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ON THE SPATIAL VARIABILITY OF BIOPHYSICAL FACTORS AND ITS INFLUENCE ON MEASURED NET ECOSYSTEM EXCHANGE OVER FOREST

机译:生物因子的空间变异性及其对森林生态系统净交换量的影响

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All natural forest ecosystems exhibit spatial variability at some range of scales. Measured fluxes of CO_2 are thus only expected to be representative of a forest ecosystem to the extent that the biophysical forcings in the flux footprint reflect average forest conditions. Here, we examine the influence of spatial variability in biomass (as expressed by the normalized difference vegetation index, NDVI), and the amount of absorbed photosynthetically active radiation (APAR) on the estimate of net ecosystem exchange of CO_2 from eddy-covariance measurements at a height of 46 m above a forest canopy of h = 26 m at the Morgan-Monroe State Forest (MMSF, Indiana, USA) AmeriFlux site (Schmid et al., 2000). An IKONOS satellite scene is used to determine the distribution of NDVI in the vicinity of the MMSF site. Slope angle information is obtained from a digital terrain model. Growing season average PAR is calculated for each grid-point. First incoming solar radiation is modeled across the topographical domain using the method of Moore et al. (1993). Direct and diffuse beam solar radiation are calculated based on atmospheric optical transmission, estimated from observations on the MMSF tower (including a cloudiness index). Slope and aspect effect on exposure to direct beam radiation and the sky view factor effect on receipt of diffuse beam radiation is derived using the terrain model. APAR is assumed to be related to NDVI and PAR by APAR≈α_p PAR[1-exp(-LAI)] , (1) where α_p ≈ 0.94, and LAI ≈117.35 NDVI - 9.01 (Baret and Guyot 1991; Wulder et al. 1998).
机译:所有天然森林生态系统在一定范围内都表现出空间变异性。因此,仅在通量足迹中的生物物理强迫反映了平均森林状况的范围内,才期望测得的CO_2通量代表森林生态系统。在这里,我们研究了生物量的空间变异性(用归一化植被指数NDVI表示)以及吸收的光合有效辐射量(APAR)对涡旋协方差测量中CO_2净生态系统交换量的估计。摩根-梦露州立森林(MMSF,美国印第安纳州,美国)AmeriFlux站点的高度为26 m时,林冠上方的高度为46 m(Schmid et al。,2000)。 IKONOS卫星场景用于确定MMSF站点附近NDVI的分布。倾斜角信息是从数字地形模型中获得的。计算每个网格点的生长季节平均PAR。首先使用Moore等人的方法对整个地形域内的太阳辐射进行建模。 (1993)。直射光束和漫射光束的太阳辐射是根据大气的光学透射率计算得出的,该透射率是根据MMSF塔的观测值(包括浊度指数)估算得出的。使用地形模型可以得出斜率和高宽比对直接光束辐射的影响以及天空因素对漫射光束辐射的接收的影响。通过APAR≈α_pPAR [1-exp(-LAI)],(1)假设APAR与NDVI和PAR相关。(1)其中α_p≈0.94,LAI≈117.35NDVI-9.01(Baret and Guyot 1991; Wulder等。 1998)。

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