R
Rengaswamy Ramesh
Researcher at Physical Research Laboratory
Publications - 204
Citations - 13261
Rengaswamy Ramesh is an academic researcher from Physical Research Laboratory. The author has contributed to research in topics: Monsoon & Holocene. The author has an hindex of 40, co-authored 200 publications receiving 11718 citations. Previous affiliations of Rengaswamy Ramesh include Indian Council of Agricultural Research & April.
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Book Chapter
The Physical Science Basis
E. Jansen,J Overpeck,Keith R. Briffa,J. C. Duplessy,F. Joos,Masson-Delmotte,Daniel Olago,B. Otto-Bliesner,W. R. Peltier,Stefan Rahmstorf,Rengaswamy Ramesh,D Raynud,D Rind,O Solomina,Ricardo Villalba,De Zhang +15 more
Book ChapterDOI
Information from paleoclimate archives
Valérie Masson-Delmotte,Michael Schulz,Ayako Abe-Ouchi,Juerg Beer,Andrey Ganopolski,J F Gonzáles Rouco,Eystein Jansen,Kurt Lambeck,Jürg Luterbacher,Tim R Naish,Timothy J. Osborn,Bette L. Otto-Bliesner,T Quinn,Rengaswamy Ramesh,Maisa Rojas,X Shao,Axel Timmermann +16 more
Journal ArticleDOI
High-Resolution Holocene Environmental Changes in the Thar Desert, Northwestern India
Yehouda Enzel,Lisa L. Ely,Sheila Mishra,Rengaswamy Ramesh,Rivka Amit,Boaz Lazar,S. N. Rajaguru,Victor R. Baker,Amir Sandler +8 more
TL;DR: Sediments from Lunkaransar dry lake in northwestern India reveal regional water table and lake level fluctuations over decades to centuries during the Holocene that are attributed to changes in the southwestern Indian monsoon rains as mentioned in this paper.
Journal ArticleDOI
Strontium isotopes and rubidium in the Ganga-Brahmaputra river system: Weathering in the Himalaya, fluxes to the Bay of Bengal and contributions to the evolution of oceanic87Sr/86Sr
TL;DR: In this paper, the concentrations of Rb and Sr and87Sr/86Sr isotopic ratios have been measured in the dissolved load of the Ganga-Brahmaputra (G-B) river system.
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A δ 13 C record of late Quaternary climate change from tropical peats in southern India
TL;DR: In this article, the authors present a δ13C record spanning the past 20 kyr from peats in the Nilgiri hills, southern India, and observe the key climate shifts that are already known to have occurred during the last glacial maximum (18 kyr ago) and the subsequent deglaciation.