Paleoclimatic reconstruction from the late pleistocene holocene sedimentary archives of Ladakh himalaya

Abstract

The climate which is as old as the earth itself has been ever changing as a newlineresponse to change in composition, energy and circulation of the atmosphere. The newlinecurrent understanding of climate and its variation which are based on barely three newlinecentury old instrumental data is insufficient to assess the wider pattern, major forcing newlineand its effects. newline