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Meteorology Winds

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Meteorology Winds. Reference. From the Ground Up Chapter 6.4: Winds Pages 130 - 136. 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. - PowerPoint PPT Presentation
17
Sep 2012 Lesson 4.4 Meteorology Winds
Transcript
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

Page 9: Meteorology Winds

Mountain Winds• Anabatic Wind (AKA Valley Breeze)

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

Page 10: Meteorology Winds

Mountain Winds• Mountain Wave

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

Page 11: Meteorology Winds

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)

Page 13: Meteorology Winds

Wind Effects• Eddies

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

Page 14: Meteorology Winds

Wind Effects• Dust Devils

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

Page 15: Meteorology Winds

Wind Effects• Tornadoes

– Very concentrated, violent lows formed in unstable weather

Page 16: Meteorology Winds

Wind Effects• Jet Stream

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

Page 17: Meteorology Winds

Next Lesson

4.5 – MeteorologyHumidity, Temperature & Stability

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


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