A bias-corrected projection for the changes in East Asian summer monsoon rainfall under global warming

被引:0
作者
Shijie Zhou
Gang Huang
Ping Huang
机构
[1] Chinese Academy of Sciences,State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics
[2] Qingdao National Laboratory for Marine Science and Technology,Laboratory for Regional Oceanography and Numerical Modeling
[3] University of Chinese Academy of Sciences,Center for Monsoon System Research, Institute of Atmospheric Physics
[4] Chinese Academy of Sciences,undefined
[5] Joint Center for Global Change Studies (JCGCS),undefined
来源
Climate Dynamics | 2020年 / 54卷
关键词
East Asian summer monsoon; Rainfall; Bias correction; CMIP5; Global warming;
D O I
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中图分类号
学科分类号
摘要
Projecting regional rainfall changes in a warmer climate attracts ongoing attention. However, large uncertainty still exists in multi-model projection. In this study, we introduce a bias-corrected method to correct the multi-model projection of changes in East Asian summer monsoon (EASM) rainfall based on the historical and RCP8.5 runs of 25 models from phase 5 of Coupled Model Intercomparison Project. Firstly, the total rainfall changes are separated into the thermodynamic component due to increased specific humidity and the dynamic component due to circulation changes. The thermodynamic component is corrected using the observed present-day rainfall and the increase rate of specific humidity based on the wet-get-wetter mechanism. On the other hand, the dynamic component with the circulation changes is corrected based on a “spatial emergent constraint” method, which is further validated by the perfect model approach. Together, these corrections give an integrated projection for EASM rainfall changes under global warming. Such an approach can improve the signal-to-noise ratio of projection effectively, from the original 0.73 of the multimodel mean to around 1.9. The corrected projection of EASM rainfall changes shows a pronounced increase in southern China, the northwest Pacific and a belt from northern China to northeastern China, and a weak increase in other EASM regions.
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页码:1 / 16
页数:15
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  • [1] Abe M(2011)Estimation of future surface temperature changes constrained using the future-present correlated modes in inter-model variability of CMIP3 multimodel simulations J Geophys Res 116 D18104-1167
  • [2] Shiogama H(2003)The version-2 global precipitation climatology project (GPCP) monthly precipitation analysis (1979–present) J Hydrometeorol 4 1147-232
  • [3] Nozawa T(2002)Constraints on future changes in climate and the hydrologic cycle Nature 419 224-2821
  • [4] Emori S(2012)Higher precision estimates of regional polar warming by ensemble regression of climate model projections Climate Dyn 39 2805-678
  • [5] Adler RF(2013)On the robustness of emergent constraints used in multimodel climate change projections of arctic warming J Climate 26 669-4596
  • [6] Huffman GJ(2016)Will a warmer world mean a wetter or drier Australian monsoon? J Climate 29 4577-8092
  • [7] Chang A(2015)The response of precipitation minus evapotranspiration to climate warming: why the “wet-get-wetter, dry-get-drier” scaling does not hold over land J Climate 28 8078-5227
  • [8] Ferraro R(2013)Link between land-ocean warming contrast and surface relative humidities in simulations with coupled climate models Geophys Res Lett 40 5223-77
  • [9] Xie P-P(2013)Projected change in East Asian summer monsoon precipitation under RCP scenario Meteorol Atmos Phys 121 55-9439
  • [10] Janowiak J(2015)Distinct effects of global mean warming and regional sea surface warming pattern on projected uncertainty in the South Asian summer monsoon Geophys Res Lett 42 9433-2701