Clouds And Precipitation Flashcards
Clouds with vertical development
Cumulus, cumulonimbus
Middle clouds
Altostratus, altocummulus
Between 6000 and 23000 feet
Freezing rain
Falling super cool water freezes on contact with a surface
Virga
Rainfall that does not reach the surface
Humidification
Air parcel cools to the dewpoint temperature becoming visible
Supercooled droplets
Water droplets existing at temperatures below freezing
Sinking parcel of air is _____ and _____
Commpressed, warms
Stable atmosphere
Air parcel is colder and denser than surrounding air
Sleet
Tiny pellets of Falling frozen water
Cloud fraction
Amount of cloud cover
Unstable atmosphere can be caused by?
Solar heating of surface, warm surface air moved into an area by wind, cooler air moving over a warm surface
Equilibrium of gravity
Balances the buoyant air parcel
High clouds
Cirrostratus, Cirrus, Cirrocumulus
Above 16,000 feet
Mostly ice crystals
Rain/drizzle
Falling liquid
Collision – coalescence process
The process of producing precipitation by liquid particles colliding and joining
Cloud
Visible aggregate of tiny water droplets or ice crystals suspended in the air
Hail
Pallets of falling frozen water of many sizes
Dry adiabatic rate
The rate of change of temperature in a rising or descending unsaturated air Parcel
Low clouds
Stratus, stratocumulus, nimbostratus
Surface to 6500 feet
How can an air parcel rise?
Surface heating, fronts, mountain topography
Adiabatic process
A process that takes place without a transfer of heat between the system such as an air parcel and it’s surroundings
Unstable atmosphere
Air parcel is warmer and lighter than surrounding air
Ice crystal (Bergeron) process
A process that produces precipitation which involves tiny ice crystals in a super cool cloud growing larger at the expense of the surrounding liquid droplets
When is the atmosphere most stable?
In the early morning around sunrise when the lowest surface air temperature is recorded
Precipitation
Any form of water falling to earth from the atmosphere
Second step of formation of clouds
Ascent - Air parcel rises
Coalescence
Merging of cloud droplets by collision
Fallstreaks
Ice crystals and stuff like that fall from high cirrus clouds
Orographic uplift
Forced lifting along a topographic barely
Moist adiabatic rate
The rate of change of temperature in a rising or descending saturated air parcel
First step of formation of clouds
Particulates or dirty air and or ice crystals combine with water vapor
Snow
Falling frozen ice crystals
Third step in formation of clouds
Cooling – the buoyed air parcel cools with increased height
Arising parcel of air ______ and ______
Expands and cools