1.5 °C and 2.0 °C of global warming intensifies the hydrological extremes in China

被引:13
作者
Shu, Zhangkang [1 ,2 ,3 ,4 ]
Jin, Junliang [1 ,3 ,4 ]
Zhang, Jianyun [1 ,3 ,4 ]
Wang, Guoqing [1 ,3 ,4 ]
Lian, Yanqing [3 ,4 ]
Liu, Yanli [1 ,3 ,4 ]
Bao, Zhenxin [1 ,3 ,4 ]
Guan, Tiesheng [1 ,3 ,4 ]
He, Ruimin [1 ,3 ,4 ]
Liu, Cuishan [1 ,3 ,4 ]
Jing, Peiran [1 ,5 ]
机构
[1] Natl Key Lab Water Disaster Prevent, Nanjing 210029, Peoples R China
[2] Sichuan Univ, Coll Water Resource & Hydropower, State Key Lab Hydraul & Mt River Engn, Chengdu 610065, Peoples R China
[3] Yangtze Inst Conservat & Dev, Nanjing 210098, Peoples R China
[4] Minist Water Resources, Res Ctr Climate Change, Nanjing 210029, Peoples R China
[5] Wuhan Univ, State Key Lab Water Resources Engn & Management, Wuhan 430072, Peoples R China
基金
中国国家自然科学基金;
关键词
Extreme discharge; Climate change; 1.5 degrees C/2.0 degrees C warming targets; Acceleration; China; YELLOW-RIVER BASIN; CLIMATE-CHANGE; PRECIPITATION; STREAMFLOW; MODEL; CMIP5; DROUGHT; UNCERTAINTY; VARIABILITY; PERFORMANCE;
D O I
10.1016/j.jhydrol.2024.131229
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
Global warming has been shown to have a profound impact on hydrological process, especially on hydrological extremes. To avoid the potential risk of extreme hazards, it is essential to project changes in hydroclimatic extremes under the 1.5 degrees C and 2.0 degrees C targets of the Paris Agreement, especially in China, which is geographically, climatologically, economically, and socially complex. Here, this study projects future changes in hydroclimatic extremes in China under 1.5 degrees C and 2.0 degrees C warming targets based on a distributed hydrological model driven by an ensemble of downscaled general circulation models. The study shows that global warming of 1.5 degrees C and 2.0 degrees C would perceptibly affect the spatial patterns of extreme rainfall and extreme heat in China. The intensification of events such as extreme rainfall, meteorological drought, and extreme heat would intensify the hydrological extremes, including floods and hydrological droughts. The risk of future extreme floods and hydrological droughts will increase simultaneously, with a 34.6% (38.0%) probability of acceleration (more severe floods and droughts) in a 1.5 degrees C (2.0 degrees C) warming world. Correspondingly, global warming tends to exacerbate the water cycle, with a 92.5% (94.2%) probability that at least one extreme event will exhibit intensification characteristics in the 1.5 degrees C (2.0 degrees C) warming scenario. The acceleration of the water cycle and the intensification of the hydrological extremes may have adverse impacts on the balanced development of China 's ecological and economic society.
引用
收藏
页数:15
相关论文
共 50 条
  • [31] Additional risk in extreme precipitation in China from 1.5 °C to 2.0 °C global warming levels
    Li, Wei
    Jiang, Zhihong
    Zhang, Xuebin
    Li, Laurent
    Sun, Ying
    [J]. SCIENCE BULLETIN, 2018, 63 (04) : 228 - 234
  • [32] Changes in extreme temperature over China when global warming stabilized at 1.5 °C and 2.0 °C
    Sun, Cenxiao
    Jiang, Zhihong
    Li, Wei
    Hou, Qiyao
    Li, Laurent
    [J]. SCIENTIFIC REPORTS, 2019, 9 (1)
  • [33] Tibetan Plateau amplification of climate extremes under global warming of 1.5 °C, 2 °C and 3 °C
    You, Qinglong
    Wu, Fangying
    Shen, Liucheng
    Pepin, Nick
    Jiang, Zhihong
    Kang, Shichang
    [J]. GLOBAL AND PLANETARY CHANGE, 2020, 192 (192)
  • [34] Implications of differential effects between 1.5 and 2 °C global warming on temperature and precipitation extremes in China's urban agglomerations
    Yu, Rong
    Zhai, Panmao
    Lu, Yanyu
    [J]. INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2018, 38 (05) : 2374 - 2385
  • [35] Agricultural water demands in Central Asia under 1.5 °C and 2.0 °C global warming
    Li, Zhi
    Fang, Gonghuan
    Chen, Yaning
    Duan, Weili
    Mukanov, Yerbolat
    [J]. AGRICULTURAL WATER MANAGEMENT, 2020, 231 (231)
  • [36] Spatiotemporal variations of aridity index over the Belt and Road region under the 1.5°C and 2.0°C warming scenarios
    Zhou, Jian
    Jiang, Tong
    Wang, Yanjun
    Su, Buda
    Tao, Hui
    Qin, Jiancheng
    Zhai, Jianqing
    [J]. JOURNAL OF GEOGRAPHICAL SCIENCES, 2020, 30 (01) : 37 - 52
  • [37] Changes in fire weather climatology under 1.5 °C and 2.0 °C warming
    Son, Rackhun
    Kim, Hyungjun
    Wang, Shih-Yu
    Jeong, Jee-Hoon
    Woo, Sung-Ho
    Jeong, Ji-Yoon
    Lee, Byung-Doo
    Kim, Seung Hee
    LaPlante, Matthew
    Kwon, Chun-Geun
    Yoon, Jin-Ho
    [J]. ENVIRONMENTAL RESEARCH LETTERS, 2021, 16 (03):
  • [38] More robust changes in the East Asian winter monsoon from 1.5 to 2.0°C global warming targets
    Miao, Jiapeng
    Wang, Tao
    Chen, Dong
    [J]. INTERNATIONAL JOURNAL OF CLIMATOLOGY, 2020, 40 (11) : 4731 - 4749
  • [39] Short-term concurrent drought and heatwave frequency with 1.5 and 2.0°C global warming in humid subtropical basins: a case study in the Gan River Basin, China
    Zhang, Yuqing
    You, Qinglong
    Mao, Guangxiong
    Chen, Changchun
    Ye, Zhengwei
    [J]. CLIMATE DYNAMICS, 2019, 52 (7-8) : 4621 - 4641
  • [40] Impacts of global warming of 1.5 °C and 2.0 °C on precipitation patterns in China by regional climate model (COSMO-CLM)
    Sun, Hemin
    Wang, Anqian
    Zhai, Jianqing
    Huang, Jinlong
    Wang, Yanjun
    Wen, Shanshan
    Zeng, Xiaofan
    Su, Buda
    [J]. ATMOSPHERIC RESEARCH, 2018, 203 : 83 - 94