Articles | Volume 17, issue 17
https://doi.org/10.5194/acp-17-10467-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-17-10467-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
07 Sep 2017
Research article |
| 07 Sep 2017
Dominance of climate warming effects on recent drying trends over wet monsoon regions
Chang-Eui Park
School of Environmental Science and Engineering, South University of
Science and Technology of China, Shenzhen 518055, China
Su-Jong Jeong
CORRESPONDING AUTHOR
School of Environmental Science and Engineering, South University of
Science and Technology of China, Shenzhen 518055, China
Chang-Hoi Ho
School of Earth and Environmental Sciences, Seoul National University,
Seoul, 08826, South Korea
Hoonyoung Park
School of Earth and Environmental Sciences, Seoul National University,
Seoul, 08826, South Korea
Shilong Piao
Key Laboratory of Alpine Ecology and Biodiversity, Institute of
Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China
Sino-French Institute for Earth System Science, College of Urban and
Environmental Sciences, Peking University, Beijing 100871, China
Center for Excellence in Tibetan Earth Science, Chinese Academy of
Sciences, Beijing 100085, China
Jinwon Kim
Department of Atmospheric and Oceanic Sciences, University of
California, Los Angeles, CA 90024, USA
Song Feng
Department of Geosciences, University of Arkansas, Fayetteville, AR 72701, USA
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Cited
14 citations as recorded by crossref.
- Shifts in Dry-Wet Climate Regions over China and Its Related Climate Factors between 1960–1989 and 1990–2019 J. Xu et al. 10.3390/su14020719
- Amplification of Coupled Hot‐Dry Extremes Over Eastern Monsoon China X. Zhang et al. 10.1029/2023EF003604
- Spatiotemporal variations of aridity in China during 1961–2015: decomposition and attribution C. Liu et al. 10.1016/j.scib.2018.07.007
- Wetting trend in Northwest China reversed by warmer temperature and drier air H. Deng et al. 10.1016/j.jhydrol.2022.128435
- Indicators for evaluating trends of air humidification in arid regions under circumstance of climate change: Relative humidity (RH) vs. Actual water vapour pressure (ea) Q. Wei et al. 10.1016/j.ecolind.2020.107043
- Land surface processes response to warming and wetting trend in Northwest China X. Ma et al. 10.1088/1748-9326/ad70cd
- 我国西北干旱区“暖湿化”问题及其未来趋势讨论 发. 陈 et al. 10.1360/SSTe-2022-0405
- Discussion of the “warming and wetting” trend and its future variation in the drylands of Northwest China under global warming F. Chen et al. 10.1007/s11430-022-1098-x
- Spatiotemporal variations of meteorological drought and its dominant factors in different climate regions for the first two decades of the twenty-first century Y. Xing et al. 10.1007/s00704-024-04833-w
- Land Surface Temperature Sensitivity to Changes in Vegetation Phenology Over Northern Deciduous Forests C. Park & S. Jeong 10.1029/2023JG007498
- Dominant factor of dry‐wet change in China since 1960s J. Xu et al. 10.1002/joc.6728
- Dynamic Evolution and Copula-Based Multivariable Frequency Analysis of Meteorological Drought Considering the Spatiotemporal Variability in Northwestern China W. Zhang et al. 10.3390/w15213861
- Changes in aridity and its driving factors in China during 1961–2016 L. Liu et al. 10.1002/joc.5781
- Impacts of climate change and human activity on the potential distribution of Aconitum leucostomum in China L. Xu et al. 10.1016/j.scitotenv.2023.168829
14 citations as recorded by crossref.
- Shifts in Dry-Wet Climate Regions over China and Its Related Climate Factors between 1960–1989 and 1990–2019 J. Xu et al. 10.3390/su14020719
- Amplification of Coupled Hot‐Dry Extremes Over Eastern Monsoon China X. Zhang et al. 10.1029/2023EF003604
- Spatiotemporal variations of aridity in China during 1961–2015: decomposition and attribution C. Liu et al. 10.1016/j.scib.2018.07.007
- Wetting trend in Northwest China reversed by warmer temperature and drier air H. Deng et al. 10.1016/j.jhydrol.2022.128435
- Indicators for evaluating trends of air humidification in arid regions under circumstance of climate change: Relative humidity (RH) vs. Actual water vapour pressure (ea) Q. Wei et al. 10.1016/j.ecolind.2020.107043
- Land surface processes response to warming and wetting trend in Northwest China X. Ma et al. 10.1088/1748-9326/ad70cd
- 我国西北干旱区“暖湿化”问题及其未来趋势讨论 发. 陈 et al. 10.1360/SSTe-2022-0405
- Discussion of the “warming and wetting” trend and its future variation in the drylands of Northwest China under global warming F. Chen et al. 10.1007/s11430-022-1098-x
- Spatiotemporal variations of meteorological drought and its dominant factors in different climate regions for the first two decades of the twenty-first century Y. Xing et al. 10.1007/s00704-024-04833-w
- Land Surface Temperature Sensitivity to Changes in Vegetation Phenology Over Northern Deciduous Forests C. Park & S. Jeong 10.1029/2023JG007498
- Dominant factor of dry‐wet change in China since 1960s J. Xu et al. 10.1002/joc.6728
- Dynamic Evolution and Copula-Based Multivariable Frequency Analysis of Meteorological Drought Considering the Spatiotemporal Variability in Northwestern China W. Zhang et al. 10.3390/w15213861
- Changes in aridity and its driving factors in China during 1961–2016 L. Liu et al. 10.1002/joc.5781
- Impacts of climate change and human activity on the potential distribution of Aconitum leucostomum in China L. Xu et al. 10.1016/j.scitotenv.2023.168829
Latest update: 30 May 2025
Short summary
In dry monsoon regions, a decrease in precipitation induces drying trends. In contrast, the increase in potential evapotranspiration due to increased atmospheric water-holding capacity, a secondary impact of warming, works to increase aridity over the humid monsoon regions despite the increase in precipitation. Our results explain the recent drying in the humid monsoon regions. This also supports the drying trends over the warm and water-sufficient regions in future climate.
In dry monsoon regions, a decrease in precipitation induces drying trends. In contrast, the...
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