Extended Data Fig. 10: The performance of CMIP6 models on climatological precipitation over HMA.
From: Precipitation regime changes in High Mountain Asia driven by cleaner air
The climatological mean of summer precipitation (mm·month−1) in and around HMA derived from multiple observations (GPCC, CRU, APHRO and GPM) and the historical simulations of 12 CMIP6 models from 1995–2014. For the GPM, the period of 2001–2020 is used. For each model, the results of the ensemble mean are shown. Numbers denote the pattern correlation coefficients of HMA precipitation between the corresponding model and GPCC data. The boundaries of HMA are identified as an isoline of 2500 m according to Global Multi-resolution Terrain Elevation Data 201052.
