Millennial to centennial-scale climate oscillations since 15000 cal yrs BP from Kanwar wetland in the Central Ganga Plain, India

Author:

Phartiyal BinitaORCID,Tiwari ArvindORCID,Kawsar Masud,M.C Manoj,Shekhar Mayank,Ali S. Nawaz,Bhushan Ravi,Pachchigar Rujal R.,Kumar Anurag,K Prasanna,Sharma AnupamORCID

Funder

Birbal Sahni Institute of Palaeosciences

Publisher

Elsevier BV

Reference137 articles.

1. Late quaternary to Holocene southwest Monsoon reconstruction: a review based on Lake and Wetland systems (studies carried out during 2011-2016);Achyuthan;Proceedings of the Indian National Science Academy,2016

2. Paleoclimatic, palaeovegetational and provenance change in the Ganga Plain during the late Quaternary;Agrawal;J. Earth Syst. Sci.,2013

3. Role of surface hydrology in determining the seasonal cycle of Indian summer monsoon in a general circulation model;Agrawal;Hydrol. Earth Syst. Sci. Discuss.,2016

4. The role of sodium hexametaphosphate in the dissolution process of kaolinite and kaolin;Andreola;J. Eur. Ceram. Soc.,2004

5. Impact of the Indian Ocean dipole on the relationship between the Indian monsoon rainfall and ENSO;Ashok;Geophys. Res. Lett.,2001

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