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Analysis sea-air interaction of the tropical cyclones ...

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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.
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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.

OUTLINE

Introduction

Data & Method

Result & Discussion

Conclusion

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

INDONESIA GEOGRAPHICALPOSITION

ASIA

AUSTRALIA

HINDIA OCEAN

PACIFIC OCEAN

Equator

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

Result and Discussion TC KIRRILY 2009

SST Anomaly Monthly and Week

https://www.esrl.noaa.gov/psd/data/gridded/data.noaa.oisst.v2.highres.html#detail

92

193

TC LILI 2019

In Maluku Barat Daya Island

SST Anomaly 155 157

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

Terima KasihThank you. Question?

“ Weather Satellite for Better Future”


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