Exam 2 Flashcards
absorption
melting, evaporation, and sublimation
release
condensation, freezing, and deposition
calorie
heat energy needed to raise the temp of 1g of water (at 15 degree C) by 1 degree C
dew point
temp at which air will become saturated (100% RH)
the higher the water temp, the higher the dew point
cirrus clouds
Latin for “a lock of hair”
thin and wispy
made up of ice crystals instead of water droplets
forms at high altitudes
stratiform clouds
Latin for “spread out”
greyish sheets that cover most of sky, horizontal development
rarely broken up into individual cloud units
cumulus clouds
Latin for “mass” or “pile”
big and rounded, puffy
usually have a flat base and billow upward to great heights
weather
short-term (day-to-day) atmospheric conditions for a specific area, prone to great variability
climate
aggregate long-term average (30 yrs or more)
of weather conditions
air masses
distinctive bodies of air, characteristic of their source region
air masses interact to produce weather patterns
properties of air mass
- large (diameter > 1600km/1000mi, several km tall/deep)
- uniform horizontal properties
- consistent w/ surface properties (land or sea) from where they originate
- distinct from surrounding air; travels as one, but migrates w/ general circulation
- migrates into areas and displaces air collides w/ it
convergent lifting
low pressure
convectional lifting
local heating
orographic lifting
forced over a barrier
frontal lifting
collision of air masses
storms (severe)
cold front (cold air advancing)
cold dense air forces lighter warm air aloft
400km wide
squall
high intensity, short duration precipitation
warm front (warm air advancing)
warm air moves up and over dense cold air
1000km wide
fog and overcast, drizzly clouds
low cloud ceilings/visibilities
tornado watch
conditions are right for a tornado to occur
tornado warning
tornado sighted or observed on radar
relative humidity
actual vapor pressure divided by saturation vapor pressure (x100) (%)
drier air = lower RH
wetter air = higher RH
given single parcel of air, RH is inversely related to temp
- as temp rises, RH falls
air parcel
bodies of air w/ a specific temp and humidity
more buoyantly up or down
pushed along by prevailing winds, from HP to LP
stability
tendency of an air parcel to remain in place
- stable air resist displacement
- unstable air rises until it reaches a similar air pressure
adiabatic processes: cooling by expansion
air parcel cools internally as it expands under lower air pressure
from earth’s surface up
adiabatic processes: heating by compression
air parcel heats internally as it is compressed by higher air pressure
water makes up what % of the surface area of the planet
70%
duration of water cycle
~ 8-10 days
early earth outgassing
how earth got its water
volcanic outgassing