Inter‐Comparison of Precipitation Simulation and Future Projections Over China From an Ensemble of Multi‐GCM Driven RCM Simulations

Author:

Tong Yao12ORCID,Gao Xuejie134ORCID,Xu Ying5ORCID,Cui Xiulai2,Giorgi Filippo6ORCID

Affiliation:

1. Climate Change Research Center Institute of Atmospheric Physics Chinese Academy of Sciences Beijing China

2. Yingkou Meteorological Bureau Yingkou China

3. Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters Nanjing University of Information Science & Technology Nanjing China

4. University of Chinese Academy of Sciences Beijing China

5. National Climate Center China Meteorological Administration Beijing China

6. The Abdus Salam International Centre for Theoretical Physics Trieste Italy

Abstract

AbstractAn analysis is presented of the precipitation bias and change signal in an ensemble of regional climate model (RCM) (RegCM4) projections driven by multiple general circulation models (GCMs) over China. RegCM4 is driven by five different GCMs for the 120‐year period 1979–2099 at 25 km grid spacing, under the representative concentration pathway RCP8.5. We find that the GCMs and RegCM4 reproduce the general spatial pattern of precipitation over China in all four seasons, with RegCM4 providing greater spatial detail, especially over areas with complex terrain. The spatial patterns of precipitation bias show common features between the GCMs and RegCM4, characterized by an underestimation in the wetter regions, and an overestimation in the drier ones. Systematic increases of precipitation are projected in northern China, most pronounced in the Northwest basins, by both the GCMs and RegCM4 in all seasons except summer, when more mixed results are found. In addition, weak correlations of the projected change patterns are found in summer between the GCMs and nested RegCM4, indicating the greater role played by the representation of local convection processes during this monsoon season. The projections across the RegCM4 experiments show higher consistency and lower spread compared to the GCM ensemble, again indicating that the nested model physics significantly modulates the change signal deriving from the GCM boundary forcing.

Funder

National Natural Science Foundation of China

Natural Science Foundation of Liaoning Province

Publisher

American Geophysical Union (AGU)

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