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. 2017 Apr 27;7:1228. doi: 10.1038/s41598-017-01306-1

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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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(a–c) Regression slopes (dR95/K, %) obtained using rainfall from station (blue; for 1979–2013), TRMM (cyan; for 1998–2013) and CHIRPS (pink; for 1979–2013) data with (a) SAT, (b) DPT, and (c) T850, respectively for 1-hour, 3-hour and daily durations for Hyderabad using quantile regression (QR) at the 95th percentile, (d–f) same as (a–c) but for Chennai for period 2008–2013 for all the datasets. The figure was developed using the Generic Mapping Tools (GMT, https://www.soest.hawaii.edu/gmt/).