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Introduction
Obukhov Length is a well-known length scale in boundary layer meteorology. It characterizes stability effects (buoyancy versus shear turbulence) in the turbulent layer of the atmosphere near the surface. It is used in air pollution modelling and to characterize the shape of wind profiles in wind energy applications (among many other applications).
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Beljaars, A., Brown, A. and Wood, N., 2004: A new parametrization of turbulent orographic form drag. QJRMS, 130, pp.1327-1347.
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This document has been produced in the context of the Copernicus Climate Change Service (C3S). The activities leading to these results have been contracted by the European Centre for Medium-Range Weather Forecasts, operator of C3S on behalf of the European Union (Delegation agreement Agreement signed on 11/11/2014 and Contribution Agreement signed on 22/07/2021). All information in this document is provided "as is" and no guarantee or warranty is given that the information is fit for any particular purpose. The users thereof use the information at their sole risk and liability. For the avoidance of all doubt , the European Commission and the European Centre for Medium - Range Weather Forecasts have no liability in respect of this document, which is merely representing the author's view. |
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