Application of Dynamical and Statistical Downscaling to East Asian Summer Precipitation for Finely Resolved Datasets

<div>Taylor diagram for precipitation of the observation, GCM, DYN, STA, and HYB for subregions (South Korea: 125°E–130°E, 33°N–38°N, northern China: 113°E–131°E, 40°N–46°N, southern China: 113°E–123°E, 23°N–38°N, and Japan: 131°E–141°E, 30°N–42°N).</div>

Advances in Meteorology

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Figure 6

Figure 6: Application of Dynamical and Statistical Downscaling to East Asian Summer Precipitation for Finely Resolved Datasets 