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Holocene Variations of Monsoon Rainfall in Rajasthan

Bryson, R. A., Swain, A. M.·1981·Quaternary Research

Abstract

Two reconstructed histories of the monsoon rainfall in Rajasthan show that the monsoon was weak or absent in latest glacial time. With the advent of Holocene climatic patterns, fresh water lakes formed in dune fields and the pollen rain preserved in these reservoirs provides a basis for the reconstruction of the monsoon history. The two reconstructions, separated by only 150 km, have some features in common and some striking differences. Both show maximum monsoon amounts in the early Holocene, with a roughly two-thirds decrease to the present. Both show salinization in sub-Boreal time. Both show long intervals of near complete desiccation in the last four millennia. The shorter term variations, however, are not closely parallel. These shorter term variations may be explained in terms of the behavior of the present day interannual variability.

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Metadata

Authors
Bryson, R. A., & Swain, A. M.
Venue
Quaternary Research
Published
1981-09
Volume
16
Issue
2
Pages
135-145
ISSN
  • 0033-5894 (ISSN-L)
  • 1096-0287
OpenAlex
W1989408884
Cited by
237
References
0
FWCI
5.59
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Holocene Variations of Monsoon Rainfall in Rajasthan. https://app.cochat.ai/papers/10.1016/0033-5894(81)90041-7
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Bryson, R. A., & Swain, A. M. (1981). Holocene Variations of Monsoon Rainfall in Rajasthan. Quaternary Research. https://doi.org/10.1016/0033-5894(81)90041-7

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