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Theme-6-1-Agricultural meteorologic and hydrologic drought relations.

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dc.contributor.author Singh, K. P.
dc.contributor.author Ramamurthy, G. S.
dc.date.accessioned 2019-09-17T11:10:46Z
dc.date.available 2019-09-17T11:10:46Z
dc.date.issued 1988
dc.identifier.uri http://117.252.14.250:8080/jspui/handle/123456789/3585
dc.description.abstract Agricultural and hydrologic droughts affect a large segment of the population. Both have their roots,in meteorologic drought. Meteorologic drought occurs when precipitation over a large area is much below average for an extended period of time. Hydrologic drought (caused by low precipitation, substantial soil moisture deficits, ad high temperatures) occurs when streamflow in a given basin is much below average for several months and available water withdrawals are inadequate. Meteorologic and hydrologic factors can combine to substantially reduce crop yields, leading to an agricultural drought. Interrelationships among these droughts are investigated using long term historical data on precipitation, temperature, streamflow, and crop yields. en_US
dc.language.iso en en_US
dc.publisher National Institute of Hydrology en_US
dc.subject Agriculture en_US
dc.subject Meteorologic en_US
dc.subject Hydrologic en_US
dc.subject Drought en_US
dc.title Theme-6-1-Agricultural meteorologic and hydrologic drought relations. en_US
dc.type Technical Report en_US


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