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. 2022 Jan 17;12:823. doi: 10.1038/s41598-022-04807-w

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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 licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence 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 licence, visit http://creativecommons.org/licenses/by/4.0/.

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(a) 12-h accumulated precipitation (mm) in case CTRL over Taiwan during 12:00–23:00 UTC on July 30, 2017. Contours indicate the terrain height (m). (b) Area-mean (22.5–24° N, 119.5–121° E) of the time series of hub-height wind speed in case 356-WTs (denoted by the grey line, m s⁻¹), 10-m divergence (purple line, s⁻¹, left axis) and atmospheric stability (brown line, left axis) calculated from model levels 1 (~ 17 m) and 6 (~ 198 m) close to the rotor disk (28–192 m) in case 356-WTs (23.9–24.2° N, 120.0–120.1° E), and precipitation (black solid line, mm, left axis) of case 356-WTs and CTRL (black dashed line, mm, left axis), and the differences of precipitation (red dashed line, mm, right axis), hub-height wind speed (green dashed line, m s⁻¹, right axis) and hub-height water vapor (blue dashed line, g kg⁻¹, right axis) during 01:00–23:00 UTC on July 30, 2017. Maps and plots were produced using NCAR Command Language (NCL) version 6.6.2³⁷.