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Published byHope Briggs Modified over 9 years ago
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Chapter 6: mesoscale gravity waves This ppt summarizes the slides in the textbook. The theory is covered in class. Note: this ppt does not include section 6.6 Bores.
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Iowa gravity wave time lapse movie mpeg You Tube
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UK Ireland cold front
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5/24/2002, 21:07 UTC – IHOP
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Aral Sea
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Australia
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Fig. 6.1: isochrones of a mesoscale gravity wave crest during a major East Coast snowstorm. The wave was detected in the pressure trace. The wind barbs indicate the vector surface wind shift upon wave passage. x Greensboro (GSO)
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dry adiabat ( =46°C) moist adiabat ( w =16°C) w values (°C) Fig. 6.9: the mesoscale gravity wave event may have been triggered by elevated convection, or gravity wave adjustment. The stable low-level layer may have allowed wave ducting towards the NE.
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Fig. 6.11: synoptic setting of gravity wave activity (p’~ a few mb)
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Fig. 6.2: SLP analysis in a Midwest snowstorm. dotted lines: wave crests, dashed lines: troughs
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Fig. 6.10: schematic of a linear plane mesoscale gravity wave propagating to the right (U o =0)
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see youtube video
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Fig. 6.6: polarization relations between ’, p’, u’, and w’ in a westward tilting internal gravity wave blue = cold, red = warm
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Critical level: level where wave energy is absorbed cgcg c Fig. 6.7 Fig. 6.8
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geostrophic adjustment: principle Rossby radius of deformation: see COMET module “the balancing act of geostrophic adjustment”the balancing act of geostrophic adjustment see YouTube video: geostrophic adjustment: inertio-gravity waves and the Coriolis force
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Will a feature last or dissipate? Estimate its L R
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6.6 undular bores and solitary waves: separate slide show
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