frig Flashcards
(46 cards)
cloud shapes
cumuls
stratus
cirrus
cumulus cloud
puffy clouds with flat bases formed by convection currents or air maxes meeting
stratus clouds
flat, shapeless layers formed when air masses meet or a layer of air is pushed up the side of a mountain range. sometimes by conduction through cool ground surface (fog)
cirrus clouds
made of ice crystals which are formed when very little water vapour is in the air
rain clouds
stratus and cumulus: nimbostratus and cumulonimbus
- drops must be at least 0.5mm to fall (mist)
- rain is formed when colliding and blending together
snow
crystals in the air remain below freezing point all the way to the ground
- colder air: thin flakes
- warner air: clumpy flakes
sleet
warm near the cloud (rain) and below freezing near the ground (freezes to ice pellets)
freezing rain
when the air is warm but the ground is below freezing, rain freezes instantly after touching the ground
hail
frozen raindrops. rain is blown around into cold droplets in air and freeze
front
some between air masses
cold front
moving cold air mass overtakes warmer air mass. dense, cold air moves underneath warmer air and pushes it upward (creates cumulus clouds)
warm front
warm air mass overtakes a cooler one. warm air gently rises over top of cold air mass
stationary front
non moving cold/warm air masses meeting
occluded front
cold front catching up to a slow moving warm front and meeting with a cold front
high pressure system
air is descending, exerting pressure below it. air mass forms over ground, air cools and settles lower, causing pressure to build
low pressure system
rising air, leaving less dense air. generally smaller than a high pressure system
anticyclone
result of the coriolis effect on a high pressure cell is a clockwise rotation
cyclone
low pressure air, rotating in a counterclockwise direction
thunderstorms
formed from cumulus clouds which change into cumulonimbus clouds, only a small percentage become thunderclouds
t storm stage 1
formation of cumulus clouds which change into thunderclouds by a large amount of warm, moist air
t storm stage 2
more warm air rises into the cloud and condenses, releases latent energy which turns to thermal energy. warm air continually rises and creates an updraft. the top freezes and creates ice crystals. coalescence speeds up and rain begins. rain and cool air create a downdraft
t storm stage 3
rain and downdraft if cold air cut off the updraft of warm,moist air (source of energy). rain continues until the supply of moisture runs out
updraft
warm air moving upwards and pulling more air up
downdraft
cold air moving downwards