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