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21 Cards in this Set

  • Front
  • Back
Precipitation Amount
Depth of Rainfall.
NOAA
National Oceanic & Atmosphere Association (public service)
N.W.R.
NOAA Weather Radio (source of weather updates)
N.W.S.
National Weather Service (source of information)
S.A.M.E.
Specific Area Message Encoding (weather watch and warning)
Doppler Effect
Motion of precipitation (speed of a pitched baseball)
Front
Air masses differ in temperature, humidity, or both.
Types of Fronts
Stationary (winds blow parallel)
Cold (dense)
Warm (light)
Air Mass
Volume of Air.
Types of Air Masses (4)
Cold & Dry
Cold & Humid
Warm & Dry
Warm & Humid
G.O.E.S.
Geostationary Operational Environmental Satellite (satellite that orbits in space)
P.O.E.S.
Polar-orbiting Operational Environmental Satellite (makes sure that the planet is continually rotating on axis).
Cloud
Intermingles with Earth's surface creating fog.
Straitiform Cloud
Horizontal layers.
Cumulus Cloud
Fair-weather (vaporize rapidly)
Cumulonimbus Cloud
Heavy rain, hail, or strong & gusty surface winds.
Climate
Weather conditions. Climatology is the study of climate.
What is the ionosphere and where is it located?
The ionosphere is the absorption of radiation. It is made of electrically charged gas particles and is located within the thermosphere.
Explain in detail about the different layers within the ionosphere.
There is a D-layer, E-layer, and F-layer. The D-layer disappears at night.
The (E)lectrical layer was discovered first by Guiglielmo Marconi. The E-layer is an electrically conducting layer.
The F-layer , during the day, splits into two layers and joins at night.
How does the density of the ionosphere change in relation to day/night?
The density of the ionosphere change in relation to day and night. This is because all layers are more dense in the daytime then become less dense at night.
How does density affect radio signals?
Density affects the radio signals because the signals only bounce off of objects. They don't combine as one.