Download - Meteorology Winds

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Page 1: Meteorology Winds

Sep 2012

Lesson 4.4

Meteorology

Winds

Page 2: Meteorology Winds

Reference

From the Ground UpChapter 6.4:WindsPages 130 - 136

Page 3: Meteorology Winds

Introduction• Wind is the horizontal movement of air in

different areas and altitudes.

• It is important that pilots know where winds are, how strong and from what direction they flow, and how they change.

Page 4: Meteorology Winds

Outline• Wind Types• Wind Speed and Direction• Wind Effects

Page 5: Meteorology Winds

Winds• Wind is horizontal movement of air

• Heating of Earth creates pressure differences, air flows from high to low, therefore wind

• Upper Level Winds flow parallel to isobars and from high to low pressure areas

• Surface Winds are below 3000 ft, and are slowed by surface friction

Page 6: Meteorology Winds

Land & Sea Breezes• Sea Breeze

– Land heats faster than water during day (lower pressure)– Wind blows from water towards land

Page 7: Meteorology Winds

Land & Sea Breezes• Land Breeze

– Land cools faster than water at night (higher pressure)– Wind blows from land towards water

Page 8: Meteorology Winds

Mountain Winds• Katabatic Wind (AKA Mountain Breeze)

– At night, slope cools, air becomes denser, wind flows down from mountain

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Mountain Winds• Anabatic Wind (AKA Valley Breeze)

– During day, slope heats, air becomes less dense, flows up from valley

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Mountain Winds• Mountain Wave

– Air deflected after flowing over mountain oscillates (or bounces) up and down violently in a wave pattern.

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Gusts and Squalls• Gust

– Sudden and brief increase in wind speed and direction (several seconds)

– Usually caused by mechanical turbulence

• Squall– Sudden increase in wind speed and direction, but

last longer then a gust (several minutes)– Usually caused by fast moving cold front or

thunderstorm

Page 12: Meteorology Winds

Wind Speed & Direction• Veering is increase in wind direction

• Backing is decrease in wind direction

• Wind veers and increases with altitude (due to lack of surface friction)

• Diurnal Variation– Wind backs and decreases at night– Wind veers and increases during day (more ground heating)

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Wind Effects• Eddies

– Swirling air or vortices– Produced by friction between moving air and ground

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Wind Effects• Dust Devils

– Super-heated concentrated lows on hot, clear, stable, days– Made visible by dust or sand

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Wind Effects• Tornadoes

– Very concentrated, violent lows formed in unstable weather

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Wind Effects• Jet Stream

– Narrow bands of high-altitude and high-speed winds– Normally 2 or 3 over North America

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Next Lesson

4.5 – MeteorologyHumidity, Temperature & Stability

From the Ground UpChapter 6.5:Humidity, Temperature and StabilityPages 136 - 140


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