GEO CH 7 Flashcards
water and atmospheric moisture
Phase change:
when the state of matter changes to another
Why is finding pure water very rare on earth?
Water is polar, making it attract and dissolve almost any substance. So it is always mixed in with stuff and rarely actually found pure.
what is Deposition?
when water vapor attaches to ice causing frost
Sublimation
when water goes from ice to gas
what is more dense, ice or water?
Water is more dense than ice, that’s why ice floats in water
describe latent heat when water freezes and when it heats up
when water freezes it releases latent heat
when ice melts, it absorbs latent heat
Latent heat of vaporization:
540 Cal in latent heat to be absorbed to go from liquid to vapor
Latent heat of condensation:
540 Cal in latent heat released from vapor to return to liquid form
Latent heat of sublimation:
680 Cal in latent heat to go from solid to vapor
Humidity:
The amount of water vapor in the air
relative humidity:
remember it as X vs X
Vapor in cooler air
Vapor in warmer air
the amount of water vapor that’s actually in the air vs the max amount of water vapor that could possible be in the air at a certain temperature
Cooler air = less maximum amount of water vapor in the air possible
warmer air: maximum amount of water vapor in the air possible
What happens at saturation, or 100% relative humidity if extra addition of water vapor or decrease in temperature occurs?
active condensation if reduced the evaporation rate
Air can be saturated by:
1- being cooled down to dew-point temperature
2- addition of more water vapor to the air
3- mixing of both warm and cold air parcels which are both close to saturation
explain dew point temperature
The temperature at which air becomes saturated with water vapor, leading to condensation and the formation of water droplets
When does saturation occur in the air?
when dew-point temperature = air temperature
What is frost point?
when the air becomes saturated at temperatures below freezing
When is relative humidity the highest and lowest throughout the day?
It peaks at dawn, like 5-6 am, and is at its lowest in the afternoon, like 3-4 pm
Vapor pressure:
the share of air pressure that is made up of water vapor molecules
the higher the temperature = the higher the vapor pressure
hair hygrometer
simple terms: A tool used to measure relative humidity using a strand of hair.
real definition (how it works): an instrument used to measure relative humidity. It uses the principle that human hair changes as much as 4% in length between 0% and 100% relative humidity. It puts a bundle of human hair in a gauge, and shows how its length changes when humidity is absorbed or released by the hair
Sling psychrometer: (2)
1- Dry-bulb thermometer: records the surrounding air temperature
2- Wet bulb thermometer: covered by a wet cloth
They are both then waved around to see the temperature difference on both bulbs
parcel:
bubble of air of no definite size that retains its shape and general characteristics as it rises or sinks in the atmosphere
A parcel’s position is determined by 2 forces:
1- Upwards buoyance force
2- Downwards gravitational force
Buoyant force:
The parcel is lower density than the air surrounding it causing it to rise.
downwards gravitational force
If the parcel is higher density than the air surrounding it then it sinks/descends
define stability of parcels:
It is when a parcel remains in place, or changes its vertical position by rising or falling.
What causes a parcel to be unstable
When it reaches an altitude where the surrounding air is similar to the parcel
Dry adiabatic rate:
The rate at which “dry” air cools by expansion as it rises or heats by compression as it falls
Moist adiabatic rate
the rate at which an ascending air parcel that is moist, or saturated, cools by expansion
stratocumulus clouds:
patchy, grey, lumpy low level clouds
Altocumulus clouds
patchy rows, wave patterns, a “mackerel sky,” or lens-shaped clouds
Cirrus
feathery, hairlike fibers
What exactly is fog?
Just a cloud layer on the ground
air temp = dew point temp
Radiation fog:
formed by radioactive cooling of a land surface, especially on clear nights on areas with moist ground, when the air layer above the surface is chilled to the dew-point temperature
Rime fog:
supercooled water droplets which turn to rime frost when interacting with freezing objects
Ice crystal fog (sublimation)
when a lot of sublimation occurs, and the air is full of ice crystals
advection fog:
When air in one place migrates to another area where conditions are right for saturation.
example:
- warm moist air is moves over to cooler ocean currents which cools that air down to dew-point temperature then that causes a visible fog
Upslope fog:
when moist air is forced upwards to higher altitude, then it cools down causing a visible fog
Valley fog
fog in the valley because the cool air is less dense than the moist air causing a visible fog
Evaporation fog
water molecules evaporate from the water surface into the cold overlying air, effectively humidifying the air to saturation, followed by condensation to form fog