Mengying Zhao

Q., J.Cao, and M.Zhao. 2026. “Distinct Impacts of Carbon Dioxide Removal and Radiation Management on Regional Monsoons.” International Journal of Climatologye70413. Zuo, https://doi.org/10.1002/joc.70413. Conflicts of Interest The authors declare no conflicts of interest. Data Availability Statement The GPCC data are available at https://psl.noaa.gov/data/gridded/data.gpcc.html. References , , and . 2025.

Abstract A key uncertainty in understanding whether warming accelerates soil carbon (C) loss lies in how this response depends on other co-occurring environmental changes and the underlying mechanisms. Here we show that, in a 12-year grassland experiment, warming reduces soil C by 12.2% under drought but increases it by 6.7% under wet conditions. Such C losses during drought primarily result from the declines in mineral-associated organic C.

3.2.3.1 North Atlantic Subpolar Gyre We compute the annual maximum mixed layer depth over the North Atlantic (45°N–60°N, 50°W–20°W) as a measure of North Atlantic deep convection strength (Swingedouw et al., 2021) (Figure 4a). Under SSP2-4.5, from 2008 to 2027 to 2050–2069, the annual maximum mixed layer depth decreases by 77 m, indicating a weakening of deep convection.