Carbon and water cycling in a Bornean tropical rainforest under current and future climate scenarios

被引:29
|
作者
Kumagai, T
Katul, GG
Porporato, A
Saitoh, TM
Ohashi, M
Ichie, T
Suzuki, M
机构
[1] Kyushu Univ, Univ Forest Miyazaki, Miyazaki 8830402, Japan
[2] Duke Univ, Nicholas Sch Environm & Earth Sci, Durham, NC 27708 USA
[3] Duke Univ, Dept Civil & Environm Engn, Durham, NC 27708 USA
[4] Kyushu Univ Forest, Res Inst, Fukuoka 8112415, Japan
[5] Univ Joensuu, Fac Forestry, FIN-80101 Joensuu, Finland
[6] Nanyang Technol Univ, NIE, Ctr Trop Forest Sci Arnold Arboretum, Asia Program, Singapore 637616, Singapore
[7] Univ Tokyo, Grad Sch Agr & Life Sci, Tokyo 1138657, Japan
基金
日本科学技术振兴机构; 美国国家科学基金会;
关键词
elevated CO2; stochastic processes; water balance; tropical rainforest; photosynthesis; transpiration;
D O I
10.1016/j.advwatres.2004.10.002
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
We examined how the projected increase in atmospheric CO2 and concomitant shifts in air temperature and precipitation affect water and carbon fluxes in an Asian tropical rainforest, using a combination of field measurements, simplified hydrological and carbon models, and Global Climate Model (GCM) projections. The model links the canopy photosynthetic flux with transpiration via a bulk canopy conductance and semi-empirical models of intercellular CO2 concentration, with the transpiration rate determined from a hydrologic balance model. The primary forcing to the hydrologic model are current and projected rainfall statistics. A main novelty in this analysis is that the effect of increased air temperature on vapor pressure deficit (D) and the effects of shifts in precipitation statistics on net radiation are explicitly considered. The model is validated against field measurements conducted in a tropical rainforest in Sarawak, Malaysia under current climate conditions. On the basis of this model and projected shifts in climatic statistics by GCM, we compute the probability distribution of soil moisture and other hydrologic fluxes. Regardless of projected and computed shifts in soil moisture, radiation and mean air temperature, transpiration was not appreciably altered. Despite increases in atmospheric CO2 concentration (C-a) and unchanged transpiration, canopy photosynthesis does not significantly increase if C-i/C-n is assumed constant independent of D (where C-i is the bulk canopy intercellular CO2 concentration). However, photosynthesis increased by a factor of 1.5 if C-i/C-a decreased linearly with D as derived from Leuning stomatal conductance formulation [R. Leuning. Plant Cell Environ 1995;18:339-55]. How elevated atmospheric CO2 alters the relationship between C-i/C-a and D needs to be further investigated under elevated atmospheric CO2 given its consequence on photosynthesis (and concomitant carbon sink) projections. (C) 2004 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1135 / 1150
页数:16
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