JpGU-AGU Joint Meeting 2017

講演情報

[EE] 口頭発表

セッション記号 A (大気水圏科学) » A-AS 大気科学・気象学・大気環境

[A-AS06] [EE] 台風研究の新展開~過去・現在・未来

2017年5月20日(土) 09:00 〜 10:30 301B (国際会議場 3F)

コンビーナ:中野 満寿男(海洋研究開発機構)、和田 章義(気象研究所台風研究部)、金田 幸恵(名古屋大学宇宙地球環境研究所)、伊藤 耕介(琉球大学)、座長:伊藤 耕介(琉球大学)、座長:金田 幸恵(名古屋大学)

10:00 〜 10:15

[AAS06-05] ENSO control on Arabian Sea tropical cyclones in a changing climate

*vineet kumar singh1roxy mathew Koll1 (1.Indian Institute of Tropical meteorology)

キーワード:Pre-monsoon cyclones, ENSO, climate change

Tropical cyclones rarely occur in the Arabian Sea during the pre-monsoon month of May.
However, our analysis reveals that there has been a significant increase in the number of cyclones
in this region during the recent years. While the first half of the satellite era (1979-1996) saw a
single cyclone, the second half (1997-2014) witnessed an increase of up to six cyclones. We
investigate the mechanism and largescale conditions regulating the changes in cyclonic activity,
and explore if this increase in the frequency of cyclones will continue into the future. Our analysis
using observations and CMIP5 model simulations suggest an ENSO control on the pre-monsoon
tropical cyclones in the Arabian Sea. We find that La Niña-like conditions during the recent years
have resulted in an anomalous cyclonic circulation and reduced vertical wind shear in the Arabian
Sea via a modification of the Walker circulation, thereby providing favorable conditions for
cyclone genesis and development. This anomalous cyclonic circulation associated with the La
Niña conditions are observed throughout the middle troposphere (700-400 hPa). Nevertheless,
CMIP5 model projections suggest a 50% reduction in the number of tropical cyclones in the future
(2051-2100), as compared to the recent decades (1951-2000). Our analysis shows that this decrease
in cyclones is a response to the positive skewness towards El Niño like conditions in the future,
which results in an anomalous anticyclonic circulation in the Arabian Sea along with increase in
wind shear and decrease in relative humidity inhibiting the formation of cyclones in the region.