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36 Cards in this Set

  • Front
  • Back

calorie

amount of heat required to raise the temperature of one gram of sea water 1 degree Celsius

latent heat

energy absorbed or released during a change in state

evaporation

liquid to gas



condensation

gas to liquid

sublimation

solid to gas without ever being a liquid

deposition

gas to solid without ever being a liquid



vapor pressure

part of the atmospheric pressure attributes to water vapor

saturation

max. quantity of water vapor that the air can hold



relative humidity

ratio of the air's water vapor content to its max capacity

dew point

temperature to which a particular parcel of air has to be cooled to reach saturation

adiabatic temperature changes

cooling or warming of air caused when air is allowed ti expand or is compressed

wet adiabatic rate

rate of adiabatic cooling or warming in saturated air (5-9 C/ 1 km altitude)

dry adiabatic rate

rate of adiabatic cooing or warming in unsaturated air (1 C/ 1km)

orographic lifting

air is forced to rise over the mountains

frontal wedging

warmer, less dense air is forced to rise over cooler, more sense air

convergence

pileup of horizontal airflow forces air upward

localized convective lifting

unequal heating of ground warms air, making it less dense, an forces it to rise bc of its increased buoyancy

rain shadow dessert

dry area on the lee side of a mountain range

front

boundary between 2 air masses having different characteristics

stable air

air that resists vertical displacement

unstable air

air that does not resist veinal displacement

absolute stability

air with a lapse rate less than the wet adiabatic rate

conditional stability

moist air with a lapse rate between the dry and wet adiabatic rate

clouds

dense concentration of suspended droplets and ice crystals

stratus

sheet or layer like clouds

cumulus

cloud masses that often have flat bases

aerosols

solid and liquid particles suspended in the atmosphere

condensation nuclei

tiny bits of particulate matter that serves as surfaces on which water vapor condenses

collision- coalescence process

large cloud droplets collide and join together to for a raindrop

Bergeron Process

supercooled water freezes on contact with freezing nuclei to from ice crystals on which water vapor deposits to from snow crystals

rain

drops of water that fall from clouds, at least at a diameter of .5 mm

snow

solid form of precipitation

sleet

frozen or semi frozen rani formed when raindrops freeze as they pass through a layer of cold air

glaze

a coating of ice on objects formed when supercooled rain freezes on contact



hail

nearly spherical ice pellets having concentric layers formed by the successive freezing of layers of water

rime

thin coating of ice on objects produced when supercooled fog droplets freeze on contact