Final Flashcards
covalent bond
hydrogen and oxygen share pair of electrons
hydrogen bond
slightly positive hydrogen side of one molecule is attracted to negative oxygen side of another molecule
specific heat
amount of heat required to increase temperature of given unit mass of substance by 1℃
surface tension
- At surface of water all molecules are pulled inward
- Water tends to form spherical droplets on most solid materials
latent heat
- heat energy that causes phase transitions w/o changing temperature
- released when water vapor changes into water or water changes into ice
Evaporation
water – gas
Condensation
gas – water (liquid)
Ocean water salinity
varies from 33 to 37‰ (or 3.3 to 3.7%) by weight
Saturated air
air that contains maximum possible amount of vapor at given temperature
Saturation vapor pressure
pressure exerted by vapor molecules when air is saturated w/ water vapor
Relative humidity
actual amount of water vapor in air compared w/ total amount that air could contain if saturated
Dew point
temperature at which saturation is reached
Relative Humidity (%) =
Actual Water Vapor in Air/Water Vapor Capacity x 100%
Atmospheric stability
Determining stability of air mass depends on temperature measurements
- comparison of environmental lapse rate of surrounding air, with dry adiabatic rate of rising air
- relationship of each rate describes if air is stable or unstable
Stable air:
rising air is cooler than the environmental lapse rate
Unstable air
rising air is warmer than the surrounding air
Conditional instability
release of latent heat causes rising air to become unstable
General circulation of the atmosphere
Heated air rises in tropics at ITCZ and sinks in subtropics as part of Hadley flow
Feedbacks in the Climate System
Processes that alter climate changes either by amplifying or by suppressing them
Positive feedbacks
growth or melting of glaciers
Negative feedbacks
increased evaporation during climate warming
valley
portion of terrain where drainage system is clearly established
continental divide
drainage divide on continent separating drainage basins feeding into two different oceans
infiltration rate
measure of volume of water passing into soil per unit area per unit time