An initial intercomparison of micrometeorological and ecological inventory estimates of carbon exchange in a mid-latitude deciduous forest

被引:95
作者
Ehman, JL [1 ]
Schmid, HP
Grimmond, CSB
Randolph, JC
Hanson, PJ
Wayson, CA
Cropley, FD
机构
[1] Indiana Univ, Sch Publ & Environm Affairs, Bloomington, IN 47405 USA
[2] Indiana Univ, Dept Geog, Atmospher Sci Program, Bloomington, IN 47405 USA
[3] Oak Ridge Natl Lab, Div Environm Sci, Oak Ridge, TN 37831 USA
关键词
biometry; carbon fluxes; deciduous forest; ecophysiology; eddy covariance; micrometeorology; net ecosystem production; net primary production; soil respiration;
D O I
10.1046/j.1365-2486.2002.00492.x
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
The role of mid-latitude forests in the sequestration of carbon (C) is of interest to an increasing number of scientists and policy-makers alike. Net CO2 exchange can be estimated on an annual basis, using eddy-covariance techniques or from ecological inventories of C fluxes to and from a forest. Here we present an intercomparison of annual estimates of C exchange in a mixed hardwood forest in the Morgan-Monroe State Forest, Indiana, USA for two years, 1998 and 1999. Based on eddy-covariance measurements made at 1.8 times canopy height from a tower, C uptake by the forest was 237 and 287 g C m(-2) y(-1) for 1998 and 1999, respectively. For the same time period, biometric and ecophysiological measures and modelled estimates of all significant carbon fluxes within deciduous forests were made, including: change in living biomass, aboveground and belowground detritus production, foliage consumption, and forest floor and soil respiration. Using this ecological inventory method for these same two time periods, C uptake was estimated to be 271 and 377 g C m(-2) y(-1) , which are 14.3% and 31.4% larger, respectively, than the tower-based values. The relative change between this method's annual estimates is consistent with that of the eddy-covariance based values. Our results indicate that the difference in annual C exchange rates was due to reduced heterotrophic soil respiration in 1999.
引用
收藏
页码:575 / 589
页数:15
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