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. 2017 Jul 11;7:5057. doi: 10.1038/s41598-017-05345-6

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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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Locations of the MERRA2 cells whose wet season precipitation is correlated statistically significantly at 90% confidence level with that of the corresponding stations (a). Vertical distributions of wet season precipitation (b), total column water vapor (TCWV) (c), convective available potential energy (CAPE) (d), and lifting condensation level (LCL) (e) with MERRA2 elevation for the MERRA2 cells that are separated into the same color-coded 5 groups as for the observations. This figure was plotted using the Generic Mapping Tools (GMT) V4.5.0 (https://www.soest.hawaii.edu/gmt/).