DOI: 10.1175/JCLI-D-17-0741.1
Scopus记录号: 2-s2.0-85052821624
论文题名: Potential underestimation of future Mei-Yu Rainfall with coarse-resolution climate models
作者: Chen X. ; Wu P. ; Roberts M.J. ; Zhou T.
刊名: Journal of Climate
ISSN: 8948755
出版年: 2018
卷: 31, 期: 17 起始页码: 6711
结束页码: 6727
语种: 英语
英文关键词: Climate models
; Climate prediction
; Hydrologic cycle
; Model comparison
; Monsoons
; Water budget
Scopus关键词: Budget control
; Global warming
; Moisture
; Rain
; Water analysis
; Climate prediction
; Hydrologic cycles
; Model comparison
; Monsoons
; Water budget
; Climate models
; Citrus maxima
英文摘要: The amount of rainfall during June and July along the mei-yu front contributes about 45% to the total summer precipitation over the Yangtze River valley. How it will change under global warming is of great concern to the people of China because of its particular socioeconomic importance, but climate model projections from phase 5 of the Coupled Model Intercomparison Project (CMIP5) show large uncertainties. This paper examines model resolution sensitivity and reports large differences in projected future summer rainfall along the mei-yu front between a low-resolution (Gaussian N96 grid, ~1.5° latitude-longitude) and a high-resolution (N216, ~0.7°) version of the Hadley Centre's latest climate model, the HadGEM3 Global Coupled Configuration 2.0 (HadGEM3-GC2). The high-resolution model projects large increases of summer rainfall under two representative concentration pathway scenarios (RCP8.5 and RCP4.5) whereas the low-resolution model shows a decrease. A larger increase of projected mei-yu rainfall in higher-resolution models is also observed across the CMIP5 ensemble. These differences can be explained in terms of enhanced moist static energy advection and moisture convergence by stationary eddies in the high-resolution model. A large-scale manifestation of the anomalous stationary eddies is the contrasting response to the same warming scenario by the western North Pacific subtropical high, which is almost unchanged in N216 but retreats evidently eastward in N96, reducing the southwesterly flow and consequently moisture supply to the mei-yu front. Further increases in model resolution to resolve parameterized processes and detailed orographic features will hopefully reduce the spread in future climate projections. © 2018 American Meteorological Society. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/110701
Appears in Collections: 影响、适应和脆弱性 气候变化事实与影响
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作者单位: LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China; Met Office Hadley Centre, Exeter, United Kingdom; University of Chinese Academy of Sciences, Beijing, China
Recommended Citation:
Chen X.,Wu P.,Roberts M.J.,et al. Potential underestimation of future Mei-Yu Rainfall with coarse-resolution climate models[J]. Journal of Climate,2018-01-01,31(17)