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This is the data and code for the paper titled “Changing Northern Hemisphere Weather Linked to Warming Amplification in High Mountain Asia”, which has published in Communications Earth & Environment, https://doi.org/10.1038/s43247-025-02883-0.
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This is the data and code for the paper titled “Reversed Future Drying‐Wetting Precipitation Patterns Over the Northwestern and Southeastern East Asia Driven by Reduced Aerosol Emissions”, which has published in Geophysical Research Letters, https://doi.org/10.1029/2024GL114527.
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This is the data and code for the paper titled “Impact of the Tibetan Plateau on Global High-frequency Temperature Variability”, which was published in Journal of Climate, https://doi.org/10.1175/JCLI-D-23-0271.1.
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Data and codes for the paper titled “Decadal Heatwave Fluctuations in China Caused by the Indian and Atlantic Oceans”, published in Environmental Research Letters, https://doi.org/10.1088/1748-9326/ad5b05.
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This is codes for potential vorticity inversion performed by the authors for their study titled, “Potential vorticity dynamics explain how extratropical oceans and the Arctic modulate wintertime land-temperature variations”, which was published in Earth’s Future, https://doi.org/10.1029/2022EF003275.
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This dataset is the CESM outputs and codes and the observational data for the study titled, “Enhanced Asian warming increases Arctic amplification”, which was published to Environmental Research Letters, https://doi.org/10.1088/1748-9326/acbdb1. There were four CESM experiments, namely HIST, AL500-sh0.5, amip-HIST, and amip-AL500-nosh. The observational data are the aridity index.
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This dataset is the outputs and codes of CESM experiments performed by the authors for their study titled, “Oceanic repeaters boost the global climatic impact of the Tibetan Plateau”, which was published in Science Bulletin, https://doi.org/10.1016/j.scib.2023.07.019. There were six CESM experiments, namely amip-hist, amip-TIP-nosh, amip-TIP-alb0.5, amip-TIP-sh0.5, cmip-hist, and cmip-TIP-sh0.5. The CESM model (version 2.1.3) was provided by NCAR/UCAR. In all the experiments, hist (historical) experiments were control runs, whereas the TIP (Tibetan–Iranian Plateau coupling system) -labeled experiments were sensitivity runs.