Measurement of the Sensible Eddy Heat Flux Based on Spatial Averaging of Continuous Ground-Based Observations
Using the standard eddy-covariance (EC) method to quantify mass and energy exchange at a single location usually results in an underestimation of vertical eddy fluxes at the surface. In order to better understand the reasons for this underestimation, an experimental set-up is presented that is based...
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Veröffentlicht in: | Boundary-layer meteorology 2008-07, Vol.128 (1), p.151-172 |
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Format: | Artikel |
Sprache: | eng |
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