Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/36211
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dc.contributor.authorSen, A K-
dc.contributor.authorKarmakar, P K-
dc.contributor.authorDevbarman, S-
dc.contributor.authorGupta, A K Dev-
dc.contributor.authorGupta, M K Das-
dc.contributor.authorCalla, O P N-
dc.contributor.authorRana, S S-
dc.date.accessioned2016-10-26T07:24:23Z-
dc.date.available2016-10-26T07:24:23Z-
dc.date.issued1991-10-
dc.identifier.issn0975-105X (Online); 0367-8393 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/36211-
dc.description347-350en_US
dc.description.abstractBelow 30 GHz, the thermal emission line of water vapour in the atmosphere occurs at 22.235 GHz. An estimate of attenuation and hence of water vapour scale height has been made at this frequency. The results show that both these attain a maximum value in the month of August and a minimum in the month of December over Calcutta. With the help of attenuation data and corresponding water vapour scale height data, the vertical distribution of water vapour density has been made over the same place.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJRSP Vol.20(5) [October 1991]en_US
dc.titleTropospheric water vapour modelling over a tropical location by radiometric studyen_US
dc.typeArticleen_US
Appears in Collections:IJRSP Vol.20(5) [October 1991]

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