量化全球降水的空间不均匀性变化
ID:521 View Protection:ATTENDEE Updated Time:2025-03-31 10:21:15 Hits:520 Oral Presentation

Start Time:2025-04-20 09:45(Asia/Shanghai)

Duration:15min

Session:S3-6 专题3.6 气候环境与数学 » S3-6专题3.6 气候环境与数学

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Abstract
The spatial inhomogeneity of changes in global precipitation, which is directly related to extreme flooding or drought events, represents a significant feature of climate change. To date, limited studies quantified the spatial inhomogeneity of global precipitation and its long-term change. Aiming at solving the above challenge, this study introduces a novel but simple methodological framework that is able to (1) quantify the spatial inhomogeneity of global precipitation and its variability, (2) estimate contributions of different precipitation intensities and (3) assess contributions of different regions. In this framework, the spatial inhomogeneity is quantified by the spatial variance of gridded precipitation normalized by the global mean precipitation, namely spatial coefficient of variation (SCV). Then, the spatial probability density function (PDF) of precipitation intensity is introduced to identify contributions of different precipitation intervals that lead to changes in global precipitation inhomogeneity. Finally, the global inhomogeneity can be decomposed into intra-regional and inter-regional inhomogeneity components to estimate the contributions from different regions.
The result shows that the inhomogeneity of global annual precipitation has increased consistently across multiple datasets in the satellite era (1979–2021), attributed to the increasing area of both extremely high and low precipitation. Based on the Global Precipitation Climatology Project (GPCP V2.3) dataset, the increase in inhomogeneity of global annual precipitation is primarily contributed by the intra-regional inhomogeneity component of Northern Hemispheric tropical ocean (+ 60.2%) and Southern Hemispheric tropical ocean (+ 40.3%), and is partly offset by the inter-regional inhomogeneity component of Northern Hemispheric mid-latitude ocean (− 4.5%). This study demonstrates how the spatial inhomogeneity of global precipitation can be easily estimated, which is implications for quantifying, monitoring, and understanding changes in climate extremes. Our framework offers a tool for dataset or model assessment, particularly useful for the regions susceptible to extreme precipitation events.
Keywords
气候变化,空间方差,空间变异系数,概率密度函数,降水
Speaker
刘升源
博士研究生 广东海洋大学

Submission Author
刘升源 广东海洋大学
梁卓轩 国防科技大学
徐建军 广东海洋大学深圳研究院
张邦林 国防科技大学
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  • Conference Date

    Apr 17

    2025

    to

    Apr 21

    2025

  • Apr 10 2025

    Draft paper submission deadline

  • Apr 28 2025

    Registration deadline

Sponsored By
中国科学院大气物理研究所
Organized By
中国科学院大气物理研究所
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