A case study of deviant El Niño influence on the 2023 monsoon: An anecdote involving IOD, MJO and equivalent barotropic rossby waves
Author:
Funder
Science and Engineering Research Board (SERB), Department of Science and Technology (DST), Government of India
Publisher
Springer Science and Business Media LLC
Link
https://link.springer.com/content/pdf/10.1007/s00382-024-07273-4.pdf
Reference112 articles.
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2. Alexander MA, Lau N-C, Scott JD (2004) Broadening the atmospheric bridge paradigm: ENSO teleconnections to the North Pacific in summer and to the tropical west Pacific-Indian oceans over the seasonal cycle. Vol. 147, Earth’s Climate: The Ocean-Atmosphere Interaction, Wang et al., Eds., Geophys. Monogr. Ser., AGU, Washington, D. C., 85–104. https://doi.org/10.1029/147GM05
3. Ambrizzi T, Hoskins BJ (1997) Stationary rossby-wave propagation in a baroclinic atmosphere. Q J R Meteorol Soc 123:919–928. https://doi.org/10.1002/qj.49712354007
4. Aneesh S, Bódai T (2024) Inter-model robustness of the forced change of the ENSO-Indian Summer Monsoon Teleconnection. NPJ Clim Atmos Sci 7:4. https://doi.org/10.1038/s41612-023-00541-w
5. Annamalai H, Xie SP, McCreary JP, Murtugudde R (2005) Impact of Indian Ocean Sea Surface Temperature on Developing El Niño*. J Clim 18:302–319. https://doi.org/10.1175/JCLI-3268.1
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