8-Climate Variability over the Western Himalaya Since The Little Ice Age - Dendroclimatic Implications.

dc.contributor.author	Pant, G. B.
dc.contributor.author	Borgaonkar, H. P.
dc.contributor.author	Kumar, K. Rupa
dc.date.accessioned	2022-06-02T19:48:23Z
dc.date.available	2022-06-02T19:48:23Z
dc.date.issued	2003
dc.identifier.uri	http://117.252.14.250:8080/jspui/handle/123456789/6832
dc.description.abstract	Information on long-term climate variability of western Himalayan region based on instrumental records and dendroclimatic investigation have been discussed. Instrumental records of monthly temperature and precipitation of 10 stations for about 100 years have been analysed to look into the pattern of climate variability during the 20th century. Wide network of tree-ring data of Himalayan conifers have been used to deduce climatic information beyond the instrumental period. Pre-monsoon (March-April-May) climate of western Himalaya reconstructed from tree-rings since AD 1747 do not show any impact of Little Ice Age in the later phase of the phenomenon.	en_US
dc.language.iso	en	en_US
dc.publisher	National Institute of Hydrology	en_US
dc.subject	Snow Hydrology	en_US
dc.subject	Climate	en_US
dc.subject	Western Himalaya	en_US
dc.title	8-Climate Variability over the Western Himalaya Since The Little Ice Age - Dendroclimatic Implications.	en_US
dc.type	Technical Report	en_US