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Living in Our Ocean of Air Chapter 1-2 WX Elements. Source: http://www.geog.ucsb.edu/~joel/g110_w06/lecture_notes/sun_angle/agburt02_12.jpg. Angle of incoming radiation and hours of sunlight affect heating. Source: http://easyweb.easynet.co.uk/~geography.net/kew/factors(1).htm.

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Presentation Transcript
slide2
Source: http://www.geog.ucsb.edu/~joel/g110_w06/lecture_notes/sun_angle/agburt02_12.jpg
slide3
Angle of incoming radiation and hours of sunlight affect heating.
  • Source: http://easyweb.easynet.co.uk/~geography.net/kew/factors(1).htm
slide5
Hot air rises generating an area of low pressure.
  • Air cools as it rises and falls generating an area of high pressure.
slide6
In the northern hemisphere, low pressure rotates in a counterclockwise direction.
  • In the northern hemisphere, high pressure rotates in a clockwise direction.
  • Source: http://myweb.cwpost.liu.edu/vdivener/notes/High-Low%20map.gif
wind facts
Wind Facts

Air moves horizontally from an area of high pressure to an area of low pressure.

wind facts1
Wind Facts

Wind speed is measured with an anemometer.

wind facts2
Wind Facts
  • is cooling caused by the wind.
  • Local winds blow over a short distance.
wind facts3
Wind Facts
  • sea breeze- air over the water is cooler and denser than air over land. The flow is from higher pressure to lower pressure.
wind facts4
Wind Facts
  • land breeze - at night air over land is cooler and denser. Air flows from higher pressure to lower pressure.
wind facts5
Wind Facts
  • Global winds blow steadily from specific directions over long distances.

Why did Columbus land

In the Caribbean Islands?

Wind Graphic Display

wind facts6
Wind Facts

Gaspard Gustave de Coriolis

  • The Coriolis Effect, curvature of the wind, is caused by Earth’s rotation.
wind facts7
Wind Facts
  • Jet streams are high-speed winds about 10 km above Earth’s surface.

What’s happening right now? What does it mean for weather for the next little while?

links
Links
  • GOES satellite image index
  • Weatherunderground.com
low clouds
Low Clouds
  • Stratus
    • Sheet - like cloud.
    • No turbulence.
    • May be risen fog.
    • Light drizzle or snow.
    • Close to Earth’s surface.
    • Can hide danger.
low clouds1
Low Clouds
  • Stratocumulus
    • Rolls or global masses.
    • Bulbous protrusions.
    • Heavy rain and snow
    • Varying turbulence.
    • Masks higher severe cloud buildups.
low clouds2
Low Clouds
  • Cumulonimbus
    • Vertical growth group.
    • Top has anvil shape.
    • High winds, snow, hail, rain, lightning, and tornadoes.
    • Extreme turbulence.
low clouds3
Low Clouds
  • Nimbostratus
    • Shapeless, low-level, moderate precipitation.
    • Fog and precipitation found beneath.
    • Visibility restricted.
    • Calm to light winds.
middle clouds
Middle Clouds
  • Altostratus
    • Relatively thin.
    • Sun may be seen through veil.
    • Ice crystals and super-cooled water.
    • Light precipitation.
    • Poor surface visibility.
middle clouds1
Middle Clouds
  • Altocumulus
    • Wavy solid clouds with rounded outline.
    • Light intermittent rain or snow.
    • Commonly followed by thunderstorms.
    • Poor visibility and moderate surface winds.
high clouds
High Clouds
  • Cirrus
    • Thin feathery clouds.
    • No precipitation.
    • Sign of approaching bad weather.
high clouds1
High Clouds
  • Cirrostratus
    • Thin, resembles a sheet or veil.
    • No precipitation.
    • Nearly transparent.
    • Often sign of approaching bad weather.
high clouds2
High Clouds
  • Cirrocumulus
    • Thin clouds.
    • Indicates high-level instability.
    • Similar to cirrostratus but they have a slightly “bumpy” appearance.
fracto and lenticular
Fracto and Lenticular
  • Fracto
    • Broken and/or ragged.
    • Cumulus fractos.
  • Lenticular
    • Lens-like shape.
    • Tells turbulence, visibility, precipitation.
cumulus with vertical growth
Cumulus with Vertical Growth
  • Fair weather cumulus
    • A puffy, cottonball appearance.
    • Develops from thermal updrafts.
    • Flights below can be bumpy and choppy.
cumulus with vertical growth1
Cumulus with Vertical Growth
  • Vertical growth, or building cumulus
    • Produce strong rain and moderate to severe turbulence.
    • Very strong updrafts.
    • With further building and increase in intensity, it becomes a thunderstorm.
fog types
Fog Types
  • Radiation Fog
    • Formed at night when land surfaces radiate much of the heat absorbed from the Sun back into space.
    • The cool land surface cools the air near it to below the dew point and fog is formed.
fog types1
Fog Types
  • High Inversion Fog
    • A low fog.
    • Formed by condensation of water vapor at or near the top of cool air, which is overlain by a warmer air layer.
air mass type and origination1
Air Mass Type and Origination
  • Air masses are identified by letter symbols.
  • A polar air mass (P) is cold.
  • A tropical air mass (T) is hot.
  • A maritime air mass (m) forms over water and is humid.
  • A continental air mass (c) forms over land and is dry.
air mass type and origination2
Air Mass Type and Origination
  • Aviators and meteorologists in the continental United States are chiefly concerned with air masses origination at two sources.
    • Masses that move southward from Polar Regions.
    • Masses that move northward from Tropical Regions.
air mass type and origination3
Air Mass Type and Origination
  • Cold air masses
    • Continental polar (cP)
    • Maritime polar (mP)
    • Arctic (A)
  • The principle warm air mass is maritime tropic (mT)
temperature classification of air masses
Temperature Classification of Air Masses
  • Based upon its temperature in relation to the surface over which it passes.
  • A cold air mass (k) is cooler than the Earth’s surface over which it is moving.
  • A warm air mass (w) is warmer than the Earth’s surface over which it is moving.
temperature classification of air masses1
Temperature Classification of Air Masses
  • Continental polar cold (cPk) - originates in the polar zone and moves south over a warm surface.
  • Maritime tropical warm (mTw) - originates over the Gulf of Mexico and moves toward the north over a cold surface.
characteristics of air masses
Characteristics of Air Masses
  • As an air mass moves away from its source, its original characteristics are changed because of the surface it passes over. It may:
    • Become warmer or colder.
    • Absorb or lose moisture.
    • Be lifted up by mountains or subside into valleys.
  • Cold air masses move more rapidly than warm air masses.
fronts
Fronts
  • The boundaries between air masses are called frontal zones or fronts.
  • This boundary or front moves along the Earth’s surface as one air mass displaces another.
    • If a cold air mass replaces a warmer air mass, the boundary is called a cold front.
    • If a warm air mass replaces a cold air mass, the boundary is called a warm front.
fronts1
Fronts
  • Cold Fronts
    • As warm air is forced upward, it cools, condenses into clouds, creating thunderstorms.
    • If movement is rapid, with an abundance of water vapor, violent weather takes place.
    • Squall lines develop ahead of the front.
fronts2
Fronts
  • Cold Fronts
    • Along the cold front there will be a low-pressure cell where the weather is at its worst.
      • Almost any type of clouds can be found near the cell.
      • Poor visibility, low ceilings and rain in summer.
      • Freezing rain and snow in winter.
fronts3
Fronts
  • Warm Fronts
    • Connected to a low-pressure cell, travels northeastward.
    • If cell did not move, the front would dissipate.
    • Front slips upward over cool air and forms a wedge.
    • Rises slowly which delays condensation.
fronts4
Fronts
  • Warm Fronts
    • Front is announced by cirrus clouds.
    • As front approaches other clouds, skies darken.
    • Near the frontal boundary, clouds are low, gentle rain falls and visibility is poor.
    • Warm rain falling into cooler air causes fog.
fronts5
Fronts
  • Warm Fronts
    • After front passes, there is a rise in temperatures, general clearing and change in wind direction.
    • In winter a warm front causes icing conditions at low altitudes.
    • In northern latitudes snow may also be produced.
fronts6
Fronts
  • Stationary Front
    • When air masses stop, a stationary front develops.
    • Weather can be bad for aviation along the front.
    • About every form of weather can be found.
front
Front
  • Stationary Front
    • Toward the trailing edge of the any front there will be a stationary-front condition.
    • The trailing edge stationary fronts are a great distance from the parent cell.
    • As the distance become greater the front no longer exists.
front1
Front
  • Occluded Front
    • There is a tendency for a horizontal bend or wave to occur along the front.
    • After a frontal bend starts, cold air moves ahead of a warm front.
    • The cold section moves faster than the warm section.
terrain factors
Terrain Factors
  • The presence of mountain ranges change the characteristics of a front.
  • As air masses enter the United States the mountains cause them to rise.
  • Along many seacoasts there is a breeze from the sea by day. This moist, relatively cool air rises and heats as it passes across land.
  • Convectional clouds form and bring afternoon showers.
terrain factors1
Terrain Factors
  • At night the land cools and the breeze blows toward the sea.
  • Wind blowing toward land formations and condensation will occur.
  • The reverse can happen if the wind forces clouds downward into warmer air.
turbulence
Turbulence
  • Thermal Turbulence
    • Intense surface heating causes convection currents.
    • More intense convection currents occur over dark-colored ground.
    • Less convection currents will be over light-colored ground.
    • Because velocity varies turbulent conditions are expected.
turbulence1
Turbulence
  • Thermal Turbulence
    • Presents the biggest problem for aviators during landing.
    • To eliminate during normal flight, climb above clouds.
    • Not confined to summer months.
    • When cumulus clouds are present, convection currents and thermal turbulence exists.
turbulence2
Turbulence
  • Mechanical Turbulence - Low Level
    • Results from strong wind gusts over rough terrain or manmade features.
    • Produces turbulent eddies below 500 feet.
turbulence3
Turbulence
  • Mechanical Turbulence - Mountain Wave
    • Caused by wind speeds of 25 knots or stronger.
    • Produces a large-scale wave motion.
    • Extends from ground level to tropopause and 300 nmi downwind.
    • Most intense turbulence will occur within the first two or three waves.
turbulence wind shear
Turbulence - Wind Shear

VIDEO OF WIND SHEAR

turbulence4
Turbulence
  • Wind Shear - Low Level Wind Shear (LLWS)
    • Occurs below 10,000 feet.
    • Primarily caused by frontal systems, low level jet streams and thunderstorms.
    • Occurs rapidly.

http://www.pbs.org/wgbh/nova/balloon/science/jetstream.html