Can Data Mining Help Eddy Covariance See the Landscape? A Large-Eddy Simulation Study

被引:21
作者
Xu, Ke [2 ,3 ]
Suehring, Matthias [4 ]
Metzger, Stefan [1 ,2 ]
Durden, David [1 ]
Desai, Ankur R. [2 ]
机构
[1] Battelle Mem Inst, Natl Ecol Observ Network Program, 1685 38th St, Boulder, CO 80301 USA
[2] Univ Wisconsin, Dept Atmospher & Ocean Sci, 1225 W Dayton St,AOSS 1549, Madison, WI 53706 USA
[3] Univ Michigan, Climate & Space Sci & Engn, 2455 Hayward St, Ann Arbor, MI 48109 USA
[4] Leibniz Univ Hannover, Inst Meteorol & Klimatol, Herrenhauser Str 2, D-30419 Hannover, Germany
基金
美国国家科学基金会;
关键词
Eddy covariance; Energy balance; Footprint; Large-eddy simulation; Upscaling; AIRBORNE FLUX MEASUREMENTS; ENERGY-BALANCE CLOSURE; SECONDARY CIRCULATIONS; IMBALANCE PROBLEM; CARBON-DIOXIDE; MODEL; HETEROGENEITY; EXCHANGE; NETWORK; FOREST;
D O I
10.1007/s10546-020-00513-0
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Eddy-covariance fluxes serve as an essential benchmark for Earth system models and remote sensing data. However, two challenges prevent model-data intercomparisons from fully utilizing eddy-covariance fluxes. The first challenge stems from the differing and variable spatial representativeness of the eddy-covariance measurements, or footprint bias and transience. The second originates from the phenomenon of a non-closed energy balance using eddy-covariance measurements, hypothesized to result from unaccounted mesoscale flows or under-sampling of hot spots by flux towers, among others. Previous studies have suggested that these two problems can be mitigated by either building multiple towers or by applying space-time rectification approaches, such as the environmental response function (ERF) approach. Here we ask: (1) How many eddy-flux towers do we need to sufficiently rectify location bias, close the energy budget, and sample the regional domain? (2) Can an advanced space-time rectification approach reduce the tower density, while still adequately sampling the regional flux domain? Furthermore, (3) How accurately can the ERF approach retrieve the surface-flux variation? To answer these questions, we used data from a large-eddy simulation of atmospheric flows above a heterogeneous surface as captured by an ensemble of virtual tower measurements. We calculated eddy-covariance fluxes by spatial and spatio-temporal methods. The spatial eddy-covariance method captured 89% of the prescribed total surface energy flux with about one tower per 15 km(2), while the spatio-temporal method required only one tower per 40 km(2) to capture 95% of surface energy. To capture 97% of energy, applying the ERF approach further reduced the required tower density to one tower per 200 km(2), as a result of space-time rectification and incorporating mesoscale flows. This approach also enabled retrieving the surface spatial variation of the sensible heat flux. The results provide a reference for informing and designing future observation systems based on flux tower clusters, and scale-aware data products.
引用
收藏
页码:85 / 103
页数:19
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