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A. Capacity B. Humidity C. Condensation D. Saturation
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A. Capacity B. Humidity C. Condensation D. Saturation
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A. Condensation B. Evaporation C. Melting D. sublimation
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A. Condensation B. Evaporation C. Melting D. sublimation
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A. Adiabatic rate B. Dew point C. Relative humidity D. Water capacity
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A. Adiabatic rate B. Dew point C. Relative humidity D. Water capacity
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A. Clouds B. Hail C. Dew D. sleet
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A. Clouds B. Hail C. Dew D. sleet
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A. Dry B. Stable C. Saturated D. unstable
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A. Dry B. Stable C. Saturated D. unstable
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A. A different composition B. At lower altitudes C. Colder D. thicker
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A. A different composition B. At lower altitudes C. Colder D. thicker
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A. Cirrus B. Nimbostratus C. Cumulus D. stratus
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A. Cirrus B. Nimbostratus C. Cumulus D. stratus
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A. Cirrus B. Nimbus C. Cumulus D. stratus
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A. Cirrus B. Nimbus C. Cumulus D. stratus
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A. Carbon dioxide B. Nitrogen C. Oxygen D. Water
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A. Carbon dioxide B. Nitrogen C. Oxygen D. Water
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A. Glaze B. Sleet C. Hail D. Snow
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A. Glaze B. Sleet C. Hail D. Snow
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A. Orographic lifting B. Frontal wedging C. Convergence D. Localized convective lifting
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A. Orographic lifting B. Frontal wedging C. Convergence D. Localized convective lifting
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A. Stratus B. Alto C. Cumulus D. nimbo
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A. Stratus B. Alto C. Cumulus D. nimbo
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A. Gets bigger B. Gets smaller C. Cools D. Warms
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A. Gets bigger B. Gets smaller C. Cools D. Warms
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A. Dry adiabatic rate B. Rate of change C. Wet adiabatic rate D. Environmental lapse rate
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A. Dry adiabatic rate B. Rate of change C. Wet adiabatic rate D. Environmental lapse rate
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A. Cumulostratus B. Cumulonimbus C. Altonimbus D. cirrus
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A. Cumulostratus B. Cumulonimbus C. Altonimbus D. cirrus
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A. Air pressure B. Convergence C. Divergence D. The Coriolis effect
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A. Air pressure B. Convergence C. Divergence D. The Coriolis effect
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A. Air masses B. Cyclones C. Anticyclones D. Jet streams
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A. Air masses B. Cyclones C. Anticyclones D. Jet streams
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A. Clouds B. Hail C. Lows D. Winds
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A. Clouds B. Hail C. Lows D. Winds
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A. Psychrometer B. Hygrometer C. Anemometer D. Barometer
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A. Psychrometer B. Hygrometer C. Anemometer D. Barometer
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A. Psychrometer B. Hygrometer C. Anemometer D. Barometer
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A. Psychrometer B. Hygrometer C. Anemometer D. Barometer
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A. Closely spaced isobars B. Widely spaced isobars C. Closely spaced isotherms D. Widely spaced isotherms
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A. Closely spaced isobars B. Widely spaced isobars C. Closely spaced isotherms D. Widely spaced isotherms
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A. Coriolis Effect B. Temperature C. Friction D. Pressure differences
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A. Coriolis Effect B. Temperature C. Friction D. Pressure differences
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A. Cyclonic currents B. Isobars C. Jet streams D. Pressure gradients
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A. Cyclonic currents B. Isobars C. Jet streams D. Pressure gradients
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A. Cloud formation B. Clear skies C. Precipitation D. Both A & B E. Both A & C
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A. Cloud formation B. Clear skies C. Precipitation D. Both A & B E. Both A & C
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A. Majority wind B. Westerlies C. Prevailing wind D. Widespread wind
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A. Majority wind B. Westerlies C. Prevailing wind D. Widespread wind
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A. Warm B. Cold C. High D. Low
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A. Warm B. Cold C. High D. Low
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A. Northern Hemisphere subpolar low B. Southern Hemisphere subpolar low C. Northern Hemisphere subtropical low D. Southern Hemisphere polar E. Tropics
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A. Northern Hemisphere subpolar low B. Southern Hemisphere subpolar low C. Northern Hemisphere subtropical low D. Southern Hemisphere polar E. Tropics
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A. Cirrus B. Cumulus C. Cumulonimbus D. Stratus
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A. Cirrus B. Cumulus C. Cumulonimbus D. Stratus
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A. Left B. Right C. Bottom D. Top
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A. Left B. Right C. Bottom D. Top
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A. Air has to have a dry adiabatic rate B. Air must be sinking C. Air must be getting warmer D. Must be saturated
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A. Air has to have a dry adiabatic rate B. Air must be sinking C. Air must be getting warmer D. Must be saturated
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