Weather Flashcards
Humidity
Humidity is the amount of water vapor present in the air
Cumulus Cloud
Cumulus clouds are clouds which have flat bases and are often described as “puffy”, “cotton-like” or “fluffy” in appearance.
Stratus Cloud
Stratus clouds are low-level clouds characterized by horizontal layering with a uniform base, as opposed to convective or cumuliform clouds that are formed by rising thermals
Cirrus Cloud
Cirrus is a genus of atmospheric cloud generally characterized by thin, wispy strands, giving the type its name from the Latin word cirrus, meaning a ringlet or curling lock of hair.
Cumulonimbus Cloud
Cumulonimbus, from the Latin cumulus and nimbus, is a dense, towering vertical cloud associated with thunderstorms and atmospheric instability, forming from water vapor carried by powerful upward air currents.
Condensation
water that collects as droplets on a cold surface when humid air is in contact with it
Evaporation
the process of turning from liquid into vapor
Precipitation
the action or process of precipitating a substance from a solution.
Runoff
the draining away of water (or substances carried in it) from the surface of an area of land
Rain
Rain is liquid water in the form of droplets that have condensed from atmospheric water vapor and then becomes heavy enough to fall under gravity
Sleet
a form of precipitation consisting of ice pellets, often mixed with rain or snow.
Snow
ice crystals that precipitate from the atmosphere and undergo changes on the Earth’s surface.
Hail
pellets of frozen rain that fall in showers from cumulonimbus clouds.
Polar-Maritime Airmass
Maritime polar air masses are cool, moist, and unstable. Some maritime polar air masses originate as continental polar air masses over Asia and move westward over the Pacific, collecting warmth and moisture from the ocean.
Tropical-Maritime Airmass
Maritime tropical air masses originate over the warm waters of the tropics and Gulf of Mexico, where heat and moisture are transferred to the overlying air from the waters below. The northward movement of tropical air masses transports warm moist air into the United States, increasing the potential for precipitation.