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Effects of South China Sea/western North Pacific summer monsoon on tropospheric biennial oscillation (TBO)
Zheng Bin, Gu De-Jun, Lin Ai-Lan, Li Chun-Hui
2007, 16 (5):
1472-1476.
doi: 10.1088/1009-1963/16/5/051
Abstract
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PDF (191KB)
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Several theories have been developed to explain tropical biennial
oscillation (TBO), as an air--sea interactive system to impact Asian
and global weather and climate,
and some models have been established to produce a TBO. A
simple 5-box model, with almost all the key processes associated with
TBO, can produce a TBO by including air--sea interactions in the
monsoon regions. Despite that, the South China Sea/western North
Pacific summer monsoon (SCS/WNPSM), a very important monsoon
subsystem, is neglected. In this paper, based on the dynamical
framework of 5-box model, the term of SCS/WNPSM has been added and a
6-box model has been developed. Comparing the difference of TBO
sensibilities with several key parameters, air--sea coupling
coefficient α, SST-thermocline feedback coefficient
γ and wind-evaporation feedback coefficient λ,
between the modified model and original model, TBO is more sensible
to the parameters in the new model. The results imply that the
eastern Pacific and local wind-evaporation play more important roles
in the TBO when including SCS/WNPSM.
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