Why does The konkan coast experiences orographic rainfall
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Enhanced observational information on the spatial
distribution of rainfall, at a finer resolution, is vital for
evaluation of mesoscale models. The present study
examines the daily rainfall data from a high-density
mesoscale rain gauge network consisting of 25 stations
within a hundred sq. km. area, during the south west
monsoon season (June–September) for the period 1996–
2000. The rainfalls reported are from lake catchments
along the Western Ghats, falling in the district of Raigad
and other urban locations in and around Mumbai. Us-
ing this data-set, an attempt has been made to examine
the spatial distribution of heavy rainfall events. Poor
correlations between stations indicate that they cannot
be pooled together during spatial averaging for repre-
senting rainfall over the area. Heavy rainfall events
contributed largest rainfall amounts at the foothills of
the ghats and the least for sites on the Western ghats
at higher altitudes. The results suggest that different
controls modulate the synoptic situations to produce a
spectrum of spatial and temporal precipitation vari-
ability on local scales, which would require further ob-
servational and modeling efforts to understand and
predict.
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Answer:
The Konkan Coast experiences orographic rainfall because the monsoon winds which blow over the Arabian Sea strike the western side of the Western Ghats resulting in heavy rainfall. By the time these winds reach the Eastern Ghats, they are already dry as they have already shed their moisture.
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