The Detection Of Nonstationarity In The Determination Of Deposition Fluxes
Price
Free (open access)
Transaction
Volume
36
Pages
6
Published
1999
Size
356 kb
Paper DOI
10.2495/EURO990342
Copyright
WIT Press
Author(s)
L. Dutaur, S. Cieslik, A. Carrara and A. Lopez
Abstract
The Detection of Nonstationarity in the Determination of Deposition Fluxes A contribution to subproject BIATEX-2 L Dutaur\ S. Cieslik\ A. Carrara^ and A. Lopez^ ' Environment Institute, Joint Research Centre, 21020 Ispra (VA), Italy Laboratoire d'Aerologie, Universite Toulouse III, 31400 Toulouse, France Introduction The eddy-correlation method is largely considered as the most reliable way of measuring vertical fluxes of scalar variables between the earth's surface and the atmosphere. It is based on the calculation of the covariance of two rapidly fluctuating quantities: the vertical component of the wind vector (H>) and the variable under consideration (noted hereafter as C where this variable is a concentration). Fluctuations are defined by W (1) where the overbar denotes the time averaging operation; the flux is then expressed by
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