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ISSN: 1674-9278
CN: 11-5918/P

Evaluation of CMIP6 for historical temperature and precipitation over the Tibetan Plateau and its comparison with CMIP5

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Impacts of climate-induced permafrost degradation on vegetation: A review

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Will China achieve its 2060 carbon neutral commitment from the provincial perspective?

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New perspectives on ‘warming–wetting’ trend in Xinjiang, China

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Projected drought conditions in Northwest China with CMIP6 models under combined SSPs and RCPs for 2015–2099

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The policy-driven peak and reduction of China's carbon emissions

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Permafrost change in Northeast China in the 1950s–2010s

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Contribution of nearly-zero energy buildings standards enforcement to achieve carbon neutral in urban area by 2060

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Integrated impacts of climate change on glacier tourism

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Enhancing coastal areas governance for sustainable tourism in the context of urbanization and climate change in eastern Thailand

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Impacts of degrading permafrost on streamflow in the source area of Yellow River on the Qinghai-Tibet Plateau, China

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Corporate innovation and environmental investment: The moderating role of institutional environment

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Influences of forest fires on the permafrost environment: A review

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A new look at roles of the cryosphere in sustainable development

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Economic development, energy demand, and carbon emission prospects of China's provinces during the 14th Five-Year Plan period: Application of CMRCGE model

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Degrading permafrost and its impacts

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Change in drought conditions and its impacts on vegetation growth over the Tibetan Plateau

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Understanding systemic risk induced by climate change

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An integrated approach to evaluating the coupling coordination degree between low-carbon development and air quality in Chinese cities

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Recognition and analysis of potential risks in China's carbon emission trading markets

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Impacts of household living consumption on energy use and carbon emissions in China based on the input–output model

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Regional differences in global glacier retreat from 1980 to 2015

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Climate change projection over the Tibetan Plateau based on a set of RCM simulations

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