Improvements of a dynamic global vegetation model and simulations of carbon and water at an upland-oak forest

被引:9
作者
Mao Jiafu [1 ]
Wang Bin
Dai Yongjiu
Woodward, F. I.
Hanson, P. J.
Lomas, M. R.
机构
[1] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geop, Beijing 100029, Peoples R China
[2] Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China
[3] Beijing Normal Univ, Sch Geog, Beijing 100875, Peoples R China
[4] Univ Sheffield, Ctr Terr Carbon Dynam, Sheffield S10 2TN, S Yorkshire, England
[5] Univ Sheffield, Dept Anim & Plant Sci, Sheffield S10 2TN, S Yorkshire, England
[6] Oak Ridge Natl Lab, Div Environm Sci, Oak Ridge, TN 37831 USA
基金
中国国家自然科学基金;
关键词
dynamic global vegetation models; terrestrial carbon and water fluxes; Eddy covariance; calibration;
D O I
10.1007/s00376-007-0311-7
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The interest in the development and improvement of dynamic global vegetation models (DGVMs), which have the potential to simulate fluxes of carbon, water and nitrogen, along with changes in the vegetation dynamics, within an integrated system, has been increasing. In this paper, some numerical schemes and a higher resolution soil texture dataset were employed to improve the Sheffield Dynamic Global Vegetation Model (SDGVM). Using eddy covariance-based measurements, we then tested the standard version of the SDGVM and the modified version of the SDGVM. Detailed observations of daily carbon and water fluxes made at the upland oak forest on the Walker Branch Watershed in Tennessee, USA offered a unique opportunity for these comparisons. The results revealed that the modified version of the SDGVM did a reasonable job of simulating the carbon and water flux and the variation of soil water content (SWC). However, at the end of the growing season, it failed to simulate the effect of the limitations on the soil respiration dynamics and as a result underestimated this respiration. It was also noted that the modified version overestimated the increase in the SWC following summer rainfall, which was attributed to an inadequate representation of the ground water and thermal cycle.
引用
收藏
页码:311 / 322
页数:12
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