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Cloud
Aggregation of tiny water droplets and ice crystals that are suspended in air.
Clouds form:
When the air becomes saturated and the water vapor condenses or deposits onto tiny particles
Warm clouds
Form in the tropics and only have cloud droplets
Cold clouds
Form in the midlatitudes and only have ice crystals
Mixed-phase clouds
Have both cloud droplets and ice crystals
Cloud classifications is based on:
Altitude and shape
Stratiform clouds
Flat and layered clouds with horizontal development
Cumuliform clouds
Puffy and globular clouds with vertical development
Cirroform clouds
Wispy clouds are usually high in altitude and made of ice crystals
Fog
Low-lying cloud, often in contact the ground
Fog results from:
Cooling or when air becomes saturated through the addition of water vapor.
Presence of fog means:
Air temperature and the dew point temperature at ground level are the same
Radiation fog
Forms at night when Earth’s surface cools, aided by clear skies and calm winds, usually dissipates by sunrise
Advection fog
Forms when warm, moist air moves over a cold surface, causing the air to cool and become saturated, can occur with windy conditions
Evaporation fog
Forms when cold air moves over a warmer body of water, resulting in evaporation and then condensation as fog. (aka stem fog)
Upslope fog
Occurs when relatively humid air moves up a gradually sloping landform or up a mountain
Frontal fog
Formed when rain evaporates as it falls through a layer of cool air below. (Aka precipitation fog)
Cloud condensation nuclei (CCN)
Microscopic particles (aerosols) on which condensation occurs, resulting in cloud droplets.
Ice nuclei (IN)
Microscopic particles (aerosols) on which deposition occurs, resulting in ice crystals
Cloud droplets
CCN + condensed water surrounding it
Water vapor needs a __ to condense or deposit on depending on the temperature
Surface
Ice nuclei needs:
Bacteria, particles of clay and other minerals, and other compounds that mimic the hexagonal crystalline structure of ice
Mixed phase clouds contain:
Some ice crystals and more cloud droplets
Temperatures are below freezing in mixed-phase clouds, the cloud droplets are:
Supercooled
Precipitation occurs when:
Cloud droplets or ice crystals grow large enough to fall with gravity
Collision-coalescence process
for raindrops in warm clouds
Bergeron process
for snowflakes in cold clouds
Two primary mechanisms form precipitaion
Collision-coalescence process and Bergeron process
Colision-coalescence process happens mostly:
Over regions in which air is very humid and relatively clean.
Aggregation
As snowflakes fall, collide with one another and merge in the process of:
Hail
Hard rounded pellets of ice only produced in large cumulonimbus clouds