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Full metadata record
DC Field | Value | Language |
---|---|---|
dc.contributor.author | Pandey, R. P. | - |
dc.contributor.author | Ramasastri, K. S. | - |
dc.date.accessioned | 2019-09-26T11:56:23Z | - |
dc.date.available | 2019-09-26T11:56:23Z | - |
dc.date.issued | 2002 | - |
dc.identifier.citation | Hydrological Sciences-Journul 47(8),August 2002 | en_US |
dc.identifier.uri | http://117.252.14.250:8080/jspui/handle/123456789/3643 | - |
dc.description.abstract | Droughts 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.iso | en | en_US |
dc.publisher | Taylor & Francis | en_US |
dc.subject | Drought frequency | en_US |
dc.subject | Climatic regions | en_US |
dc.subject | Precipitation | en_US |
dc.subject | Potential evapotranspiration (PET) | en_US |
dc.subject | Mean annual deficit | en_US |
dc.title | Incidence of droughts in different climatic regions | en_US |
dc.type | Article | en_US |
Appears in Collections: | Research papers in International Journals |
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Restricted Acess.pdf | 411.81 kB | Adobe PDF | View/Open |
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