Simulating the Biogeochemical and Biogeophysical Impacts of Transient Land Cover Change and Wood Harvest in the Community Climate System Model (CCSM4) from 1850 to 2100

被引:193
作者
Lawrence, Peter J. [1 ]
Feddema, Johannes J. [2 ]
Bonan, Gordon B. [1 ]
Meehl, Gerald A. [1 ]
O'Neill, Brian C. [1 ]
Oleson, Keith W. [1 ]
Levis, Samuel [1 ]
Lawrence, David M. [1 ]
Kluzek, Erik [1 ]
Lindsay, Keith [1 ]
Thornton, Peter E. [3 ]
机构
[1] Natl Ctr Atmospher Res, Boulder, CO 80307 USA
[2] Univ Kansas, Dept Geog, Lawrence, KS 66045 USA
[3] Oak Ridge Natl Lab, Div Environm Sci, Oak Ridge, TN 37831 USA
基金
美国国家科学基金会;
关键词
USE TRANSITIONS; CARBON; SCENARIOS;
D O I
10.1175/JCLI-D-11-00256.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
To assess the climate impacts of historical and projected land cover change in the Community Climate System Model, version 4 (CCSM4), new time series of transient Community Land Model, version 4 (CLM4) plant functional type (PFT) and wood harvest parameters have been developed. The new parameters capture the dynamics of the Coupled Model Intercomparison Project phase 5 (CMIP5) land cover change and wood harvest trajectories for the historical period from 1850 to 2005 and for the four representative concentration pathway (RCP) scenarios from 2006 to 2100. Analysis of the biogeochemical impacts of land cover change in CCSM4 reveals that the model produced a historical cumulative land use flux of 127.7 PgC from 1850 to 2005, which is in general agreement with other global estimates of 156 PgC for the same period. The biogeophysical impacts of the transient land cover change parameters were cooling of the near-surface atmosphere over land by -0.1 degrees C, through increased surface albedo and reduced shortwave radiation absorption. When combined with other transient climate forcings, the higher albedo from land cover change was counteracted by decreasing snow albedo from black carbon deposition and high-latitude warming. The future CCSM4 RCP simulations showed that the CLM4 transient PFT parameters can be used to represent a wide range of land cover change scenarios. In the reforestation scenario of RCP 4.5, CCSM4 simulated a drawdown of 67.3 PgC from the atmosphere into the terrestrial ecosystem and product pools. By contrast the RCP 8.5 scenario with deforestation and high wood harvest resulted in the release of 30.3 PgC currently stored in the ecosystem.
引用
收藏
页码:3071 / 3095
页数:25
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