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The measurement and modelling of the carbon dioxide exchange at a highArctic site in Svalbard

机译:斯瓦尔巴特群岛高海拔地区二氧化碳交换的测量和建模

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摘要

Well-documented models of soil respiration and C-3 photosynthesis are combined to investigate the overall carbon dioxide balance of a high arctic polar semidesert site near Ny-Alesund, Svalbard. Measurements of carbon dioxide fluxes from an eddy correlation system and climate variables are used to calibrate this combined model for the snowmelt-summer period in 1995. Particular emphasis was put on modelling effectively the separate soil respiration and net photosynthesis of the moss/lichen, vascular plant and bare soil areas within the heterogeneous site, and ascertaining whether moss/lichen communities could be effectively modelled using a C-3 photosynthetic model. The calibrated model of 1995 data was subsequently tested in predictive mode against eddy correlation nux measurements recorded in 1996. The model is shown to simulate effectively both years and highlights the important role that the timing of snowmelt, summer precipitation and soil temperature has upon the overall carbon dioxide balance of this site. A previous conjecture by the author from the limited flux measurements that the investigated period in 1995 was an overall sink for carbon dioxide and that the same period in 1996 was an overall source of carbon dioxide is borne out by the model runs with 3.9 +/- 3.7 gC m(-2) being assimilated into the vegetation during the 1995 period and 5.0 +/- 3.3 gC m(-2) being returned to the atmosphere during the same period in 1996.
机译:有据可查的土壤呼吸和C-3光合作用的模型相结合,以研究斯瓦尔巴特群岛Ny-Alesund附近的一个高北极极地半沙漠地的总体二氧化碳平衡。利用涡流相关系统的二氧化碳通量测量值和气候变量来校准1995年融雪夏季的组合模型。特别强调有效地模拟苔藓/地衣,维管束的土壤呼吸和净光合作用异质站点内的植物和裸露的土壤区域,并确定是否可以使用C-3光合作用模型有效地模拟苔藓/地衣群落。随后,对1995年数据的校准模型进行了预测,并与1996年记录的涡旋相关量进行了对比。该模型被证明可以有效地模拟这两年,并突显了融雪时间,夏季降水和土壤温度在总体上的重要作用。该站点的二氧化碳平衡。作者先前从有限通量测量中得出的一个推测是,该模型运行于3.9 +/-上,证明了1995年的调查时期是二氧化碳的总体汇,而1996年同期是二氧化碳的总体来源。在1995年期间将3.7 gC m(-2)吸收到植被中,并在1996年同期将5.0 +/- 3.3 gC m(-2)返回大气。

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