Meterology

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30 Terms

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Latitude

- earth's distance North or South of equator measured from the earth.

  • Runs east-west

  • positive= north

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Parallel

  • Line connecting all points along the same latitudinal angle

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Longitude: 

  • Angular distance east or west of the prime meridian measured from the center of the earth.

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Meridian

  • Line connecting all points along the same longitude

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Atmosphere

thin gaseous layer surrounding the earth

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Hydrosphere

All of the earth's water

  • Frozen portion (Cryosphere)

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Lithosphere

earth's crust and portion of upper mantle; the entire solid planet

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Biosphere

all living organisms of the earth

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Surface

AWOS/ASOS stations

ASOS measures wind levels @ 10m

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Upper air

  • Radiosondes, sensors ascend through atmosphere tethered to helium-filled balloon

  • Dropsondes, sensors dropped from aircraft

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Radar

  • detection and ranging. Ultra high frequency radio waves, reflected, emit 1000+ pulses each second.

    • Reflectivity

    • Storm relative velocity

    • velocity

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Radar Reflectivity

  • Scattered energy

  • Will also detect dust, pollution, insects, ect.

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Satellite Data

  • 2 main types

    • Geostationary (GOES), same place over equator

    • Polar Orbiters (POES), orbit from pole to pole

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Visible Imagery

  • Scattered/ reflected sunlight

  • Brightness controlled by albedo

  • Track storms, fronts

  • ONLY useful in daylight

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Infrared Imagery

  • Measures heat

  • Useful day and night

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Maps

850mb map, 700mb map, 500mb map, 300/250mb

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850mb map

shows advections of air masses

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700mb map

shows shortwaves

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500mb map,

halfway point between surface and tropopause

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300/250mb,

level of the jet stream

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3 types of balance

  • Hydrostatic

  • Geostrophic

  • Gradient

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Isopleths

connect points of equal value

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Interpolate

between stations to approximate isopleths location in all other places

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Ridge (high)

Coriolis effect may increase to counteract the PGF and centrifugal forces, causing supergeostrophic winds.

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Supergeostrophic

flow, wind faster around curved high than in a purely geostrophic (straight) environment

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Trough (low)

Centrifugal force is acting with the Coriolis force, reducing the coriolis force and causing subgeostrophic winds.

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Subgeostrophic

flow, wind slower around curved low than in a purely geostrophic (straight) environment.

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Zonal

when winds blow parallel to line of latitude (mostly east->west)

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Meridional

when winds blow parallel to meridian lines (mostly north->south)

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Mesoscale Models

runs for 3days or less