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. 2017 Oct 3;8:708. doi: 10.1038/s41467-017-00744-9

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© The Author(s) 2017

Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/.

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Fig. 5 — Evolution of temperature, pressure and winds leading to widespread extreme precipitation events. Composite evolution of a sea surface temperature (SST) and b air temperature (850–500 hPa) anomalies (colors, °C), c mean sea level pressure (MSLP, colors, Pa) and wind (vectors, m s⁻¹), leading to widespread extreme precipitation events over central India (on 0-day). Daily data from OISST and NCEP reanalysis, for the period 1982–2015 is used for the composite analysis