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Oceanography
Oceanography Chp 5
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Cards (15)
Lower
atmosphere
Evenly
mixed
Predominantly
nitrogen
and
oxygen
Air
has mass
Formation of steam fog
1.
Evaporation
of
water vapor
2.
Saturation
point reached
3.
Condenses
into
fog
Atmospheric
circulation
Solar energy
reaching earth depends on angle of sun, latitude, season,
transparency
of atmosphere, reflectivity of surface
Heat balance
Net radiation is the balance between
incoming shortwave
and
outgoing longwave radiation
Uneven solar heating
Drives global
circulation
of air
Rotation of
Earth
Drives global
circulation
of air
Coriolis effect
Deflects anything that flies or flows across Earth's surface from a straight path
Right in Northern Hemisphere (counterclockwise)
Left in Southern Hemisphere (clockwise)
Coriolis effect and atmospheric cells
1.
Warm
air rises at equator
2. Loses
moisture
through rainfall
3.
1/3
away from equator air becomes
dense
4. Falls back toward surface
5. Deflected right in northern hemisphere and left in southern hemisphere
Atmospheric circulation cells
Hadley
cells (trade winds)
Ferrel
cells (westerlies)
Polar
cells (polar easterlies)
Wind patterns
Doldrums
Intertropical Convergence Zone
Subtropical High
Trade winds
Daytime patterns
Nighttime
patterns
Storms
Regional
atmospheric disturbances with strong winds and
rain
Cyclones are huge
rotating
masses of
low
pressure air
Tornado
is a smaller funnel of fast-spinning wind associated with severe
thunderstorms
Air masses
Large body of air with uniform temperature, humidity, and density
Formation of extratropical cyclone
1. 2 contrasting air masses
2. Rotates counterclockwise in northern
hemisphere
3. Move eastward
Tropical cyclones
Great masses of
warm
, humid rotating
air
At least
74
miles per hour
Sea surface temperatures at least
26
degrees celsius
Counterclockwise in
Northern
Hemisphere and clockwise in
Southern
Hemisphere
Hurricanes-Atlantic
Typhoon-Eastern
Pacific
Cyclones-Western
Pacific
/
Indian
Ocean