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Geography exam 2 part 2

AB
D.A.R. (dry adiabatic rate)-(1)when the air is rising and the relative humanity is less than 100% (2) whenever the air is subsiding
dewcondensation onto the surface of an object that has dropped below the dew point temperature
dew point temperaturethe temp at which an air mass becomes saturated and relative humidity is 100%. At that point condensation or sublimation will occur
divergent wind circulationpressure-and-wind system where the airflow is outward away from the center, where pressure is highest
doldrumszone of low pressure and calms along the equator
doppler radaradvanced type of radar that can detect motion in storms, specifically motion toward and away from the radar signal
E.L.R. Environmental lapse ratedecrease in temperature with altitude under normal atmospheric conditions; approximately 6.5*C/1000 meters (3.6*F/1000 ft)
el ninowarm countercurrent that influences the central and eastern pacific
equatorial low/troughzone of low atmospheric pressure centered more or less over the equator where heated air is rising
evaporationliquid to gas
evapotranspirationthe loss of moisture to the atmosphere from plants, soils, and water bodys
upslope fogwhere rises up along the sides of a mountain, it cools and it cools and condences
evaporation fogwhen cold r settle over a warm body of water
radiation fogI formed when ir cools I contact with a cold ground surface
advection/California fogformed by the movement of warm moist air across a cold sea or land surface, as the air moves across that cold surface it cools, relative humidity rises, and the air condences
freezingliquid to solid
freezing rain “sleet”-condensation falling then freezing
frontal liftinghappens when warm and cold air masses meet and the warm air is forced to rise; the line of separation at the surface of the planet between warm and cold masses
occulded front- two cold air masses meet forcing all warm air upwards
stationary frontwarm and cold air masses are next to each other but neither is aggressive



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