final exam Flashcards
(102 cards)
clouds
a large aggregation of tiny moisture droplets and ice crystals suspended in air
cloud formation
warm air parcel rises and cools
once air parcel reaches dew point temp, it becomes saturated
condensation occurs around a cloud condensation nuclei
a cloud cannot form without this nuclei
a particle >10^-4mm around which condensation occurs and cloud formation begins
natural sources
meteoric dust, clay, silt, volcanic material and sea salt
anthropogenic sources
sulfur and nitrogen compounds from combustion
cloud forming processes
1.collision- coalescence
-temp in the cloud are above freezing (0 deg. C)
-water is in liquid and vapour form
heavier moisture droplets begin to fall & collide with other droplets
-the colliding droplets merge together to form large drops–> rain
2. Bergeron Ice-crystal process
-temps are below freezing
-water is in super-cooled liquid, vapour &ice forms
-air surrounding ice has lower vapour pressure than air surrounding water
-water vapour travels from high to low pressure areas (towards ice)
-water vapour freezes and ice crystal grows (accretion/riming)
cloud classification low: up to 2000m
- Stratus: uniform, featureless grey clouds (stratiform)
- Nimbostratus: grey, dark, low clouds with drizzling rain (stratiform)
- Cumulus: grow vertically, can extend into middle level, puffy, billowy flat based clouds with swelling tops, associated with fair weather (cumuliform)
- Stratocumulus: soft, grey, globular cloud masses in groups or waves (both stratiform & cumuliform)
- Cumulonimbus: dense, heavy, massive, grow vertically into higher levels, associated with thunder storms, forms anvil shape (cumuliform)
cloud classification middle: 2000m-6000m
- Altostratus: thin to think grey clouds, similar to stratus (stratiform)
- Altocumulus: globular clouds in groups or lines (cumuliform)
cloud classification high: 6000m-13000m
- Cirrus: wispy, feathery, thin, “mares’ tales” can indicated oncoming storms
Cirrostratus: (stratiform)
1. Stratiform: flat, ;layered, with horizontal development
2. Cumuliform: puffy, globular, with vertical development
Snow
precipitation falls through cold layer from cloud to ground as frozen
sleet
precipitation falls frozen though cold layer (partially) melts through warm layer
refreezes through cold layer and falls to surface as frozen precipitation
T<0 degree refreeze partially melted
T< -6 degree from >750 m, ice pellets from liquid
freezing rain
precipitation falls frozen through cold layer
T<10 deg
melts through warm layer
T>3 deg
rain falls to surface and freezes at surface
Rain
falls through frozen cold layer
melts through warm layer
precipitation falls to surface as rain
Hail
Originates in a cumulonimbus clouds
raindrops circulate between above and below freezing
Ice layer build as a result of this
ice pellets> 0.5cm fall to ground
produced during thunderstorms
largest hailstone recorded is 47cm diameter in south Dakota
goes up and down within the cloud fluctuating between warm and cold before allowing it to fall, it grows here
winter storms include combinations of
major snowfall freezing rain strong winds blowing snow extreme wind chill
types of winter storms
ice storms
snow storm Blizzards
occur in mid to high latitudes
can result in power outages, infrastructure damage, & human health impacts
ice storms
winter storm involving at least 6.4 mm accumulation of ice
occur when a layer of warm air is between 2 layers of cold air
freezing rain
snow storms
winter storms with a large accumulation of snow
blizzards
snowstorms with:
winds > 40km/h for more than 4 hours
blowing snow that reduces visibility to 400 or less
often involve large snowfall
thunderstorms
turbulent weather accompanied by: heavy precipitation lightening thunder cumulonimbus clouds can involve squall lines of: hail, strong winds, freezing ppt , tornadoes, squall line
squall line
sudden episode of high winds and thunderstorms in an area slightly ahead of an advancing cold front
occur with frequency at ITCZ (intertropical convergence zone –> low pressure band near the equator)
warms low pressure air–> air converges at surface and rises
cooling of the air resulting in condensation, hence clouds forming–> precipitation will likely occur
thunderstorm development
warm moist air rises rapidly and cools (water vapour–> water liquid= condensation)=energy is released –> local heating of the air
violent updrafts and downdraft develop
thunderstorm activity depends on
activity depends on variation of wind speed and direction (wind shear)
can produce strong winds near the ground (downbursts)
supercells
strongest type of thunderstorm
contain persistent rotating updrafts (mesocyclone)
need high wind/convection currents, warm moist air mass
lightning and thunderstorms
lightning: flashes of light caused by huge electrical discharges that superheat the air
thunder: violent expansion of heated air created by lighting which send out audible shock waves
8 million lighting strikes/day on Earth