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P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

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Page 1: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

p. 277

Page 2: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 3: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

Cold Front: cold air behind front (often to NW)abrupt cooling as it passes

Warm Front: warm air behind front (often to S)more gradual warming

Stationary front: divides airmasses, but little forwardmotion

Occluded front: cold front “catches up” to warm frontwarm sector now only found aloftless temperature contrast

Page 4: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 5: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

Vertical displacement along a cold front

Page 6: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 7: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

COLD FRONT

Infrared Imagery Radar Imagery

Page 8: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

Profile of a warm front

Page 9: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 10: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

Occlusion sequence

p. 291

Page 11: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 12: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 13: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 14: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

Stationary Front

POLAR FRONT

POLAR AIRMASS

SUBTROPICAL AIRMASS

Page 15: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 16: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

Maturity

Page 17: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

Lifting processes and cloud cover

Page 18: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

Occlusion

Page 19: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 20: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 21: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 22: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

Convergence and divergencealong a Rossby wave

Page 23: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

If lows and highs aloft and at the surface are above one another, the systems will weaken !

Page 24: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

Divergencealoft promotesthe surfacelow

Convergencealoft promotesthe surfacehigh

Surfacedivergence

Surfaceconvergence

Page 25: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

Longwaves

Page 26: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

MIGRATE THROUGHTHE LONGWAVE TROUGHS

Page 27: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

1

2

3

Differential temperatureadvection intensifies thewave

Condensation mayrelease even moreheat energy for the storm

Less upper level divergence

No temp advection

Page 28: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

Relative vorticity

Page 29: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

Vorticity through a Rossby wave

Page 30: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 31: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 32: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 33: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 34: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 35: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

Values of absolute vorticity on a hypothetical 500 mb map

Page 36: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

Temperature variations in the lower atmospherelead to variations in upper-level pressure

Page 37: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 38: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 39: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

Example of a midlatitude cyclone

April 15

Page 40: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

April 16

Page 41: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

April 18

Page 42: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

• Flow patterns and large-scale weather

–Zonal height patterns “zonal flow”

Page 43: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

Meridional flow pattern

Page 44: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

Typical winter midlatitude cyclone paths

Page 45: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 46: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 47: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. cyclogenesisB. occlusionC. maturityD. senescence

What is the term for this early stage in the life cycle of a midlatitude cyclone?

Page 48: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. cyclogenesisB. occlusionC. maturityD. senescence

What is the term for this early stage in the life cycle of a midlatitude cyclone?

Page 49: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. cyclogenesisB. occlusionC. maturityD. senescence

What is the term for this stage in the life cycle of a midlatitude cyclone?

Page 50: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. cyclogenesisB. occlusionC. maturityD. senescence

What is the term for this stage in the life cycle of a midlatitude cyclone?

Page 51: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. AB. BC. CD. D

In which area would overrunning occur?

A

CB

D

Page 52: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. AB. BC. CD. D

In which area would overrunning occur?

A

CB

D

Page 53: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. AB. BC. CD. D

Which location would have the lowest pressure?

A

CB

D

Page 54: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. AB. BC. CD. D

Which location would have the lowest pressure?

A

CB

D

Page 55: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. 1B. 2C. 3D. 4

Which area would have the greatest positive relative vorticity?

[insert figure 10-4]

Page 56: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. 1B. 2C. 3D. 4

Which area would have the greatest positive relative vorticity?

[insert figure 10-4]

Page 57: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. 1B. 2C. 3D. 4

Which area would have the least relative vorticity?

Page 58: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. 1B. 2C. 3D. 4

Which area would have the least relative vorticity?

Page 59: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. uplift over a surface lowB. sinking airC. chaotic flowD. anticyclones

To what might divergence along the jet stream contribute?

[insert figure 10-7]

Page 60: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. uplift over a surface lowB. sinking airC. chaotic flowD. anticyclones

To what might divergence along the jet stream contribute?

Page 61: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. a barotrophic atmosphereB. divergence aloftC. convergence aloftD. negative relative vorticity

What would cause this surface low to strengthen?

[insert figure 10-11b]

Page 62: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. a barotrophic atmosphereB. divergence aloftC. convergence aloftD. negative relative vorticity

What would cause this surface low to strengthen?

Page 63: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. AB. BC. CD. D

Where is the “dry conveyor belt” in the diagram?

B

A

D

C

Page 64: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. AB. BC. CD. D

Where is the “dry conveyor belt” in the diagram?

B

A

D

C

Page 65: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. baroclinicB. zonalC. meridionalD. mythical

Which term best describes the upper air flow in the diagram?

Page 66: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. baroclinicB. zonalC. meridionalD. mythical

Which term best describes the upper air flow in the diagram?

Page 67: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. baroclinicB. zonalC. meridionalD. mythical

Which term best describes the upper air flow in the diagram?

[insert figure 10-15b]

Page 68: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming

A. baroclinicB. zonalC. meridionalD. mythical

Which term best describes the upper air flow in the diagram?

insert figure 10-15 a]

Page 69: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming
Page 70: P. 277. Cold Front: cold air behind front (often to NW) abrupt cooling as it passes Warm Front:warm air behind front (often to S) more gradual warming