Air movement ENVS 09-26-08. what makes air move ? air moves from areas of high atmospheric pressure...
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![Page 1: Air movement ENVS 09-26-08. what makes air move ? air moves from areas of high atmospheric pressure to areas of low atmospheric pressure low pressure.](https://reader030.fdocuments.us/reader030/viewer/2022032800/56649d3f5503460f94a194ff/html5/thumbnails/1.jpg)
air movement
ENVS 09-26-08
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what makes air move ?
• air moves from areas of high atmospheric pressure to areas of low atmospheric pressure
• low pressure areas – troughs
• high pressure areas - ridges
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http://www.dnr.sc.gov/climate/sco/Education/wxmap/wxmap.gif
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• isobars = equal lines of pressure• distance between isobars → change in pressure
over distance = pressure gradient• isobars close together → pressure varies rapidly
→ air flows rapidly form high to low pressure → strong winds
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pressure gradient force
• describes how rapidly air pressure changes between two points
• steep gradient (isobars close together) → air moves rapidly → pressure gradient force is large
• shallow gradient → pressure gradient force is small
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but…
• most atmospheric patterns are swirls of clouds and winds …
• very few straight patterns
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The Rotating Earth → Coriolis “Force”
• Earth is a rotating system
• On earth things that move straight appear to move on curved path as earth rotates beneath
• swirly cloud patterns on satellite images, zone of westerlies etc.
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Coriolis Effect does NOT
determine the way your sink drains !
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Coriolis Effect with (almost) no Math
a) movement to and from the poles
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N-S moving air:
• air has larger tangential velocity at equator than at pole (equator = max, pole = 0)
• as air moves polewards it maintains its tangential velocity
• since it is encountering slower moving air it “overtakes” these higher latitude air masses
• apparent deflection towards the right (in N – hemisphere)
• air moving towards the equator seems to lag lower latitude air masses → again, deflection to the right
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from: www.bom.gov.au/info/ftweather/ page_14.shtml
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Coriolis Effect Summary:
• earth is a rotational system
• standing on earth, objects that move on straight line seem to be following curved paths (because we are rotating)
• Coriolis effect deflects air masses– towards right on northern hemisphere– towards left on southern hemisphere
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Coriolis Effect - Magnitude
• effect is very small
• only affects large scale movements (Hurricanes, ocean currents etc.)
• it will not affect small, household scale currents
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air currents II
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influences on air currents
• pressure gradient force: air flows from areas of high pressure to areas of low pressure – the more rapid the change in pressure the stronger the flow
• Coriolis effect: due to rotation of the earth air masses are deflected to the right on northern hemisphere and deflected to the left on southern hemisphere
• resulting flow: geostrophic flow
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Coriolis effect
• rotating earth → air masses are moving on curved paths across earth
• on northern hemisphere: deflection to the right
• on southern hemisphere: deflection to the left
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coriolis effect
http://www.physics.umd.edu/lecdem/services/demos/demosd5/d5-11.htm
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Coriolis effect demonstrations
stationary disk
rotating disk – stationary observer
rotating disk, rotating observer
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one last time:
• on northern hemisphere – air is deflected to the right
• on southern hemisphere – air is deflected to the left
due to the rotation of the earth
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close to ground:
• friction between atmosphere and surface slows air down
• winds are stronger at high elevations
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three influences on air movement
• pressure gradient force
• Coriolis effect
• friction
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conservation of angular momentum
• combination of pressure gradient force and Coriolis effect cause air to spin
• as air is sucked into low-pressure area it spins faster and faster due to the conservation of angular momentum
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at high altitudes
• friction between atmosphere and earth’s surface is negligible
• air currents are influenced by balance between pressure gradient force and Coriolis effect
→ geostrophic winds
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development of geostrophic flow
• pressure gradient force gets air moving• Coriolis effect deflects to right and keeps
deflecting until…• effects of pressure gradient and Coriolis effect
cancel out→ now wind flows almost parallel to isobars !
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airflow symbols
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http://www.atmos.washington.edu/~mcmurdie/oct96/300mb_geownd_17oct.gif
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two ways to depict air pressure
• lines of equal pressure (isobars)
• equal pressure surfaces
http://www.physicalgeography.net/fundamentals/7d.html
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constant pressure levels
• are at higher elevation for high pressure areas
• are at lower elevation for low pressure areas
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http://www.srh.noaa.gov/hun/stormsurveys/2008-02-06/weather/12z_500mb.jpg
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Effect on Hurricanes:
• balance between Coriolis force and pressure gradient
• causes rotation of storm system
• counterclockwise in N-hemisphere
• clockwise in S-hemisphere
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surfacewinds
http://www.srh.noaa.gov/hun/stormsurveys/2008-02-06/weather/12z_500mb.jpg
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surface winds or friction layer winds
• friction between atmpsphere and earth’s surface prevents air masses to reach equilibrium between coriolis effect and pressure gradient force
• friction layer winds blow at an angle to the isobars
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local wind systems
• land and sea breezes
• Föhn winds (Chinook)
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land and sea breezes
• differential heating between sea and land
• land heats up faster and warm air rises (low pressure area over land)
• process reverses at night
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Föhn winds
• orographic rain – air masses lose most of their moisture when they cross a mountain range
• on the other side the air is warm and very clear
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for all of you who still haven’t enough…
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Global Atmospheric Circulation
ENVS 110 - 10-03-2008
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http://en.wikipedia.org/wiki/Image:IntertropicalConvergenceZone-EO.jpg
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Vertical air movement in the atmosphere
http://en.wikipedia.org/wiki/Image:Omega-500-july-era40-1979.png
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Polar Front
Planetary frontal zone
Mixing of warm and cold air exchange of heat from subtropics to higher latitudes
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Local effects
• Asian monsoon
• North American monsoon
http://img.timeinc.net/time/photoessays/2007/india_monsoon/india_monsoon_01.jpg
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Differential warming between continents and oceans• Summer – Indian sub continents heats up• Develops low-pressure zone over continent• Sucks in moist air from surrounding oceans
• India:– Warm subtropical oceans extremely moist
oceanic air– Orographic rain on southern edge of Himalayas
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