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Meehl [ 24 ] noted that a tropospheric biennial mechanism involving air-sea interactions was connected with the South Asian or Indian monsoon. Kuhnel [ 4 ] defined cloudband activity as a function of the southern oscillation index, which determines the strength and position of the main convective regions.


The NWCB formation region is located where the 40—50 day oscillation i. The decline has affected farming and other industries in coastal and inland regions. They found regions of convective mixing or strong upwelling that were susceptible to small changes in the throughflow.



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  1. NWCBs and convective activity also generate winter rainfall, but to a lesser degree [ 26 ]. Cloudband-related rainfall was also mostly limited to coastal areas, especially the west coast Figure 8 b.

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