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dc.contributor.authorRameshKumar, M.R.
dc.contributor.authorSadhuram, Y.
dc.date.accessioned1995-06-25T10:01:50Z
dc.date.accessioned2017-09-30T01:29:55Z
dc.date.available1995-06-25T10:01:50Z
dc.date.available2017-09-30T01:29:55Z
dc.date.issued1989
dc.identifier.citationMeteorology and Atmospheric Physics, vol.41; 1989; 87-97
dc.identifier.issn0177-7971
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/7193
dc.description.abstractMonthly mean surface fields of different meteorological parameters and evaporation are studied for the 1979 (poor monsoon) and 1983 (good monsoon) monsoon seasons over the Arabian Sea, in order to understand the role of evaporation on the Indian monsoon rainfall. It is noticed that in general, the sea surface temperatures are higher in 1983 throughout the monsoon season than in 1979 in the Arabian Sea excepting western region. The mean rates of evaporation on a seasonal scale are found to be equal in both years (3.66 x 10 super(10) tons/day in 1979 and 1983, respectively). No coherence is observed between the evaporation and the west coast rainfall within a season. It is also noted that the pressure distribution over the Arabian Sea is even important to advect the moisture towards the west coast of India, through winds
dc.languageen
dc.publisherSpringer
dc.relation.ispartofMeteorol Atmos Phys
dc.relation.isreferencedbySCI
dc.subjectOceanography and Limnology
dc.subject.othermonsoons
dc.subject.otherseasonal variations
dc.subject.otherevaporation
dc.subject.otherISW, Arabian Sea
dc.titleEvaporation over the Arabian Sea during two contrasting monsoons
dc.typeJournal Article


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