Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/30597
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dc.contributor.authorPatil, M N-
dc.contributor.authorParasnis, S S-
dc.date.accessioned2015-02-23T11:03:13Z-
dc.date.available2015-02-23T11:03:13Z-
dc.date.issued2001-10-
dc.identifier.issn0975-105X (Online); 0367-8393 (Print)-
dc.identifier.urihttp://hdl.handle.net/123456789/30597-
dc.description266-272en_US
dc.description.abstractStability characteristics in the atmospheric surface layer over dry convection, moist convection and alternate deep moist/unsaturated convection zones of the monsoon trough have been explored using the tower data of wind and temperature obtained during monsoon trough boundary layer experiment (MONTBLEX). In general, different characteristics in three sub-layers of a 1-30 m layer were observed before, during and after the onset of monsoon. Before onset of the monsoon, 1-4 m layer was stably stratified over dry convection (western end) and moist convection (eastern end) zones of the monsoon trough. After the onset of monsoon, inversion in this layer was not noticed. These results may possibly be attributed to the local effect. 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.30(5) [October 2001]en_US
dc.titleOn the stability of atmospheric surface layer along the monsoon rough region over Indiaen_US
dc.typeArticleen_US
Appears in Collections: IJRSP Vol.30(5) [October 2001]

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