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36 Cards in this Set

  • Front
  • Back

Properties of water

most common molecule on surface of earth


liquid is non-compressible


has magnetic polarity: H+ O-


sticks to itself:hydrogen bond


dissolves polar molecules (salts, etc)

Solid is less dense than liquid

ice floats, oceans do not freeze solid; fish survive winter


weathering of rock due to expansion of ice

energy transfer occurs during phase changes


(solid-liquid-gas)

you must add energy to melt or evaporate water;


you must remove energy to condense or freeze it


H2o is constantly changing phase at the boundaries between liquid and gas


'boiling': when water vapor forms bubbles in water

water is found

ocean: 97% of all water


freshwater: 3% of all water


ice: 77% of all fresh water


groundwater: 22% of all freshwater


atmosphere: 0.03% of all freshwater

humidity

as air temp increases, evaporation increases &condensation decreases


liquid water will evaporate until the air above it is 'saturated'

At saturation

the process of evaporation and condensation are in balance

relative humidity

expressed as a %; changes as temp changes

specific humidity

does not change with temp change. often expressed in g/kg

dewpoint

another way to express specific humidity; as a temperature

humid air

less dense than dry air: compare molecular weight of h2o, n2 &o2

Orographic lifting

prevailing winds meet a mountain range and are forced upwards


one side of the mountain is rainy where air moves upwards

rainshadow effect

the leeward side (downwind side) of the mountain is dry: air moves down the mountains


one side is wet, the other dry because of westerlie winds

frontal lifting

a cold air mass moves forward and creates a cold front


cold front lifts air upwards to form strong thunderstorms

cyclonic lifting

low pressure: rising air


high pressure: sinking air

cyclone

low pressure, NH: CCW, SH: CW, rising air, cloudy/rainy skies

anticyclone

high pressure, NH:CW, SH:CCW, sinking air, clear skies

humidity

as air temp rises it's capacity to hold water vapor increases


imagine air as a container that becomes larger as it warms

the dew point

the temp at which condensation and evaporation occur at the same rate

relative humidity

as temperature increases relative humidity decreases

specific humidity

as temperature increases specific humidity stays the same

air masses and anticyclones

homogenous air masses form underneath high pressure system (anticyclone)

air masses have two important qualities

moisture content and tempertaure

moisture content

dry: 'c' for continental


moist: 'm' for maritime (form over ocean)

temperature

warm: 'T' for Tropical


cool: 'P' for Polar

mT

maritime Tropical: responsible for our hot, humid summers

cP

continental Polar: responsible for cold, dry air in winter

mP

maritime Polar

cT

continental Tropical

Warm Front

warm air moving forward


warm air pushes ahead and over cold air


warm front moves slowly


cirrus, then altostratus, then stratus


small raindrops, mist, sprinkle,; may last for a day or so

Cold front

Cold air moving forward


cold air stays low and pushes warm air out of the way and upwards


cold front moves quickly, and is not very wide; will pass in only an hour


cumulonimbus clouds


thunderstorms; heavy downpours, large rain, short duration

Stationary front

cold air mass and warm air mass at a relative standstill

Occluded Front

Cold front catches up to warm front in a mid-latitude cyclone


combination of warm front and cold front


associated with heavy rain and long duration

cyclogenesis

the lifecycle of a mid latitude cyclone


a low pressure system: CCW rotation in NH; CW rotation in SH


storm tracks: system tends to move with the westerlies


rising air--> rain; associated with warm and cold front

Hurricanes form by

warm water and coriolis effect


created from massive equatorial rainstorms

movement ( for atlantic hurricanes in NH)

form off the coast of africa


move towards the west and intensify


as they reach the caribbean, they get into the westerlies


take a sudden swing northwards, and then to the northeast

dangers

storm surge ( in NH: onshore winds North of storm)


winds


flooding from heavy rainfall