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RECENT DECLINE IN TYPHOON ACTIVITY IN THE SOUTH CHINA SEA. LEUNG, Y K WU, M C YEUNG, K K. Content. Observation: Decline in Typhoon (TY) & Category 4-5 TY activities in the South China Sea (SCS) in the last 10 years (1996-2005) Investigation: The causes of recent decline in TY activities
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RECENT DECLINE IN TYPHOON ACTIVITY IN THE SOUTH CHINA SEA LEUNG, Y K WU, M C YEUNG, K K
Content • Observation: • Decline in Typhoon (TY) & Category 4-5 TY activities in the South China Sea (SCS) in the last 10 years (1996-2005) • Investigation: • The causes of recent decline in TY activities • Interdecadal variations of Typhoons formed east of 120E in the Western North Pacific (WNP) • Shift of recent tropical cyclone (TC) tracks, possibly • due to a change in 500 hPa steering flow or SST in SCS • but not likely due to change in TC genesis locations
Data • Tropical cyclone (TC) best track data of • Hong Kong Observatory (HKO) • 1961-2005 • TC best track data of • Regional Specialized Meteorological Centre (RSMC) • 1977-2005 • Joint Typhoon Warning Centre (JTWC) • 1961-2005
East of 120E High Tropical Cyclone Activity Region( Western North Pacific Ocean & South China Sea ) 120E Hong Kong South ChinaSea Western North Pacific
TYs Gaussian filtered time serieswith periodicities of < 10 years CAT 4-5 TYs A decline in the recent 10 years (1996-2005) Anomaly in the annual number
Frequency Spectrum by Multitaper Method ( annual no. of TYs formed east of 120E)
more fewer TY track density
Difference in 500 hPa geopotential height Difference in the 500 hPa steering flow(1995-2005 mean)-(1961-1995 mean)
Average SST over (10-20 N, 110-120 E) Correlation with 500 hPa height Difference in SST (1996-2005 mean)-(1961-1995 mean)
Correlation coefficient Correlation between 500 hPa heights and the mean SST in the SCS
Summary of results • Typhoon (TY) activity in the South China Sea (SCS) has been found to decline since the mid-1990s. • Reasons for the Decline: • inter-decadal variations, i.e. fewer TYs were formed in the Western North Pacific (mid-1990s to 2005 being quieter period). • More TY tracks towards East China Sea and Japan than towards the SCS • Shift in TC tracks may be a result of a change in the mid-tropospheric flow, the latter of which correlates well with the rising mean SST of the South China Sea
Only 1 out of 14 typhoons occurred over South China Sea in 2002
Sea Surface Temperature (SCS) &500 hpa Geopotential Heights Trends