Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/3643
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dc.contributor.authorPandey, R. P.-
dc.contributor.authorRamasastri, K. S.-
dc.date.accessioned2019-09-26T11:56:23Z-
dc.date.available2019-09-26T11:56:23Z-
dc.date.issued2002-
dc.identifier.citationHydrological Sciences-Journul 47(8),August 2002en_US
dc.identifier.urihttp://117.252.14.250:8080/jspui/handle/123456789/3643-
dc.description.abstractDroughts are governed by regional climatic parameters. The ration of mean annual precipitation (Pa) to global terrestrial mean annual precipitation (Pg), and the ratio of mean annual potential evapotranspiration (Ep) to mean annual precipitation (Pa) have been used to define the climatic regions.en_US
dc.language.isoenen_US
dc.publisherTaylor & Francisen_US
dc.subjectDrought frequencyen_US
dc.subjectClimatic regionsen_US
dc.subjectPrecipitationen_US
dc.subjectPotential evapotranspiration (PET)en_US
dc.subjectMean annual deficiten_US
dc.titleIncidence of droughts in different climatic regionsen_US
dc.typeArticleen_US
Appears in Collections:Research papers in International Journals

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