Profiles of photosynthetically active radiation, nitrogen and photosynthetic capacity in the boreal forest: Implications for scaling from leaf to canopy

被引:72
作者
Dang, QL
Margolis, HA
Sy, M
Coyea, MR
Collatz, GJ
Walthall, CL
机构
[1] Lakehead Univ, Fac Forestry, Thunder Bay, ON P7B 5E1, Canada
[2] NASA, Goddard Space Flight Ctr, Biospher Sci Branch, Greenbelt, MD 20771 USA
[3] Univ Laval, Ctr Rech Biol Forestiere, Ste Foy, PQ G1K 7P4, Canada
[4] Carleton Univ, Dept Biol, Inst Biol, Ottawa, ON K1S 5B6, Canada
[5] USDA ARS, Remote Sensing Res Lab, BARC W, Beltsville, MD 20705 USA
关键词
D O I
10.1029/97JD00194
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Profiles of photosynthetically active radiation (PAR), leaf nitrogen per unit leaf area (N-area), and photosynthetic capacity (A(max)) were measured in an aspen, two jack pine, and two black spruce stands in the BOREAS northern study area. N-area decreased with decreasing %PAR in each stand, in all conifer stands combined (r = 0.52) and in all stands combined (r = 0.46). Understory alder had higher N-area for similar %PAR than did aspen early in the growing season. A(max) decreased with decreasing N-area except for the negative correlation between N-area and A(max) during shoot flush for jack pine. For the middle and late growing season data, N-area and A(max) had r values of 0.51 for all stands combined and 0.60 for all conifer stands combined. For similar N-area the aspen stand had higher A(max) than did the conifer stands. Photosynthetic capacity expressed as a percentage of A(max) at the top of the canopy (%A(max0)) decreased with %PAR similarly in all stands, but %A(max0) decreased at a much slower rate than did %PAR. To demonstrate the implications of the vertical distribution of A(max), three different assumptions were used to scale leaf A(max) to the canopy (A(can-max)): (1) constant A(max) with canopy depth, (2) A(max) scaled proportionally to %PAR, and (3) a linear relationship between A(max) and cumulative leaf area index derived from our data. The first and third methods resulted in similar A(can-max); the second was much lower. All methods resulted in linear correlations between normalized difference vegetation indices measured from a helicopter and A(can-max) (r = 0.97, 0.93, and 0.97, respectively), but the slope was strongly influenced by the scaling method.
引用
收藏
页码:28845 / 28859
页数:15
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