3.5
4.5
5.5
6.5
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Noctilucent clouds, a "D" layer, and excellent flying conditions.
A constantly warming temperature, mother-of-pearl clouds, and generally poor flying weather.
A maximum temperature of 7°C, the strongest concentration of ozone, dense cirrus clouds, and occasionally poor flying conditions.
A temperature that remains isothermal to about 100,000 feet, the strongest concentration of ozone, and excellent flying conditions.
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Ozone gas
Argon gas
Carbon dioxide
Gaseous nitrogen
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It absorbs ultraviolet radiation.
The most the air can hold is 6 percent.
The more water vapor, the lighter the air will be.
It keeps the earth from becoming too hot by absorbing solar radiation.
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Direct solar radiation
Atmospheric scattering
Reradiated energy from the earth's surface
Reradiated energy from clouds and other atmospheric components
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Oxygen and ozone
Ozone and water vapor
Oxygen and water vapor
Ozone and carbon dioxide
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Short-wave radiation is reflected by atmospheric particles larger than .5 microns.
Short-wave radiation is reflected by atmospheric particles smaller than .5 microns.
Long-wave radiation is reflected by atmospheric particles larger than .5 microns.
Long-wave radiation is reflected by atmospheric particles smaller than .5 microns.
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Unequal heating of the earth.
Rotation of the earth.
Hadley cell.
Polar cell.
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Subtropical, Hadley, and Ferrel.
Polar, subtropical, and Hadley.
Subtropical, polar, and Ferrel.
Polar, Hadley, and Ferrel.
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Inertia.
Coriolis.
Centrifugal.
Centripetal.
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Mass.
Centripetal force.
The speed of rotation.
The radius of rotation.
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The cyclonic rotation of the earth.
The anticyclonic rotation of the earth.
An opposing force to pressure gradient.
An apparent force and therefore, it does not exist.
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To the right.
To the left.
Downward.
Upward.
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Gravity.
Coriolis.
Centrifugal.
Pressure gradient.
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Pressure gradient force and centrifugal force.
Pressure gradient force and coriolis force.
Coriolis force and centrifugal force.
Coriolis force and friction.
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Balances against friction and coriolis forces
And friction balances against centrifugal forces.
Balances against coriolis and centrifugal forces.
And centrifugal balances against coriolis force.
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Balanced against friction and coriolis forces.
And friction balanced against centrifugal forces.
Balanced against coriolis and centrifugal forces.
And centrifugal balanced against coriolis forces.
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Icelandic and Asiatic lows.
Icelandic and Aleutian lows.
Aleutian and Asiatic lows.
The Aleutian lows.
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Above the strongest horizontal shear.
Below the strongest horizontal shear.
Above the jet core.
Below the jet core.
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Above the jet core.
North of the jet core.
South of the jet core.
At the jet core's narrowest horizontal point
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Locate the 500 millibar maximum wind band.
Locate the position of the -11° Centigrade isotherm
Locate the position of the -17° Centigrade isotherm
Find where the thermal concentration is more than 5° Centigrade in 200 miles.
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Width of the 500 millibar isotherm ribbon.
Width of the 500 millibar maximum wind band.
Distance between the -17° Centigrade and the -20° Centigrade isotherms at 500 millibar.
Distance between the -20° Centigrade and the -26° Centigrade isotherms at 500 millibar.
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A decrease in the horizontal temperature contrast.
The jet axis entering into a subgradient wind field.
The conservation of angular momentum.
Coriolis force.
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Tropical jet.
Subtropical jet.
Polar-front jet.
Midlatitude jet.
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Often develop more than 400 miles apart.
Suggest that the jet stream is beginning to dissipate.
Are somewhat rare and usually occur either singly or in pairs.
Are formed during periods when the jet stream is well organized and the core exceeds 100kts.
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Decrease in amplitude.
Increase in amplitude.
Deflect towards lower heights.
Deflect towards greater heights.
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300 miles
400 miles
500 miles
600 miles
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300 miles
400 miles
500 miles
600 miles
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Move rapidly northward.
Move rapidly southward.
Intensify and move slowly eastward.
Dissipate and a new jet forms to the north.
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The wave length at which maximum energy is emitted is directly prportional to the object's temperature.
The wave length at which maximum energy is emitted is inversely proportional to the object's temperature.
An object's temperature is directly proportional to its maximum absorption wavelength.
An object's temperature is inversely proportional to its maximum absorption wavelength.
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Radiation.
Advection.
Convection.
Conduction.
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Radiation.
Advection.
Convection.
Conduction.
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By electromagnetic waves.
Horizontally by the wind.
Vertically by the wind.
By molecular motion.
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Uniform surface, stagnant air, and large-scale difluent flow.
Must be over water, stagnant air, and large-scale difluent flow.
Any nonuniform surface, stagnant air, and large-scale difluent flow.
Must be over smooth land, stagnant air, and large-scale difluent flow.
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Loss of heat by radiation.
Loss of heat by conduction.
Transport of heat by turbulence.
Transport of heat by evaporation.
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Air mass and the source region surface.
Upper- and lower-level air, and source region.
Air mass and the surface over which it is traveling.
Air-mass source region surface and the surface over which the air mass is traveling.
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MAws.
MAks.
CAwu.
CAks.
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MTwu.
MTws.
MTku.
MTks.
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CPks.
CPws.
CTws.
CTku.
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MTk.
MPw.
CPk.
CT.
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Radiation loss, thermodynamics, advection, and mechanical mixing.
Surface pressure, surface temperature, clouds, and precipitation.
Altitude, ocean currents, vegetation, and thermodynamics.
Topography, radiation loss, and mean circulation.
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Hail.
Heavy snow.
Thunderstorms.
Freezing precipitation.
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MP
CP
MT
CT
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Intensify over the heated land and the cP source regions move farther south.
Intensify over the heated land and the cP source regions move farther north.
Dissipate over the heated land and the cP source regions move farther south.
Dissipate over the heated land and the cP source regions move farther north.
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Thermal lows.
Thermal highs.
Migratory lows.
Migratory highs.
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Temperature differences between the new surface and the air mass, and the speed with which the air mass travels.
Initial characteristics of the air mass, the speed with which the air mass travels, and amount of moisture in the air mass.
Initial characteristics of the air mass, the speed with which the air mass travels, and the temperature difference between the new surface and the air mass.
Temperature differences between the new surface and the air mass, the nature of the surface over which it moves, and the speed with which the air mass travels.
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Wind speed and moisture content.
Effects of local topography and moisture content.
Wind speed and proximity to a zone of divergence.
Effects of local topography and proximity to a zone of convergence.
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Mass changes in the upper troposphere.
The jetstream pattern in the upper troposphere.
Temperature advection in the middle troposphere.
Positive vorticity advection in the lower troposphere.
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Cause the surface pressure to rise.
Increase the mass in the vertical column above the surface.
Increase the vertical extent of the column above the surface.
Vertically contract the original column of air and then expand it horizontally.
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And vertical expansion.
Contraction and vertical expansion.
Expansion and vertical contraction.
Contraction and vertical contraction.
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