Humidity Flashcards
Humidity
Saturation of air with water vapor depends on temp
Dew point
Temperature at which a parcel of air reaches saturation
Cooling air below its dew point temp typically generates dew, fog, or clouds when the dew point is above freezing and frost when it’s below freezing
Adiabatic temp changes
Occurs without the transfer of heat or mass between a system and its environment
Condensation level
Level where air parcel rises high enough that it cools to its dew point, triggering condensation
Orographic lifting
As air parcels move over land they follow the terrain
Orographic lifting occur when air is forced to rise over a mountainous barrier
Processes that lift air
Frontal lifting, in which warmer, less dense air is forced over cooler, denser air
Convergence, which is a pileup of horizontal airflow that results in upward movement
Localized convective lifting, which unequal surface heating causes localized pockets of air to rise
Clouds
Condensation occurs only when a surface exists pon which the water vapor can condense
Fog
Is defined as a cloud with its base at or very near the ground
Caused by air in contact with the ground falls below its dew point
Precipitation
Water that falls towards the ground
Wind
Result of horizontal differences in air pressure
Air flows from higher pressure to areas of lower pressure
Solar radiation is the ultimate energy source for most wind
Coriolis effect
Because the earth rotates on its axis, circulating ai is deflected toward the right in the Northern Hemisphere and toward the left in the Southern Hemisphere