震学の研究者。
OSWs were excited at 4:00 UTC when the HTHH eruption. The OSWs lasted for half a day. The observed OSWs suggest a blowout of seawater above the summit and the inflow of seawater into the crater.
November 25, 2024 at 10:13 AM
After the HTHH eruption, we observed a clear dispersive wave propagation. The observed record in Japan (S-net) shows that the high-frequency arrivals were delayed with the frequency.
November 25, 2024 at 10:09 AM