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Published byArthur Mills Modified over 9 years ago
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- tBM - topographical boundary layer model Dr. O. Liechti OlivierLiechtiAuK@compuserve.com
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Short Range Forecasting Methods of Fog, Visibility, and Low Clouds Phase IInventory Phase IIResearch & Development Phase IIIDissemination COST Action 722
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Phase IIResearch & Development WG IInitial Data WG IIModels WG IIIStatistical Methods
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WG IInitial data CDGradiosonde CDGremote sensing ZRHstations in complex topography ZRHmodel aircraft local vertical profiles
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WG IIModels DGM - LM - PAFOG FARPEGE - ALADIN - COBEL/ISBA CHEZMW - aLMo - COBEL/ISBA EZMW - aLMo - tBM GFS - NMM - NMM 3D - 2D - 1D
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pools of cold air locally enhanced snow grains
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Zurich AirportWinterthur
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IR radiative cooling
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nocturnal cooling rates
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morning fogfoggy days
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thermodynamics of low stratus radiative loss of heat surface cooling convection supersaturation, condensation snow grains (locally enhanced)
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simulation of pooling cold air IR radiative flux convection topographical volume effect local circulation through differential cooling topographical boundary layer model (tBM)
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tBM for Zurich airport
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area-elevation-distributions for the areas A, B, C, D tBM simulation (2-dim, 24 hrs)
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A B C D T [C] tBM simulation (2-dim, 24 hrs) pure topographical effect !
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A B C D h [mMSL] tBM simulation (2-dim, 24 hrs) pure topographical effect !
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models in COST 722 modeltopoz-Mixx-Mixsoil COBELflatshear––1d-ISBA PAFOGflatshear––Bewuchs tBMV(z)convectioncirculation0d NMMflatparametr.circulation1d --> comparison @ Paris CDG 03/04/05
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