Titlebook: Intraseasonal Variability in the Atmosphere-Ocean Climate System; William K. M. Lau,Duane E. Waliser Book 2005 Springer-Verlag Berlin Heid

Resign

South Asian monsoon,nd system (Figure 2.1(b, e) (.); (.)). The winds at low levels during the summer monsoon season are characterized by the strongest westerlies anywhere at 850 hPa over the Arabian Sea, known as the low-level westerly jet (LLJ) (Figure 2.1e), and a large-scale cyclonic vorticity extending from the nor

隼鷹

糾纏

Pan-America,culture, hydroelectric power, and to maintain their waterways. Rainfall over Pan-America has large interannual variability (IAV) and intraseasonal variability (ISV). In the interannual band, El Nino Southern Oscillation (ENSO) has strong impact on total seasonal rainfall (., .) over the region, whil

ASSAY

seduce

infarct

收養(yǎng)

正常

,El Ni?o Southern Oscillation connection,tion (ENSO) is the most dominant interannual climate phenomenon in the tropical ocean-atmosphere system. Both MJO and ENSO involve major shifts in tropical convection, large-scale circulation, and weather patterns around the world. The hypothesis that the MJO and ENSO may be intrinsically linked was

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Microaneurysm