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. 2022 Mar 11;13:1288. doi: 10.1038/s41467-022-28911-7

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© The Author(s) 2022

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. 6 — a The Z200 (unit: m) and b precipitation responses (mm/day) in the CESM1 to two additional heating sources added in tropical Western and Central Pacific. The green (10°S-0°, 110°E-150°E) and brown (0°-10°N, 120°E-80°W) color-filled ovals imposed in a denote the location where a pair of positive and negative heating sources are added in the CESM1. The cross-hatched areas in a and b denote the significant differences between the CTL and SEN experiments (Methods section) based on the two-sample t-test, p < 0.05.