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Quantification of Rainfall during the Late Miocene–Early Pliocene in North East India


Affiliations
1 Birbal Sahni Institute of Palaeosciences, 53 University Road, Lucknow 226 007, India
2 Dr H. S. Gour Vishwavidyalaya, Sagar 470 003, India
 

The monsoon rainfall contributes about 30% of the total global rainfall. The Asian monsoon system (ASM) is one of the largest systems and is of great significance in the global climate system. It consists of two subsystems, namely Indian summer monsoon (ISM)/southwest (SW) monsoon/South Asia summer monsoon (SASM) and East Asia monsoon (EAM).
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  • Quantification of Rainfall during the Late Miocene–Early Pliocene in North East India

Abstract Views: 428  |  PDF Views: 127

Authors

Gaurav Srivastava
Birbal Sahni Institute of Palaeosciences, 53 University Road, Lucknow 226 007, India
R. P. Tiwari
Dr H. S. Gour Vishwavidyalaya, Sagar 470 003, India
R. C. Mehrotra
Birbal Sahni Institute of Palaeosciences, 53 University Road, Lucknow 226 007, India

Abstract


The monsoon rainfall contributes about 30% of the total global rainfall. The Asian monsoon system (ASM) is one of the largest systems and is of great significance in the global climate system. It consists of two subsystems, namely Indian summer monsoon (ISM)/southwest (SW) monsoon/South Asia summer monsoon (SASM) and East Asia monsoon (EAM).

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DOI: https://doi.org/10.18520/cs%2Fv113%2Fi12%2F2253-2257