REMSS OISST is interpolated product based on microwave, IR channel.
If the satellite data is not continuous, the boundary will be very noise.
The situation is extreme in the region when the SST gradient is very high.
This case is Trami, so SST cooling is very obvious due to its slow translation speed.
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- Fri Nov 05, 2021 8:22 am
- Forum: ROMS Discussion
- Topic: Question about the typhoon-induced sea surface cooling in ROMS-WRF coupled simulation
- Replies: 3
- Views: 6328