Articles | Volume 12, issue 4
https://doi.org/10.5194/esd-12-1061-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esd-12-1061-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Climate change in the High Mountain Asia in CMIP6
Mickaël Lalande
CORRESPONDING AUTHOR
Univ. Grenoble Alpes, CNRS, IRD, G-INP, IGE, 38000 Grenoble, France
Martin Ménégoz
Univ. Grenoble Alpes, CNRS, IRD, G-INP, IGE, 38000 Grenoble, France
Gerhard Krinner
Univ. Grenoble Alpes, CNRS, IRD, G-INP, IGE, 38000 Grenoble, France
Kathrin Naegeli
Institute of Geography and Oeschger Center for Climate Change Research, University of Bern, 3012 Bern, Switzerland
Stefan Wunderle
Institute of Geography and Oeschger Center for Climate Change Research, University of Bern, 3012 Bern, Switzerland
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54 citations as recorded by crossref.
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- Increasing Flood Frequencies Under Warming in the West‐Central Himalayas S. Swarnkar & P. Mujumdar 10.1029/2022WR032772
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- Exploring the ability of the variable-resolution Community Earth System Model to simulate cryospheric–hydrological variables in High Mountain Asia R. Wijngaard et al. 10.5194/tc-17-3803-2023
- The first ensemble of kilometer-scale simulations of a hydrological year over the third pole E. Collier et al. 10.1007/s00382-024-07291-2
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- Improving climate model skill over High Mountain Asia by adapting snow cover parameterization to complex-topography areas M. Lalande et al. 10.5194/tc-17-5095-2023
- Understanding the Diversity of CMIP6 Models in the Projection of Precipitation Over Tibetan Plateau H. Qiu et al. 10.1029/2023GL106553
- Impacts of land surface darkening on frozen ground and ecosystems over the Tibetan Plateau S. Tang et al. 10.1007/s11430-023-1363-3
- Analysis of combined series of hydrological angular momentum developed based on climate models J. Nastula et al. 10.3389/feart.2024.1369106
Latest update: 21 Nov 2024
Short summary
Climate change over High Mountain Asia is investigated with CMIP6 climate models. A general cold bias is found in this area, often related to a snow cover overestimation in the models. Ensemble experiments generally encompass the past observed trends, suggesting that even biased models can reproduce the trends. Depending on the future scenario, a warming from 1.9 to 6.5 °C, associated with a snow cover decrease and precipitation increase, is expected at the end of the 21st century.
Climate change over High Mountain Asia is investigated with CMIP6 climate models. A general cold...
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