Amplifying population exposure of extreme precipitation across Yellow River Basin, China at 1.5° C, 2.0° C and 3.0° C global warming

被引:0
|
作者
Yao, Rui [1 ,2 ,3 ]
Ma, Zice [1 ,4 ]
Sun, Peng [1 ,2 ,3 ]
Ge, Chenhao [1 ]
机构
[1] Anhui Normal Univ, Sch Geog & Tourism, Wuhu 241002, Peoples R China
[2] Anhui Normal Univ, State Key Lab Earth Surface Proc & Resource Respon, Wuhu 241002, Peoples R China
[3] Anhui Normal Univ, Engn Technol Res Ctr Resources Environm & GIS, Wuhu 241002, Peoples R China
[4] Chuzhou Univ, Sch Comp & Informat Engn, Chuzhou, Peoples R China
基金
中国国家自然科学基金;
关键词
Extreme precipitation; Population exposure; Global warming; Statistical downscaling; Yellow River Basin; TEMPERATURE-CHANGES; FUTURE CHANGES; TRENDS; PERFORMANCE; RAINFALL; INCREASE; REACHES; INDEXES; IMPACT; HEAT;
D O I
10.1007/s11069-025-07161-y
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Intensified extreme precipitation events are expected in a warming climate, yet the specific impacts of such events at 1.5 degrees C, 2.0 degrees C, and 3.0 degrees C global warming levels on socioeconomic factors in the Yellow River Basin (YRB), China, remain unclear. This study investigates population exposure (PE) to extreme precipitation under these warming scenarios using downscaled and bias-corrected outputs from the latest Coupled Model Intercomparison Project phase 6 (CMIP6) and population data aligned with shared socioeconomic pathways (SSPs). Our findings indicate that while extreme precipitation is concentrated in the upper YRB, the population exposure in these areas is relatively low. In contrast, under 3.0 degrees C global warming, the lower YRB experiences a PE that is 7.57 and 3.11 times higher than under 1.5 degrees C and 2.0 degrees C warming, respectively. The total change in population exposure (PETC), primarily influenced by the population change effect (PCE), shows a significant decrease, estimated at -234 people/km(2) at the 3.0 degrees C warming level, due to migration or population decline mitigating the hazards of extreme precipitation. The climate change effect (CCE) is identified as the primary driver of PETC across the YRB. These results suggest that limiting global warming to between 1.5 degrees C and 2.0 degrees C could significantly reduce the PETC for extreme precipitation events in the YRB.
引用
收藏
页数:20
相关论文
共 50 条
  • [41] Climate change impacts on Canadian yields of spring wheat, canola and maize for global warming levels of 1.5 °C, 2.0 °C, 2.5 °C and 3.0 °C
    Qian, Budong
    Zhang, Xuebin
    Smith, Ward
    Grant, Brian
    Jing, Qi
    Cannon, Alex J.
    Neilsen, Denise
    McConkey, Brian
    Li, Guilong
    Bonsal, Barrie
    Wan, Hui
    Xue, Li
    Zhao, Jun
    ENVIRONMENTAL RESEARCH LETTERS, 2019, 14 (07)
  • [42] Future water security in the major basins of China under the 1.5 °C and 2.0 °C global warming scenarios
    Zhai, Ran
    Tao, Fulu
    Chen, Yi
    Dai, Huichao
    Liu, Zhiwu
    Fu, Bojie
    SCIENCE OF THE TOTAL ENVIRONMENT, 2022, 849
  • [43] Projection of actual evapotranspiration using the COSMO-CLM regional climate model under global warming scenarios of 1.5 °C and 2.0 °C in the Tarim River basin, China
    Su, Buda
    Jian, Dongnan
    Li, Xiucang
    Wang, Yanjun
    Wang, Anqian
    Wen, Shanshan
    Tao, Hui
    Hartmann, Heike
    ATMOSPHERIC RESEARCH, 2017, 196 : 119 - 128
  • [44] The Warming of the Tibetan Plateau in Response to Transient and Stabilized 2.0°C/1.5°C Global Warming Targets
    Jintao Zhang
    Qinglong You
    Fangying Wu
    Ziyi Cai
    Nick Pepin
    Advances in Atmospheric Sciences, 2022, 39 : 1198 - 1206
  • [45] The Warming of the Tibetan Plateau in Response to Transient and Stabilized 2.0°C/1.5°C Global Warming Targets
    Zhang, Jintao
    You, Qinglong
    Wu, Fangying
    Cai, Ziyi
    Pepin, Nick
    ADVANCES IN ATMOSPHERIC SCIENCES, 2022, 39 (07) : 1198 - 1206
  • [46] Projecting Changes in Rainfall Extremes for the Huai River Basin in the Context of 1.5 °C and 2 °C Global Warming
    Wang, Yueyang
    Wang, Yanjun
    Wang, Yan
    Ju, Qin
    Jin, Junliang
    Bao, Zhenxin
    ATMOSPHERE, 2022, 13 (10)
  • [47] Impacts of Global Warming of 1.5, 2.0 and 3.0 °C on Hydrologic Regimes in the Northeastern U.S.
    Siddique, Ridwan
    Mejia, Alfonso
    Mizukami, Naoki
    Palmer, Richard N.
    CLIMATE, 2021, 9 (01) : 1 - 18
  • [48] Increased Exposure of China's Cropland to Droughts under 1.5 °C and 2 °C Global Warming
    Miao, Lijuan
    Zhang, Jing
    Kattel, Giri Raj
    Liu, Ran
    ATMOSPHERE, 2022, 13 (07)
  • [49] Population exposure to compound dry and hot events in China under 1.5 and 2°C global warming
    Wu, Xinying
    Hao, Zengchao
    Tang, Qiuhong
    Zhang, Xuan
    Feng, Sifang
    Hao, Fanghua
    INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2021, 41 (12) : 5766 - 5775
  • [50] Drought losses in China might double between the 1.5 °C and 2.0 °C warming
    Su, Buda
    Huang, Jinlong
    Fischer, Thomas
    Wang, Yanjun
    Kundzewicz, Zbigniew W.
    Zhai, Jianqing
    Sun, Hemin
    Wang, Anqian
    Zeng, Xiaofan
    Wang, Guojie
    Tao, Hui
    Gemmer, Marco
    Li, Xiucang
    Jiang, Tong
    PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2018, 115 (42) : 10600 - 10605