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Please use this identifier to cite or link to this item:
http://krishi.icar.gov.in/jspui/handle/123456789/32954
Full metadata record
DC Field | Value | Language |
---|---|---|
dc.contributor.author | ICAR_CRIDA | en_US |
dc.date.accessioned | 2020-02-25T09:25:22Z | - |
dc.date.available | 2020-02-25T09:25:22Z | - |
dc.date.issued | 2005-01-01 | - |
dc.identifier.citation | Not Available | en_US |
dc.identifier.issn | Not Available | - |
dc.identifier.uri | http://krishi.icar.gov.in/jspui/handle/123456789/32954 | - |
dc.description | Not Available | en_US |
dc.description.abstract | Drought is temporary reduction in water or moisture availability significantly below the normal amount for a specific period. It is a climatic anomaly characterized by deficient supply of moisture resulting either from sub-normal rainfall, erratic rainfall distribution, higher water need or a combination of all the 3 factors. Droughts, in general, are extreme hydrologic events causing acute water shortages which persist long enough to trigger detrimental effects on human, vegetation, animals and ecosystem over a considerable area. To a meteorologist, drought is the absence of rain, while to the agriculturist it is the deficiency of soil moisture in the crop root zone to support crop growth and productivity. Based on the criteria, concept of its utilization and different schools of thought, drought is broadly categorized into meteorological drought, hydrological drought, agricultural drought and socio-economic drought. In rainfed areas, drylands are more prone to ‘drought’. Since last one decade of 21st Century, it has been observed that monsoon rains are deviating much from its predictions and the states/regions which never experience such a natural calamity comes under mild to acute drought–prone regions. In cases of field crops and other vegetation, it creates moisture-stress conditions when the amount of water needed for evapotranspiration exceeds the total amount of moisture available in soil. To define, drought is taken to have occurred over an area where the annual average rainfall is less than 50–75% of the normal south–west (S–W) monsoon rains. Delayed onset of S– W monsoon rains or early receding of monsoon rains towards half–way of the season or long gaps between 2 heavy and effective rains during rainy season are the general phenomenon of agricultural drought in India. The India Meteorological Department (IMD) generally predicts the monsoon status (weak or normal) 3–4 months before for each state/region. In this article, the nature, impacts of recent agricultural droughts in India and mitigation strategies are reviewed | en_US |
dc.description.sponsorship | Not Available | en_US |
dc.language.iso | English | en_US |
dc.publisher | ICAR_CRIDA | en_US |
dc.relation.ispartofseries | Not Available; | - |
dc.subject | Drought, Impacts of drought, Drought mitigation strategies | en_US |
dc.title | Drought mitigation strategies in rainfed regions of India | en_US |
dc.title.alternative | Drought mitigation strategies in rainfed regions of India | en_US |
dc.type | Book | en_US |
dc.publication.projectcode | Not Available | en_US |
dc.publication.journalname | Not Available | en_US |
dc.publication.volumeno | Not Available | en_US |
dc.publication.pagenumber | Not Available | en_US |
dc.publication.divisionUnit | Not Available | en_US |
dc.publication.sourceUrl | Not Available | en_US |
dc.publication.authorAffiliation | ICAR_CRIDA | en_US |
dc.ICARdataUseLicence | http://krishi.icar.gov.in/PDF/ICAR_Data_Use_Licence.pdf | en_US |
Appears in Collections: | NRM-CRIDA-Publication |
Files in This Item:
File | Description | Size | Format | |
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Drought mitigation strategies in rainfed regions of India.pdf | 397.89 kB | Adobe PDF | View/Open |
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