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DOI | 10.1007/s00382-018-4327-8 |
Precipitable water and CAPE dependence of rainfall intensities in China | |
Dong W.; Lin Y.; Wright J.S.; Xie Y.; Yin X.; Guo J. | |
发表日期 | 2019 |
ISSN | 0930-7575 |
起始页码 | 3357 |
结束页码 | 3368 |
卷号 | 52期号:2020-05-06 |
英文摘要 | The influence of temperature on precipitation in China is investigated from two aspects of the atmospheric water cycle: available water vapor and atmospheric instability. Daily observations are used to analyze how rainfall intensities and its spatial distribution in mainland China depend on these two aspects. The results show that rainfall intensities, and especially rainfall extremes, increase exponentially with available water vapor. The efficiency of water vapor conversion to rainfall is higher in northwestern China where water vapor is scarce than in southeastern China where water vapor is plentiful. The results also reveal a power law relationship between rainfall intensity and convective instability. The fraction of convective available potential energy (CAPE) converted to upward velocity is much larger over southeastern China than over the arid northwest. The sensitivities of precipitation to temperature-induced changes in available water vapor and atmospheric convection are thus geographically reciprocal. Specifically, while conversion of water vapor to rainfall is relatively less efficient in southeastern China, conversion of CAPE to upward kinetic energy is more efficient. By contrast, in northwestern China, water vapor is efficiently converted to rainfall but only a small fraction of CAPE is converted to upward motion. The detailed features of these relationships vary by location and season; however, the influences of atmospheric temperature on rainfall intensities and rainfall extremes are predominantly expressed through changes in available water vapor, with changes in convective instability playing a secondary role. © 2018, Springer-Verlag GmbH Germany, part of Springer Nature. |
英文关键词 | Available water vapor; China; Convective instability; Rainfall intensity |
语种 | 英语 |
scopus关键词 | air temperature; convective system; potential energy; precipitation (climatology); precipitation intensity; rainfall; spatial distribution; temperature effect; water vapor; China |
来源期刊 | Climate Dynamics |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/146466 |
作者单位 | Ministry of Education Key Laboratory for Earth System Modeling, Department of Earth System Science, and Joint Center for Global Change Studies (JCGCS), Tsinghua University, Beijing, 100084, China; ERT, Inc., at NOAA National Climatic Data Center, Asheville, NC 28801, United States; State Key Laboratory of Severe Weather and Key Laboratory of Atmospheric Chemistry of China Meteorological Administration (CMA), Chinese Academy of Meteorological Sciences, Beijing, 100081, China |
推荐引用方式 GB/T 7714 | Dong W.,Lin Y.,Wright J.S.,et al. Precipitable water and CAPE dependence of rainfall intensities in China[J],2019,52(2020-05-06). |
APA | Dong W.,Lin Y.,Wright J.S.,Xie Y.,Yin X.,&Guo J..(2019).Precipitable water and CAPE dependence of rainfall intensities in China.Climate Dynamics,52(2020-05-06). |
MLA | Dong W.,et al."Precipitable water and CAPE dependence of rainfall intensities in China".Climate Dynamics 52.2020-05-06(2019). |
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