闪烁计
显热
涡度相关法
协方差
鲍恩比率
环境科学
能量平衡
焊剂(冶金)
潜热
结束语(心理学)
校准
热流密度
大气科学
风速
遥感
近似误差
气象学
不确定性传播
行星边界层
观测误差
物理
湍流
数学
统计
机械
化学
传热
热力学
生态系统
生态学
经济
生物
有机化学
市场经济
大气湍流
作者
Pierre Solignac,Aurore Brut,Jean-Louis Selves,Jean-Pierre Béteille,Jean-Philippe Gastellu-Etchegorry,P. Keravec,Pierre Béziat,Éric Ceschia
标识
DOI:10.5194/amt-2-741-2009
摘要
Abstract. The use of scintillometers to determine sensible heat fluxes is now common in studies of land-atmosphere interactions. The main interest in these instruments is due to their ability to quantify energy distributions at the landscape scale, as they can calculate sensible heat flux values over long distances, in contrast to Eddy Covariance systems. However, scintillometer data do not provide a direct measure of sensible heat flux, but require additional data, such as the Bowen ratio (β), to provide flux values. The Bowen ratio can either be measured using Eddy Covariance systems or derived from the energy balance closure. In this work, specific requirements for estimating energy fluxes using a scintillometer were analyzed, as well as the accuracy of two flux calculation methods. We first focused on the classical method (used in standard softwares) and we analysed the impact of the Bowen ratio on flux value and uncertainty. For instance, an averaged Bowen ratio (β) of less than 1 proved to be a significant source of measurement uncertainty. An alternative method, called the "β-closure method", for which the Bowen ratio measurement is not necessary, was also tested. In this case, it was observed that even for low β values, flux uncertainties were reduced and scintillometer data were well correlated with the Eddy Covariance results. Besides, both methods should tend to the same results, but the second one slightly underestimates H while β decreases (<5%).
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