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Conceptual Models of Cold Air Features: Comma
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Cloud Structures in Satellite Images
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Typical development in initial phase often „ enhanced cumuli cloud (EC)“ EC
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Typical cloud configurations in comma stage meso-scale cloud spiral usually in cold air behind CF bright in all three channels (WV, IR,VIS) discriminating between: –comma head (with embedded convective cells) –comma tail (less bright and smoother structure)
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Comma
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Meteorological Physical Background
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Physical Background of "Comma" Two types of development observed: –development within cold air: barotropic instability, baroclinic instability and CISK mechanisms –development out of occlusion spirals: the innermost part of the occlusion spiral is torn off;
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Physical Background of "Comma" Conveyor belt theory: –Comma cloud within rising branch of dry intrusion
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dry intrusion
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Key Parameters
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Relevant numerical parameters and their typical distribution situated in front of (close to) trough line –at 1000 hPa –at 500 hPa
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comma
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Relevant numerical parameters and their typical distribution within CA unstable
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CA unstable
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Relevant numerical parameters and their typical distribution vorticity maximum –at the rear edge PVA maximum –directly above cloud feature height of IPV is lowest at comma cloud
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Vorticity maximum:
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PVA maximum:
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Height of IPV=2:
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Relevant numerical parameters and their typical distribution At the left side of the jet axis, In several cases in the left exit region of a jet streak In such case spiral feature of comma weaker –shear vorticity
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Jet streak PVA Jet streak
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Typical Appearance in Vertical Cross Sections
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Isentrops: –unstable layer from surface up to 700hPa –frontal zone only in middle levels above the unstable layer unstable upper level front
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unstable
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Divergence and vertical motion: –convergence in low layer –divergence above –upward motion in thick layer within comma
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convergence divergence
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Vorticity maximum – at the rear of the comma feature –curvature dominant –shear in case of jet streak PVA –above comma feature
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PVA
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