The seasonal water and energy exchange above and within a boreal aspen forest

被引:94
|
作者
Blanken, PD
Black, TA
Neumann, HH
den Hartog, G
Yang, PC
Nesic, Z
Lee, X
机构
[1] Univ Colorado, Dept Geog, Boulder, CO 80309 USA
[2] Univ Colorado, Environm Studies Program, Boulder, CO 80309 USA
[3] Univ British Columbia, Vancouver, BC V5Z 1M9, Canada
[4] Meteorol Serv Canada, Downsview, ON, Canada
[5] Yale Univ, New Haven, CT USA
基金
加拿大自然科学与工程研究理事会;
关键词
biometeorology; boreal forest; deciduous forest; transpiration; radiation; surface energy balance;
D O I
10.1016/S0022-1694(01)00343-2
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
The seasonal water and energy exchange of a boreal aspen forest underlain by a hazelnut understory is described. Measurements of above-aspen latent and sensible heat, short-wave and net radiation, and photosynthetically active radiation are compared to those measured above the hazelnut understory. Understory radiation measurements were cn made using a tram system. Energy storage at each measurement height was determined, and measurements of the soil moisture, temperature, and heat flux were made using an array of probes. The mean annual air temperature and total precipitation during 1994 were 1.2 degreesC and 488.4 mm, respectively, above the 1951-1980 average -0.2 degreesC and total 462.6 mm. There was a pronounced seasonal development of leaves. with the maximum Leaf area index of the hazelnut (3.3 m(2) m(-2)) exceeding that of the aspen (2.3 m(2) m(-2)). Beneath-aspen radiation decreased exponentially as the aspen leaf area increased, and the calculated effective extinction coefficients decreased as the plant area index increased. At full aspen leaf 27, 23, and 20% of the above-aspen short-wave, net, and photosynthetically active radiation, respectively, reached the hazelnut. The diurnal energy balance at both heights showed pronounced seasonal trends. Sensible heat from the forest door dominated during the leaf-free period, whereas latent heat from the overstory dominated during the leafed period. The fraction of the annual precipitation evaporated was 82-91%, with 67-68%, 26-28%, and 4-7% originating from the aspen, hazelnut, and soil, respectively. Over the leafed period, soil water was depleted from the root zone (0-60 cm depth) and accumulated between the 61-123 cm depth, overall resulting in a deficit of 34.7 mm between 0-123 cm depths. This soil water balance compared well with the daily integrated difference between precipitation and eddy-covariance determined measurements of evaporation. (C) 2001 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:118 / 136
页数:19
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