Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/4176
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dc.contributor.authorसिंह, दिगम्बर-
dc.contributor.authorकुमार, ए. आर. सेंथिल-
dc.contributor.authorअरोड़ा, मनोहर-
dc.contributor.authorसिंह, ओमकार-
dc.contributor.authorअल्लका, नागेश्वर-
dc.date.accessioned2020-03-05T05:29:35Z-
dc.date.available2020-03-05T05:29:35Z-
dc.date.issued2019-
dc.identifier.urihttp://117.252.14.250:8080/jspui/handle/123456789/4176-
dc.description.abstractEvapotranspiration is an important component of hydrological cycle- It plays an important role for crop selection. Hence, accurate estimation of ET is essential. The ET varies from 4mm to 6mm per month for arid to semi & and areas in India. The temperature, wind speed, humidity and solar radiation are mainly required for the estimation of the evapotranspiration rates. In this connection, various ET methods (viz., Penman Monteith, Hargreaves, Turc, Priestley and Tailor, Jenson etc.) are mainly available for estimation. In this study, available meteorological data of Roorkee area for the year 1987 & 2018 has been used. In present study, the average monthly ET were estimated in the order of 4.6 mm (3.4 mm - 6-9 mm) and 4.3 mm (4.34 ram-4.37 mm) as per Penman Monteith and Hargreaves methods respectively. Penman Monteith method of ET estimation was found as best method in this study.en_US
dc.language.isootheren_US
dc.publisherराष्ट्रीय जलविज्ञान संस्थानen_US
dc.subjectEvapotranspirationen_US
dc.subjectHydrological cycleen_US
dc.titleप्रपत्र-1.5-विभिन्न वाष्पोत्सर्जन विधियों द्वारा रुड़की क्षेत्र के लिए वाष्पोत्सर्जन दरों का तुलनात्मक अध्ययनen_US
dc.typeTechnical Reporten_US
Appears in Collections:छठवीं राष्ट्रीय जल संगोष्ठी - जल संसाधन एवं पर्यावरण, 16-17 दिसंबर 2019



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