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  <title>DSpace Collection:</title>
  <link rel="alternate" href="http://117.252.14.250:8080/jspui/handle/123456789/4244" />
  <subtitle />
  <id>http://117.252.14.250:8080/jspui/handle/123456789/4244</id>
  <updated>2026-04-14T20:18:13Z</updated>
  <dc:date>2026-04-14T20:18:13Z</dc:date>
  <entry>
    <title>WSES-2-Evaporation from water bodies and its control</title>
    <link rel="alternate" href="http://117.252.14.250:8080/jspui/handle/123456789/4245" />
    <author>
      <name>Makwana, M. M.</name>
    </author>
    <id>http://117.252.14.250:8080/jspui/handle/123456789/4245</id>
    <updated>2025-11-13T04:36:13Z</updated>
    <published>1992-07-01T00:00:00Z</published>
    <summary type="text">Title: WSES-2-Evaporation from water bodies and its control
Authors: Makwana, M. M.
Abstract: Evaporation  of  water has an important role  in  the  hydrologic cycle of nature.  It is a natural process and occurs when  solar radiation falls on a water body and the energy so transmitted  is acquired by water molecules which in turn get separated and  move upward  causing  the evaporation phenomenon.   The loss   of   water from   water storage structures  like  reservoirs,  irrigation tanks  through  the  process  of evaporation causes considerable  reduction in storage.  The huge costs involved in the construction of these storage   structures   make it imperative to utilise  every  single drop  of  water stored.  Estimation of evaporation  loss in the country indicate that the annual evaporation from a water surface in  the semi-arid tropics is as high as 2000 mm. Annual  average value of evaporation ranges from 1400 mm to 1800 mm over a   large portion of the country.   More information about spatial variation of  evaporation reveals that values exceeding 2000 mm occur over west Rajasthan and parts of Saurashtra and Tamilnadu, while  less than 1400  mm is reported at coastal Mysore, Bihar  plateau  and east M.P.</summary>
    <dc:date>1992-07-01T00:00:00Z</dc:date>
  </entry>
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