Environmental control of canopy stomatal conductance in a tropical deciduous forest in northern Thailand

被引:55
|
作者
Igarashi, Yasunori [1 ]
Kumagai, Tomo'omi [1 ]
Yoshifuji, Natsuko [2 ]
Sato, Takanori [3 ]
Tanaka, Nobuaki [4 ]
Tanaka, Katsunori [5 ]
Suzuki, Masakazu [3 ]
Tantasirin, Chatchai [6 ]
机构
[1] Nagoya Univ, Hydrospher Atmospher Res Ctr, Nagoya, Aichi 4648601, Japan
[2] Kyoto Univ, Grad Sch Agr, Kyoto 6068502, Japan
[3] Univ Tokyo, Grad Sch Agr & Life Sci, Bunkyo Ku, Tokyo 1130023, Japan
[4] Univ Tokyo, Grad Sch Agr & Life Sci, Univ Tokyo Forests, Ecohydrol Res Inst, Seto, Aichi 4890031, Japan
[5] Japan Agcy Marine Earth Sci & Technol, Dept Environm Geochem Cycle Res, Kanazawa Ku, Yokohama, Kanagawa 2360001, Japan
[6] Kasetsart Univ, Fac Forestry, Bangkok 10900, Thailand
关键词
Tropical monsoon forest; Stomatal control; Transpiration; Water vapor flux; Eddy covariance; Soil moisture; NET ECOSYSTEM EXCHANGE; LEAF-AREA INDEX; FLUX-SCALED TRANSPIRATION; VAPOR-PRESSURE DEFICIT; INTERANNUAL VARIABILITY; PHOTOSYNTHETIC CAPACITY; CLIMATIC IMPACT; SEASONAL FOREST; ENERGY FLUXES; WATER-VAPOR;
D O I
10.1016/j.agrformet.2014.11.013
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Tropical seasonal forests in Southeast Asia are among the most important biomes in terms of global and local hydrologic and carbon fluxes, and their vulnerability to climate change. We conducted eddy flux measurements in a teak (Tectona grandis Linn. f.) plantation in northern Thailand over a 6-year period; this forest undergoes a drastic seasonal change in foliage with somewhat constant incident radiative energy. We used a combination of actual evapotranspiration (ET) flux data and an inversed version of a simple two-layer ET model for estimating the mean canopy stomatal conductance (g(s)). The main novelty of this analysis is that canopy conductance can be extracted from total surface conductance (including the canopy and forest floor effects), and thus environmental and biological controls of g(s) are explicitly compared among seasons and years. The relationship between seasonal variations in the leaf area index (LAI) and g(s) revealed an apparent effect of leaf age on leaf gas exchange capacity: within a year, g(s) peaked earlier than full-leaf expansion and abruptly declined after the peak of LAI. We used this result to classify three leaf age stages: leaf-out, mid-growing, and leaf-senescence seasons. Then, two ecophysiological parameters, the reference value of g(s) (g(sref)), and the sensitivity of g(s) to atmospheric demand (m), as well as their proportion (m/g(sref)), were derived from the logarithmic response curve of g(s) to vapor pressure deficit (VPD) for each season. We showed seasonal variation in g(sref) as follows: leaf-out season approximate to mid-growing season > leaf-senescence season. m demonstrated little seasonality and little interannual variation was observed in either parameter. This resulted in a value of almost 0.6 for m/g(sref) during the leaf-senescence season and of less than 0.6 in the leaf-out and mid-growing seasons, which suggests that the teak trees had strict stomatal regulation to prevent excessive xylem cavitation during the leaf-senescence season (i.e., under drought conditions) and less strict stomatal regulation during the leaf-out and mid-growing seasons (i.e., under moist conditions) when little risk of water stress-induced hydraulic failure would occur. In addition, we obtained a simple linear relationship between soil moisture and g(sref), which can be a powerful tool for further research of land atmosphere interactions using global climate and vegetation dynamics models. (C) 2014 Elsevier B.V. All rights reserved.
引用
收藏
页码:1 / 10
页数:10
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