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Latitude
- earth's distance North or South of equator measured from the earth.
Runs east-west
positive= north
Parallel
Line connecting all points along the same latitudinal angle
Longitude:
Angular distance east or west of the prime meridian measured from the center of the earth.
Meridian
Line connecting all points along the same longitude
Atmosphere
thin gaseous layer surrounding the earth
Hydrosphere
All of the earth's water
Frozen portion (Cryosphere)
Lithosphere
earth's crust and portion of upper mantle; the entire solid planet
Biosphere
all living organisms of the earth
Surface
AWOS/ASOS stations
ASOS measures wind levels @ 10m
Upper air
Radiosondes, sensors ascend through atmosphere tethered to helium-filled balloon
Dropsondes, sensors dropped from aircraft
Radar
detection and ranging. Ultra high frequency radio waves, reflected, emit 1000+ pulses each second.
Reflectivity
Storm relative velocity
velocity
Radar Reflectivity
Scattered energy
Will also detect dust, pollution, insects, ect.
Satellite Data
2 main types
Geostationary (GOES), same place over equator
Polar Orbiters (POES), orbit from pole to pole
Visible Imagery
Scattered/ reflected sunlight
Brightness controlled by albedo
Track storms, fronts
ONLY useful in daylight
Infrared Imagery
Measures heat
Useful day and night
Maps
850mb map, 700mb map, 500mb map, 300/250mb
850mb map
shows advections of air masses
700mb map
shows shortwaves
500mb map,
halfway point between surface and tropopause
300/250mb,
level of the jet stream
3 types of balance
Hydrostatic
Geostrophic
Gradient
Isopleths
connect points of equal value
Interpolate
between stations to approximate isopleths location in all other places
Ridge (high)
Coriolis effect may increase to counteract the PGF and centrifugal forces, causing supergeostrophic winds.
Supergeostrophic
flow, wind faster around curved high than in a purely geostrophic (straight) environment
Trough (low)
Centrifugal force is acting with the Coriolis force, reducing the coriolis force and causing subgeostrophic winds.
Subgeostrophic
flow, wind slower around curved low than in a purely geostrophic (straight) environment.
Zonal
when winds blow parallel to line of latitude (mostly east->west)
Meridional
when winds blow parallel to meridian lines (mostly north->south)
Mesoscale Models
runs for 3days or less