CHARACTERISTICS OF FREQUENCY SPECTRUM VARIATION OFINTRASEASONAL OSCILLATION OF CONVECTION DURINGSOUTH CHINA SEA SUMMER MONSOON

LIN Ai-lan; LIANG Jian-yin; LI Chun-hui

Abstract:

Datasets of equivalent temperature of black body (TBB) and sea surface temperature (SST) ranging from 1980 to 1997 are used to diagnose and analyze the characteristics of frequency spectrum and strength of intraseasonal variation of convection. The relationship between the strength of intraseasonal oscillation of convection, strength of convection itself and SST in the South China Sea (SCS) is studied. It is shown that, there are distinguishable annual, interannual and interdecadal variations in both strength and frequency spectrum of intraseasonal variation of convection in SCS. There are connections between strength of convection, strength of ISO1 in the summer half (s.h.) year and SST in ensuing winter half (w.h.) year in SCS. The strong (weak) convection and strong (weak) ISO1 are associated with negative (positive) bias of SST in ensuing w.h. year in SCS.

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LIN Ai-lan, LIANG Jian-yin, LI Chun-hui. CHARACTERISTICS OF FREQUENCY SPECTRUM VARIATION OFINTRASEASONAL OSCILLATION OF CONVECTION DURINGSOUTH CHINA SEA SUMMER MONSOON [J]. Journal of Tropical Meteorology, 2006, 12(1): 34-40.

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CHARACTERISTICS OF FREQUENCY SPECTRUM VARIATION OFINTRASEASONAL OSCILLATION OF CONVECTION DURINGSOUTH CHINA SEA SUMMER MONSOON

Guangzhou Institute of Tropical and Marine Meteorology, CMA

Abstract: Datasets of equivalent temperature of black body (TBB) and sea surface temperature (SST) ranging from 1980 to 1997 are used to diagnose and analyze the characteristics of frequency spectrum and strength of intraseasonal variation of convection. The relationship between the strength of intraseasonal oscillation of convection, strength of convection itself and SST in the South China Sea (SCS) is studied. It is shown that, there are distinguishable annual, interannual and interdecadal variations in both strength and frequency spectrum of intraseasonal variation of convection in SCS. There are connections between strength of convection, strength of ISO1 in the summer half (s.h.) year and SST in ensuing winter half (w.h.) year in SCS. The strong (weak) convection and strong (weak) ISO1 are associated with negative (positive) bias of SST in ensuing w.h. year in SCS.

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CHARACTERISTICS OF FREQUENCY SPECTRUM VARIATION OFINTRASEASONAL OSCILLATION OF CONVECTION DURINGSOUTH CHINA SEA SUMMER MONSOON

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