Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean
By Anil Kumar Gupta, David Morrill Anderson, J. Overpeck. Nature, 2003
1,224 citations recorded by the source corpus.
Subfields: Atmospheric Science, Ecology, Environmental Chemistry
View Paper: https://www.semanticscholar.org/paper/8281947f0c70b03870644fa131ad4fcb05b1f291
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- R. Nigam
- D. K. Naik
- R. Saraswat
- Andreas Mackensen
- R. Seager
- David Morrill Anderson
- Simon Brewer
- Anil Kumar Gupta
In Ecology
In Environmental Chemistry
Citations in the corpus
- Millennial temperature reconstruction intercomparison and evaluation (2006, neutral): “Additional funding was provided as follows: from the UK Natural Environment Research Council for M. N. Juckes, K. R. Briffa and T. J. Osborn; from the Swedish Research Council for A. Moberg.”
- Adaptation and human migration, and evidence of agriculture coincident with changes in the Indian summer monsoon during the Holocene (2006, background): “Gupta et al.12 point out that throughout the Holocene, weak monsoon events coincide with cool periods in the North Atlantic when ice rafting was more extensive41, supporting the hypothesis that changes in the circum-North Atlantic have a downstream influence on the Indian monsoon (Figure 1).”
- El Niño as a mediator of the solar influence on climate (2007, background): “, 2005], and anoxic sediments off the coast of Oman [Gupta et al., 2003], converge to a coherent depiction of the Indian and Asian monsoons: In all these records,”
- Orbital forcing and role of the latitudinal insolation/temperature gradient (2009, background): “LTG control of Monsoon extent could also explain observed sub-orbital teleconnections between high latitude cooling events and aridity in Monsoon regions (Blunier et al. 1998; Gupta et al. 2003).”
- Deglaciation in the tropical Indian Ocean driven by interplay between the regional monsoon and global teleconnections (2013, background): “The deglacial WMI is interpreted as the result of cold anomalies generated by sea ice feedbacks in the North Atlantic.”