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

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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

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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

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,El Niño 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