Meteorology 5.07 Wind References: Air Command Weather Manual Chapters 5 and 11 FTGU Pages 129-132.
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Transcript of Meteorology 5.07 Wind References: Air Command Weather Manual Chapters 5 and 11 FTGU Pages 129-132.
![Page 1: Meteorology 5.07 Wind References: Air Command Weather Manual Chapters 5 and 11 FTGU Pages 129-132.](https://reader036.fdocuments.net/reader036/viewer/2022062314/56649d765503460f94a570cb/html5/thumbnails/1.jpg)
Meteorology
5.07 WindReferences:
Air Command Weather Manual Chapters 5 and 11FTGU Pages 129-132
![Page 2: Meteorology 5.07 Wind References: Air Command Weather Manual Chapters 5 and 11 FTGU Pages 129-132.](https://reader036.fdocuments.net/reader036/viewer/2022062314/56649d765503460f94a570cb/html5/thumbnails/2.jpg)
5.07 Wind
• MTPs:– Pressure Gradient– Veering and Backing– Coriolis Force– Surface Friction– Gusts and Squalls– Diurnal Effects
![Page 3: Meteorology 5.07 Wind References: Air Command Weather Manual Chapters 5 and 11 FTGU Pages 129-132.](https://reader036.fdocuments.net/reader036/viewer/2022062314/56649d765503460f94a570cb/html5/thumbnails/3.jpg)
Pressure Gradient
• Wind– the horizontal movement of air– caused by pressure differences in the
horizontal
![Page 4: Meteorology 5.07 Wind References: Air Command Weather Manual Chapters 5 and 11 FTGU Pages 129-132.](https://reader036.fdocuments.net/reader036/viewer/2022062314/56649d765503460f94a570cb/html5/thumbnails/4.jpg)
Pressure Gradient
• Pressure Gradient– the rate of change of pressure over a given distance– measured at right angles to the isobars
• close together = steeper gradient and stronger winds• further apart = shallower gradient and weaker winds
![Page 5: Meteorology 5.07 Wind References: Air Command Weather Manual Chapters 5 and 11 FTGU Pages 129-132.](https://reader036.fdocuments.net/reader036/viewer/2022062314/56649d765503460f94a570cb/html5/thumbnails/5.jpg)
Pressure Gradient
![Page 6: Meteorology 5.07 Wind References: Air Command Weather Manual Chapters 5 and 11 FTGU Pages 129-132.](https://reader036.fdocuments.net/reader036/viewer/2022062314/56649d765503460f94a570cb/html5/thumbnails/6.jpg)
Veering and Backing
Veering– Wind changes direction
clockwise– Wind veers and increases
during the day– Wind veers and increases
with increase in altitude
Backing•Wind changes direction counter-clockwise•Wind backs and decreases at night•Wind backs and decreases with decrease in altitude
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Veering and Backing
2222
320°
c
270° b
240°a
180°
1 140°
2 120°3
BACKING
VEERING
N Example:Winds start the day at 300o and by 1400 the winds are 340o and by night they are 310o
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Coriolis Force
• Coriolis Force:– Earth turns below atmosphere
• In N Hemisphere deflected to the right• To left in S Hemisphere• http://www.youtube.com/watch?v=_36MiCUS1ro
![Page 9: Meteorology 5.07 Wind References: Air Command Weather Manual Chapters 5 and 11 FTGU Pages 129-132.](https://reader036.fdocuments.net/reader036/viewer/2022062314/56649d765503460f94a570cb/html5/thumbnails/9.jpg)
Confirmation
• Wind is:
• Pressure Gradient is:
• Backing is:
• Describe Coriolis Force.
![Page 10: Meteorology 5.07 Wind References: Air Command Weather Manual Chapters 5 and 11 FTGU Pages 129-132.](https://reader036.fdocuments.net/reader036/viewer/2022062314/56649d765503460f94a570cb/html5/thumbnails/10.jpg)
Surface Friction
• Surface friction– Friction between surface and atmosphere slows
movement of air, this in turn slows Coriolis force– Only up to a few thousand feet (except in mountainous
regions)
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Gusts and Squalls
• Gusts– a brief rapid increase
of wind speed. – may be associated
with a rapid change in wind direction
– Causes may be related to mechanical turbulence and unequal heating
1414
Mechanical Turbulence Unequal Heating
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Gusts and Squalls
• Squalls–A sudden increase in wind strength
–Longer than a gust
–May be caused by a fast moving cold front or thunderstorm
–May be accompanied by a rapid change in direction
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Confirmation
• What is surface friction and what are its effects?
• Gusty conditions may be caused by
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Diurnal Effects
• If isobaric pattern and pressure gradient are identical– During day…– At night…
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Diurnal Effects
Land and Sea Breezes
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Diurnal Effects
1515
Land BreezeLand Breeze
Warm Air Cold Air
HL
This condition is very local and affects only a narrow area along the coast:
Occurs at night; and
Wind blows from the land (high pressure) towards the warm water (low pressure area)
11
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Diurnal Effects
1616
Sea BreezeSea Breeze
H
Cold Air
L
Warm Air
Occur during the day
Wind blows from the sea
12
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Diurnal Effects
Memory Tool
Ana goes up and throws the Kat down.
The Kat comes down at night
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Diurnal Effects
1818
Katabatic WindKatabatic WindAt night, the slopes of hills cool. The air
contact with them becomes cooler and therefore denser and it blows down the slope. Also known as a Mountain Breeze.
Denser Air
Less Dense Air
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Diurnal Effects
1717
AnabaticAnabatic WindWindSlopes of hills not covered by snow will be
warmed during the day. The air in contact with them becomes warmer and less dense and therefore flows up the slope. Also known as a Valley Breeze.
Less Dense Air
Denser Air
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Confirmation
• When do sea breezes occur?
• What causes a Katabatic wind?
• What is it called when vapour changes to liquid?
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The Effects of a Hurricane