Indonesia Agency for Meteorology
Climatology and Geophysics (BMKG)
Pattimura Meteorological Station of Ambon
Senior Forecaster & Observer Staff
Rion Suaib Salman
Analysis sea-air interaction of the tropical cyclones Kirrily (2009) and Lili (2019) in the Banda Sea, Maluku region.
Introduction
- SST > 26℃- Ocean
- 5° and 30° latitude
Why me interested with this study?
- TC is a beautiful phenomenon
- Many small Island
- Banda Sea is Very large and deep
- Global impact factor
ASIA
AUSTRALIA
HINDIA OCEAN
PACIFIC OCEAN
Equator
Asia MonsoonAustralia Monsoon
Tropical Cyclone
ENSOIODITCZMJO
- New SATAID software from JMA- Sandwich product mixing with VS channel- GSM model from JMA (Vertical wind shear)
MTSAT-1 data
TC Kirrily 200926 – 28 April
Himawari-8 data
TC Lili 20196 – 8 May
NOAA Satellite
SST anomaly (VHRR)
Obsevation Data
Tual MeteorologicalStation
Obsevation Data
Saumlaki MeteorologicalStation
- New SATAID software from JMA- Sandwich product mixing with VS channel- GSM model from JMA (Vertical wind shear)
- GRADS software- SST Anomaly per month and week before- Interpretation
- Rainfall- Suddenly increasing
- Rainfall- Suddenly increasing
Data & Method
SST Anomaly Monthly and Week
https://www.esrl.noaa.gov/psd/data/gridded/data.noaa.oisst.v2.highres.html#detail
92
193
Conclusion
1/ Banda Sea has a big supply for the formation of tropicalcyclones.
2/ Although the anomaly SST totally different between twotropical cyclones but warm of the ocean gave us a prove thatSST becomes the main factor.
3/ After SST was constantly warm, that can make thedynamical atmospheric above the Banda Sea give a response(sea-air interaction).
Many thanks to:
- Mr. Bodo ZESCHKE (Center Vlabs, Melbourne) give us more experience & New knowledge of Meteorological Satellite with more study case and discussion.
- Mr. Aki SHIMITZU (JMA) develops SATAID software for us especially (Indonesia) in the tropical regions.
- Mr. Jeff Wilson & Mrs. Agnes Lane