The Köppen‐Trewartha Climate‐Type Changes Over the CORDEX‐East Asia Phase 2 Domain Under 2 and 3 °C Global Warming.

For the comprehensive estimation of regional climate change over East Asia (EA) at the 2 and 3 °C global warming levels (GWLs), the Köppen‐Trewartha climate‐type change is assessed with ensemble regional climate change projections in line with Coordinated Regional Climate Downscaling Experiment (CORDEX)‐EA phase 2. Under the 2 °C (3 °C) GWL, 17.6% (25.2%) of the EA region is expected to undergo major climate‐type changes. Tropical and subtropical climate types will expand northward, accompanied by increasing hydroclimatic intensity. Limiting GWL to 2 °C shows benefits by preventing subtropical‐type expansion around far EA. Desertification over inland regions of EA exhibits scenario dependency. Boreal and tundra climate types over high‐latitude regions will tend to decrease rapidly, especially over the Tibetan Plateau. The results are expected to be a baseline assessment of climate change over EA under the 2 and 3 °C GWLs above the preindustrial level. Plain Language Summary: This paper investigates the Köppen‐Trewartha climate‐type changes over East Asia (EA) at the 2 and 3 °C global warming levels (GWLs) with the ensemble regional climate simulations. Under the 2 °C (3 °C) GWL, 17.6% (25.2%) of the EA region is expected to undergo major climate‐type changes. The result shows increased tropical, subtropical, and desert climate types accompanied by intensification of hydroclimatic stress. In addition, boreal and tundra climate types over high‐latitude regions will tend to decrease rapidly, especially over the Tibetan Plateau under the 2 and 3 °C GWLs. Key Points: Baseline assessment of climate change over East Asia under the 2 and 3 °C global warming is here presentedOf the East Asia region, 17.6% (25.2%) is expected to experience major climate‐type changes under the 2 and 3 °C global warmingThe changes are accompanied by intensified hydroclimatic stress and have statistically significant trends until the end of the 21st century [ABSTRACT FROM AUTHOR]