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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. 2 — Evolution of moisture transport leading to widespread extreme precipitation events. Composite evolution of moisture transport (kg m⁻¹ s⁻¹, vectors) and a, b specific humidity (g kg⁻¹, colors), c moisture advection (10⁻⁶ g kg⁻¹ s⁻¹, colors) and d moisture convergence (10⁻⁵ g kg⁻¹ s⁻¹, colors), leading to widespread extreme precipitation events (more than ten grid cells with daily rainfall ≥ 150 mm) over central India (on 0-day). Daily data for the period 1982–2015 is used for the composite analysis, based on NCEP (a, c, d) and ERA-Interim reanalysis (b). The analysis is for vertically integrated (1000–200 hPa) values for summer (June–September)