DOI: 10.1175/JCLI-D-11-00317.1
Scopus记录号: 2-s2.0-84865188032
论文题名: Simulated local and remote biophysical effects of afforestation over the Southeast United States in boreal summer
作者: Chen G.-S. ; Notaro M. ; Liu Z. ; Liu Y.
刊名: Journal of Climate
ISSN: 8948755
出版年: 2012
卷: 25, 期: 13 起始页码: 4511
结束页码: 4522
语种: 英语
Scopus关键词: Atmospheric carbon dioxide
; Carbon sequestration
; Community climate system model
; Fully-coupled
; Hydrologic models
; Initial values
; Lake States
; Land surface models
; Local cooling
; Local effects
; Local surfaces
; Model results
; Quasi-equilibrium
; Remote surfaces
; Southeast United States
; Time-scales
; Atmospheric chemistry
; Biophysics
; Carbon dioxide
; Climate models
; Experiments
; Water supply
; Reforestation
; afforestation
; biophysics
; carbon sequestration
; climate change
; climate modeling
; evapotranspiration
; hydrological modeling
; land surface
; latent heat flux
; numerical model
; precipitation (climatology)
; summer
; Corn Belt
; Great Lakes [North America]
; United States
; Zea mays
英文摘要: Afforestation has been proposed as a climate changemitigation strategy by sequestrating atmospheric carbon dioxide. With the goal of increasing carbon sequestration, a Congressional project has been planned to afforest about 18million acres by 2020 in the SoutheastUnited States (SEUS), theGreat Lake states, and the Corn Belt states. However, biophysical feedbacks of afforestation have the potential to counter the beneficial climatic consequences of carbon sequestration. To assess the potential biophysical effects of afforestation over the SEUS, the authors designed a set of initial value ensemble experiments and long-term quasi-equilibrium experiments in a fully coupled Community Climate System Model, version 3.5 (CCSM3.5). Model results show that afforestation over the SEUS not only has a local cooling effect in boreal summer [June-August (JJA)] at short and long time scales but also induces remote warming over adjacent regions of the SEUS at long time scales. Precipitation, in response to afforestation, increases over the SEUS (local effect) and decreases over adjacent regions (remote effect) in JJA. The local surface cooling and increase in precipitation over SEUS in JJA are hydrologically driven by the changes in evapotranspiration and latent heat flux. The remote surface warming and decrease in precipitation over adjacent regions are adiabatically induced by anomalous subsidence. Our results suggest that the planned afforestation efforts should be developed carefully by taking account of short-term (local) and long-term (remote) biophysical effects of afforestation. © 2012 American Meteorological Society.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/52323
Appears in Collections: 气候变化事实与影响
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作者单位: Center for Climatic Research, University of Wisconsin-Madison, Madison, WI, United States; Center for Forest Disturbance Science, USDA Forest Service, Athens, GA, United States
Recommended Citation:
Chen G.-S.,Notaro M.,Liu Z.,et al. Simulated local and remote biophysical effects of afforestation over the Southeast United States in boreal summer[J]. Journal of Climate,2012-01-01,25(13)