Module 2.2 METEOROLOGY: CLOUD PHYSICS Flashcards
It is the study of the physical processes
that lead to the formation, growth and precipitation of atmospheric clouds
Cloud Physics
It is a puffy thing in the sky which is a mass of water drops or ice crystals suspended in the atmosphere.
Cloud
TYPES OF CLOUDS
LOW-LEVEL CLOUDS
MIDDLE-LEVEL CLOUDS
HIGH-LEVEL CLOUDS
VERTICAL DEVELOPMENT CLOUDS
TYPES OF LOW-LEVEL CLOUDS
STRATUS
STRATOCUMULUS
CUMULUS
CUMULONIMBUS
These are the clouds that is often look like
thin, white sheets covering the whole sky.
Stratus
These are the clouds are patchy gray or
white clouds that often have dark honey-comb appearance.
Stratocumulus
These are the clouds that looks like
fluffy, white cotton balls in the sky.
Cumulus
These are the clouds that grows on hot days when warm, wet air rises very
high into the sky.
Cumulonimbus
TYPES OF MIDDLE-LEVEL CLOUDS
ALTOSTRATUS
ALTOCUMULUS
These are the gray or blue-gray clouds composed of ice crystals and water
droplets.
Altostratus
These are the clouds that have several patchy white or gray layers and seem to be made up of many small rows of fluffy ripples.
Altocumulus
TYPES OF HIGH-LEVEL CLOUDS
CIRRUS
CIRROSTRATUS
CIRROCUMULUS
These are delicate, feathery clouds that are made mostly of ice crystals.
Cirrus
These are thin, white clouds that cover the
whole sky like a veil.
Cirrostratus
These are thin, sometimes patchy, sheet-like clouds.
Cirrocumulus
TYPE OF VERTICAL DEVELOPMENT CLOUDS
NIMBOSTRATUS
These are dark, gray clouds that seem
to fade into falling rain or snow.
Nimbostratus
Cloud Formation Process in order
Evaporation
Convection
Adiabatic Cooling
Saturation
Condensation
Cloud Growth
Precipitation
These are large bodies of air with uniform
temperature and humidity characteristics, formed over source regions with similar surface properties.
Air Masses
These are boundaries between contrasting air masses with different temperature, humidity, and density properties, leading to dynamic atmospheric instability and cloud formation.
Fronts
TYPES OF FRONTS
Warm Front
Cold Front
It is when warm air advances (overpasses) and rises over cooler air, leading to gradual cloud development and precipitation.
Warm Front
Example of Warm Front (Clouds)
Altostratus
Nimbostratus
It is a type of front that has a moderate weather and precipitations are extended.
Warm Front
It is when cold air advances and displaces warm air, leading to rapid uplift, condensation, and the formation of cumulonimbus clouds and severe
weather.
Cold Front
It is a type of Front that has a severe weather resulting to thunder storms and heavy rain. Precipitations are NOT EXTENDED.
Cold Front
5 FACTORS INFLUENCING CLOUD PARTICLE SIZE & DISTRIBUTION
Temperature
Humidity
Aerosols
Vertical Motion
Atmospheric Composition/Condition
It is the behavior of the Clouds
(Atmospheric Thermodynamics, Radiation etc.)
Cloud Physics