Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/35632
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dc.contributor.authorChatterjee, R N-
dc.contributor.authorPrakash, Prem-
dc.contributor.authorAli, Kaushar-
dc.contributor.authorKapoor, R K-
dc.date.accessioned2016-10-10T10:19:33Z-
dc.date.available2016-10-10T10:19:33Z-
dc.date.issued1996-02-
dc.identifier.issn0975-105X (Online); 0367-8393 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/35632-
dc.description8-14en_US
dc.description.abstractSome characteristics of the precipitation echoes from layer type clouds in Delhi region have been studied using radar observations made during 1960-1962. The study showed that the height of the layer echoes first observed varied between 3.0 and 13.0 km. Mean height of the first observed layer echoes was about 8 km in summer (April-June), 10 km during monsoon (July-September) and 7 km during winter (November-March). The depth of these echoes have been found to be usually in the range 0.5-6.0 km and horizontal extensions varied between wide limits ranging from 12 to 200 km. Occurrence of layer echoes preceded by convective development has been found to be maximum during summer while melting band feature occurred more frequently during monsoon. Rainfall rate and liquid water content I layer clouds as well as the percentage contribution towards season’s rainfall from such clouds have also been estimated.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.25(1) [February 1996]en_US
dc.titleCharacteristics of layer type radar echoes around Delhien_US
dc.typeArticleen_US
Appears in Collections:IJRSP Vol.25(1) [February 1996]

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