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Abstract
The representation of sub-grid scale boundary layer processes is central to understanding the errors in numerical weather prediction model forecasts. Of particular importance are statistics associated with convective turbulence, notably the temporal and spatial variations of kinetic energy dissipation rate. In this paper we outline how a 1.5-micron Doppler lidar system may be used in this context, and propose an operational network of such systems for use in numerical forecasting. Copyright © 2009 Royal Meteorological Society
You have requested "on-the-fly" machine translation of selected content from our databases. This functionality is provided solely for your convenience and is in no way intended to replace human translation. Show full disclaimer
Neither ProQuest nor its licensors make any representations or warranties with respect to the translations. The translations are automatically generated "AS IS" and "AS AVAILABLE" and are not retained in our systems. PROQUEST AND ITS LICENSORS SPECIFICALLY DISCLAIM ANY AND ALL EXPRESS OR IMPLIED WARRANTIES, INCLUDING WITHOUT LIMITATION, ANY WARRANTIES FOR AVAILABILITY, ACCURACY, TIMELINESS, COMPLETENESS, NON-INFRINGMENT, MERCHANTABILITY OR FITNESS FOR A PARTICULAR PURPOSE. Your use of the translations is subject to all use restrictions contained in your Electronic Products License Agreement and by using the translation functionality you agree to forgo any and all claims against ProQuest or its licensors for your use of the translation functionality and any output derived there from. Hide full disclaimer
Details
1 Centre for Environmental Systems Research, School of Environment and Life Sciences, University of Salford, Salford, Greater Manchester, M5 4WT