How well do we know the flux of CO2 from land-use change?

被引:143
作者
Houghton, R. A. [1 ]
机构
[1] Woods Hole Res Ctr, Falmouth, MA 02540 USA
来源
TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY | 2010年 / 62卷 / 05期
基金
美国国家科学基金会;
关键词
SOIL CARBON; FOREST BIOMASS; COVER CHANGE; DEFORESTATION; CLIMATE; SEQUESTRATION; CULTIVATION; MANAGEMENT; INCREASES; BIOSPHERE;
D O I
10.1111/j.1600-0889.2010.00473.x
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Five new estimates of global net annual emissions of carbon from land use and land-use change collectively describe a gradually increasing trend in emissions, from similar to 0.6 PgC yr-1 in 1850 to similar to 1.3 PgC yr-1 in the period 1950-2005, with an annual range that varies between +/- 0.2 and +/- 0.4 PgC yr-1 of the mean. All estimates agree in the upward trend from 1850 to similar to 1950 but not thereafter. In recent decades, when rates of land-use change and biomass density should be better known than in the past, the estimates are more variable. Most analyses have used three quasi-independent estimates of land-use change that are based on national and international agricultural and forestry data of limited accuracy in many countries. Further, the estimates of biomass used in the analyses have a common but limited literature base, which fails to address the spatial variability of biomass density within ecosystems. In contrast to the sources of information that have been used to date, a combination of existing ground and remote sensing data are available to determine with far higher accuracy rates of land-use change, aboveground biomass density, and, hence, the net flux of carbon from land use and land-use change.
引用
收藏
页码:337 / 351
页数:15
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