3. Water In The Atmosphere Flashcards
evaporation
change in the state of water from liquid to gas
condensation
change in the state of water from gas to liquid
hydrologic cycle
movement of water within the atmosphere, biosphere, lithosphere, and hydrosphere
transpiration
loss of water to the atmosphere by plants
hydrogen bond
bond between water molecules that results from the attraction between one water molecule’s positive end and another’s negative end
latent heat
energy that is absorbed or released during a change in the state of a substance, such as during evaporation or condensation of water
saturation
point at which an air parcel’s water vapor content is equal to its water vapor capacity
humidity
the amount of water vapor in the atmosphere
evapotranspiration
combined processes of evaporation and transpiration
hygrometer
instrument used to measure humidity
vapor pressure
portion of air pressure exerted exclusively by molecules of water vapour
millibar (mb)
measure of atmospheric pressure; average sea level pressure is 1013.25 mb
saturation vapor pressure
vapor pressure at which saturation occurs
specific humidity
water vapor content of the atmosphere, expressed in grams of water per kilogram of air (g/kg)
relative humidity (RH)
ratio of water vapour content to water vapour capacity, expressed as a percentage
air parcel
body of air of uniform humidity and temperature
dew point
temperature at which air becomes saturated
adiabatic cooling
cooling of an air parcel through expansion
adiabatic warming
warming of an air parcel through compression
dry adiabatic rate
rate of temperature change in an unsaturated parcel of air; 10°C/1, 000 m
lifting condensation level (LCL)
altitude at which an air parcel becomes saturated
moist adiabatic rate
rate of cooling in a saturated air parcel; usually about 6°C/ 1, 000m
stable atmosphere
condition in which air parcels are cooler and denser than the surrounding air and will not rise unless forced to do so
unstable atmosphere
condition in which air parcels rise on their own because they are warmer and less dense than the surrounding air