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Doppler Radar Information and Definitions
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The NEXRAD WSR-88D Radar is one of
the most advanced operational weather
radar in the world. It gives meteorologists and the general public the
ability to see "inside" a storm. Using the NEXRAD radar, forecasters can
predict the weather with the aid of data such as reflectivity, velocity,
and spectrum width of an atmospheric disturbance. Since this data was
unavailable in the past, the WSR88-d NEXRAD system has the capability to save more
lives than radars of the past. For full technical details on the NEXRAD Radar
system, visit NOAA's
Radar Operation Center.
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What is and why does APRSFL use Level II Radar Data?
There are two different sets of data that NEXRAD sites put out. One is
named NIDS and one is named Level II data. There are many
advantages to Level II produced radar images. Level II, for example, are
shown with 128 colors instead of 15 providing more detail in intensity.
This allows the ability to delineate certain phenomena (e.g. gust fronts,
hook echoes) that are sometimes hard to see using NIDS data. The Level II data
is available in 0.5 dBZ increments, while NIDS reflectivity data is only
available in 5.0 dBZ increments. This lower precision in the NIDS data
causes large errors in any estimates of precipitation and precipitation
rate. There are many other differences, but for this brief explaination,
it is clear why we use Level II data to render the images you see.
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Base Reflectivity, Base Velocity & Spectrum Width
Base Reflectivity is one of the basic quantities
that Doppler radar measures. Color intensity corresponds to the
amount of radiation that is scattered or reflected back to the radar by
whatever targets are located in the radar beam at a given location. These
targets can be hydrometeors (snow, rain drops, hail, cloud drops or ice
particles) or other targets (dust, smoke, birds, airplanes, insects).
Base Velocity is the average radial velocity
of the targets in the radar beam at a given location. Radial
velocity is the relationship between the target's motion and the direction
of the radar beam. Positive values (warm colors) denote
out-bound velocities that are moving away from the radar. Negative
values (cool colors) are in-bound velocities that are moving towards the
radar.
Base Spectrum Width is a measure of velocity
dispersion within the radar sample volume. The primary use of this product
is to estimate turbulence associated with mesocyclones and boundaries.
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The parabolic reflector inside the radome
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Since this is primarily an Amateur Radio site, you have to see this!
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Here's some of the specifications for the WSR88D....
The inside of the Kylstron transmitter cabinet
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Transmitter Type: S-band, klystron tube
Amplifier (53 dB gain typical)
Frequency: 2700 to 3000 MHz
Power: 750 kw peak at klystron output
Transmitter to antenna loss: 2 dB typical
Average Power: 300 to 1300 watts
Antenna Type: center fed paraboloid
Antenna Size: 28 feet in diameter
Polarization: linear horizontal
Gain at 2850 MHz: 45.5 dB (including radome loss)
Beamwidth at 2850 MHz: 0.925 deg
First sidelobe: -29 dB (others less than -40 dB beyond 10 deg)
Radome: fiberglass foam sandwich frequency tuned, 39 foot truncated sphere
Radome two way loss: 0.24 dB at 2850 MHz
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Photos taken during a tour of a WSR-88d site back in 2005...
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aprsfl.net © 2003-2012 Dave Anderson KG4YZY & Sean Fleeman N4SCF
Your IP Address: 38.107.179.228
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