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- W2187676155 abstract "Failure of southwest monsoon rainfall during 2002 highlighted again the need for examining the impact of intense low pressure systems (Tropical depression and above) over North West Pacific (NWP) on Indian Summer Monsoon Rainfall (ISMR) with a longer series of data. Month wise tracks of NWP intense low pressure systems, located west of 140°east from June to September for 38 years from 1963 have been considered. These include 27 All India normal/excess and 11 deficient monsoon years. These data have been analyzed with All India monsoon rainfall (AIMR) of the same years. It has been observed that NWP systems located west of 120°east and AIMR are positively correlated with correlation coefficient (CC) of +0.368. When an NWP system is located west of 120°east and a low pressure area (LPA) is observed over the Bay, monsoon depression (MD) forms over the Bay, otherwise an LPA forms over the Bay. Under these conditions east-west trough is seen up to 500 hPa and it continues up to the NWP system. The situation enhances the rainfall activity over India. It has been also observed that excess cyclone genesis over Northwest Pacific during summer monsoon is not the cause of monsoon failure over the country. Correlation coefficient (CC), computed between AIMR and total number of systems that crossed 30° north, are negatively correlated (-0.438). Both types of correlation coefficients suggest that NWP systems influence ISMR in both ways but they can not alter normal/ excess monsoon conditions into deficient monsoon conditions and vice versa." @default.
- W2187676155 created "2016-06-24" @default.
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- W2187676155 date "2011-01-01" @default.
- W2187676155 modified "2023-09-27" @default.
- W2187676155 title "Some aspects of the influence of North West Pacific systems on Indian Summer Monsoon Rainfall" @default.
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