Please use this identifier to cite or link to this item: http://117.252.14.250:8080/jspui/handle/123456789/3555
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dc.contributor.authorMolnar, L.-
dc.contributor.authorKubjatko, F.-
dc.date.accessioned2019-09-12T12:13:08Z-
dc.date.available2019-09-12T12:13:08Z-
dc.date.issued1992-
dc.identifier.urihttp://117.252.14.250:8080/jspui/handle/123456789/3555-
dc.description.abstractThe areal distribution of precipitations in mountains is described by means of precipitation gradients using long term standard network data and comparing them with the experimental catchment study. Presented results have proved the importance of more accurate determination of precipitation gradients, heavily depending on the location of the network stations, observational and mainly windy conditions within the catchment. Seasonality of precipitation gradients as well as redistribution of snow have also been documented.en_US
dc.language.isoenen_US
dc.publisherNational Institute of Hydrologyen_US
dc.title1.1-Determination of precipitation gradients in mountainsen_US
dc.typeTechnical Reporten_US
Appears in Collections:International Symposium on Hydrology of Mountainous Areas, 28-30 May 1992 at Shimla (India).

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