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. 2017 Dec 11;7:17347. doi: 10.1038/s41598-017-17599-1

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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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Mechanisms of aerosol induced suppression: Reduced aerosol loading makes the atmosphere unstable causing reduced divergence of moisture and normal convection leading to uplift of moisture and subsequently normal precipitation. While in case of increased aerosol loading the divergence of moisture is enhanced accompanied with stable atmospheric conditions. Conflation of these effects suppresses the precipitation. Figure was created using CorelDRAW × 6 (www.coreldraw.com).