DOI: 10.1175/JCLI-D-12-00479.1
Scopus记录号: 2-s2.0-84877642216
论文题名: Climate Feedbacks in CCSM3 under Changing CO2 Forcing. Part II: Variation of Climate Feedbacks and Sensitivity with Forcing
作者: Jonko A.K. ; Shell K.M. ; Sanderson B.M. ; Danabasoglu G.
刊名: Journal of Climate
ISSN: 8948755
出版年: 2013
卷: 26, 期: 9 起始页码: 2784
结束页码: 2795
语种: 英语
Scopus关键词: Absorption and emissions
; Climate feedbacks
; Climate sensitivity
; Fully-coupled model
; Long-wave radiation
; Model configuration
; Slab ocean models
; Temperature changes
; Carbon dioxide
; Computer simulation
; Feedback
; Greenhouse gases
; Sensitivity analysis
; Solar radiation
; Vapors
; Climate change
; air temperature
; albedo
; atmospheric lapse rate
; carbon dioxide
; climate feedback
; climate forcing
; climate modeling
; climate variation
; cloud
; general circulation model
; greenhouse gas
; sensitivity analysis
; water vapor
英文摘要: Are equilibrium climate sensitivity and the associated radiative feedbacks a constant property of the climate system, or do they change with forcing magnitude and base climate? Using the radiative kernel technique, feedbacks and climate sensitivity are evaluated in a fully coupled general circulation model (GCM) for three successive doublings of carbon dioxide starting from present-day concentrations. Climate sensitivity increases by 23% between the first and third CO2 doublings. Increases in the positive water vapor and cloud feedbacks are partially balanced by a decrease in the positive surface albedo feedback and an increase in the negative lapse rate feedback. Feedbacks can be decomposed into a radiative flux change and a climate variable response to temperature change. The changes in water vapor and Planck feedbacks are due largely to changes in the radiative response with climate state. Higher concentrations of greenhouse gases and higher temperatures lead to more absorption and emission of longwave radiation. Changes in cloud feedbacks are dominated by the climate response to temperature change, while the lapse rate and albedo feedbacks combine elements of both. Simulations with a slab ocean model (SOM) version of the GCMare used to verify whether an SOM-GCM accurately reproduces the behavior of the fully coupled model. Although feedbacks differ in magnitude between model configurations (with differences as large as those between CO2 doublings for some feedbacks), changes in feedbacks between CO2 doublings are consistent in sign andmagnitude in the SOM-GCM and the fully coupled model. © 2013 American Meteorological Society. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/51904
Appears in Collections: 气候变化事实与影响
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作者单位: Oregon State University, Corvallis, OR, United States; National Center for Atmospheric Research, Boulder, CO, United States
Recommended Citation:
Jonko A.K.,Shell K.M.,Sanderson B.M.,et al. Climate Feedbacks in CCSM3 under Changing CO2 Forcing. Part II: Variation of Climate Feedbacks and Sensitivity with Forcing[J]. Journal of Climate,2013-01-01,26(9)