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Downscaling and bias adjustment have been conducted by the BASD software. For a comprehensive description of version 1.0 of the methods see Lange (2019, doi:10.5194/gmd-12-3055-2019). The models are: canesm5_r1i1p1f1 cnrm-cm6-1_r1i1p1f2 gfdl-esm4_r1i1p1f1 ipsl-cm6a-lr_r1i1p1f1 miroc6_r1i1p1f1 mri-esm2-0_r1i1p1f1 the variables are tas- daily mean of near surface air temperature (K) pr - daily precipitation (kg m-2 s-1 ) the final horizontal resolution is 0.25° and the area covered longitude 44.125 -90.875 & latitude 33.125-56.375
The reference article: Fallah, B., Russo, E., Menz, C. et al. Anthropogenic influence on extreme temperature and precipitation in Central Asia. Sci Rep 13, 6854 (2023). https://doi.org/10.1038/s41598-023-33921-6
climate change, Central Asia, bias adjustment, statistical downscaling
climate change, Central Asia, bias adjustment, statistical downscaling
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