The effective radiative forcing (ERF) and associated surface air temperature change over eastern China are estimated using multi-model results from CMIP5 (Coupled Model Intercomparison Project Phase 5). The model results show that, relative to 1850, the multi-model and annual mean aerosol ERF for the year 2005 is −4.14 W m−2 at the top of the atmosphere over eastern China (20°–45°N, 105°–122.5°E). As a result of this ERF, the multi-model and annual mean surface air temperature change in eastern China during 1850–2005 is −1.05 °C, leading to a climate sensitivity of 0.24 °C/(W m−2) in this region.
CITATION STYLE
LIU, R. J., & LIAO, H. (2017). Assessment of aerosol effective radiative forcing and surface air temperature response over eastern China in CMIP5 models. Atmospheric and Oceanic Science Letters, 10(3), 228–234. https://doi.org/10.1080/16742834.2017.1301188
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