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Conceptual Models of Cold Air Features: Comma

Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

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Page 1: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

Conceptual Models of Cold Air Features:

Comma

Page 2: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

Cloud Structures in Satellite Images

Page 3: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

Typical development

• in initial phase often „ enhanced cumuli cloud (EC)“ EC

Page 4: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

EC

EC

Page 5: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

EC

EC

Page 6: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

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)

Page 7: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images
Page 8: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

Comma

Page 9: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

Comma

Page 10: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

Comma

Page 11: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

Comma

Page 12: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

Meteorological Physical Background

Page 13: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

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;

Page 14: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

Physical Background of "Comma"

• Conveyor belt theory:

– Comma cloud within rising branch of dry intrusion

Page 15: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

dry intrusion

Page 16: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

Key Parameters

Page 17: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

Relevant numerical parameters and their

typical distribution

• situated in front of (close to) trough line – at 1000 hPa

– at 500 hPa

Page 18: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

comma

Page 19: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

Relevant numerical parameters and their typical distribution

• within CA• unstable

Page 20: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

CAunstable

Page 21: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

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

Page 22: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

Vorticity maximum:

Page 23: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

PVA maximum:

Page 24: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

Height of IPV=2:

Page 25: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

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

Page 26: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

Jet streak

PVA

Jet streak

Page 27: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

Typical Appearance in Vertical Cross Sections

Page 28: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images
Page 29: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

• Isentrops:– unstable layer from

surface up to 700hPa

– frontal zone only in middle levels above the unstable layer

unstable

upperlevelfront

Page 30: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

unstable

Page 31: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

• Divergence and vertical motion:– convergence in low

layer– divergence above– upward motion in

thick layer within comma

Page 32: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

convergence

divergence

Page 33: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images
Page 34: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images
Page 35: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

• Vorticity maximum– at the rear of the

comma feature– curvature dominant – shear in case of jet

streak

• PVA – above comma feature

Page 36: Conceptual Models of Cold Air Features: Comma. Cloud Structures in Satellite Images

PVA