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Effects of South China Sea/western North Pacific summer monsoon on tropospheric biennial oscillation (TBO) 总被引:2,自引:0,他引:2 下载免费PDF全文
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. 相似文献
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Interdecadal variability of the tropospheric biennial oscillation in the western North Pacific 下载免费PDF全文
The observed tropospheric biennial oscillation (TBO) in the western North Pacific (WNP) monsoon region has an interdecadal variability with a period of 40-50 yr. That suggests a weaker effect of the TBO on the East Asia followed by a stronger one. A simple analytic model was designed to investigate the mechanism of the interdecadal variability of the TBO. The results indicated that a local TBO air-sea system not only supports the TBO variability in the WNP monsoon region but also produces an interdecadal variability of the TBO. 相似文献
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