Evaluating the role of South Asian High on the transition phase of the Indian summer monsoon
Author:
Publisher
Springer Science and Business Media LLC
Subject
Atmospheric Science
Link
https://link.springer.com/content/pdf/10.1007/s00704-021-03890-9.pdf
Reference50 articles.
1. Abe M, Hori M, Yasunari T, Kitoh A (2013) Effects of the Tibetan Plateau on the onset of the summer monsoon in South Asia: the role of the air-sea interaction. J Geophys Res Atmos 118:1760–1776. https://doi.org/10.1002/jgrd.50210
2. Agrawal, N., Singh, B. B., and Pandey, V. K., (2021a) Fidelity of Regional Climate Model v4.6 in capturing seasonal and subseasonal variability of Indian summer monsoon. Dynamics of Atmospheres and Oceans. 94. https://doi.org/10.1016/j.dynatmoce.2021.101203.
3. Agrawal N, Pandey VK, Mishra SK, Pandey VS (2021b) Modeling seasonal trends in optimum temperatures over India. J Water Climate Change 12(5):1420–1436. https://doi.org/10.2166/wcc.2020.072
4. Carvalho LMV, Jones C, Cannon F, Norris J (2016) Intraseasonal-to-interannual variability of the Indian monsoon identified with the large-scale index for the Indian monsoon system (LIMS). J Climate 29:2941–2962. https://doi.org/10.1175/JCLI-D-15-0423.1
5. Cen S, Chen W, Chen S et al (2020) Potential impact of atmospheric heating over East Europe on the zonal shift in the South Asian high: the role of the Silk Road teleconnection. Sci Rep 10:6543. https://doi.org/10.1038/s41598-020-63364-2
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