Title: Radars
1Radars
- Sandra Cruz-Pol
- Professor
- Electrical and Computer Engineering Department
- University of Puerto Rico at Mayagüez
- CASA- Collaborative Adaptive Sensing of the
Atmosphere - 2006
2What is a Radar?Radio detection and ranging
- How does a radar work?
- Radar Concepts
- Games
3The frequency of the em wave used depends on the
application. Some frequencies travel through
clouds with virtually no attenuation. ALL em
waves move at the speed of light
4 5(No Transcript)
6Compare to Acoustic Echo-location
hello
7Acoustic Echo-location
hello
8Acoustic Echo-location
hello
distance
9Hi !!
t 2 x range / speed of sound
Example range 150 m Speed of sound 340
meters/second t 2 X 150 / 340 1 second
10RADAR Echolocation(RADAR RAdio Detection And
Ranging)Microwave Echo-Location
Tx
Rx
Microwave Transmitter
Receiver
11Target Range
Tx
Rx
time
t 2 x range / speed of light measure t, then
determine Range
Example t .001 sec Speed of light c 3x108
meters/second Range .001 x 3x108 / 2
150,000 m 150 km
12Thresholding
Threshold Voltage
time
- Measure time elapsed between transmit pulse
- and target crossing a threshold voltage.
- Then calculate range.
- Dont report back any information from targets
that - dont cross the threshold
13Range-Gating
Range Gates
time
14- We will see that Radars work by
- Transmitting microwave pulses.
- and measuring the
- Time delay (range)
- Amplitude
- Frequency
- Polarization
- of the microwave echo in each range gate
15Target Size
Scattered wave amplitude conveys size of the
scattering objects. Measure amplitude, determine
size.
time
16Target Radial Velocity
Frequency ft
Frequency ft fd
17Target Radial Velocity
Frequency ft
Frequency ft fd
18Zero Velocity for Crossing Targets
Frequency ft
Doppler Frequency
Frequency ft fd
19Target Spatial Orientation
Large Drops
Polarization Pt
Small Drops
Polarization Ps
20Example Weather Echoes
Microwave Transmitter
Receiver
21Echo versus Range(range profile)
Transmitted Pulse 1
Cloud Echo
time
22In summary, radars work by Transmitting
microwave pulses. and measuring the
of the microwave echo in each range gate
Time delay (range)
Amplitude (size)
Frequency (radial velocity)
Polarization (spatial orientation oblateness)
23Other concepts of Radars
24Colors in radar images
- The colors in radar images indicate the amount of
rain falling in a given area. - Each raindrop reflects the energy from the radar.
Therefore, the more raindrops in a certain area,
the brighter the color in the radar image of that
area. - The bright red color around the eye of a
hurricane radar image indicates the area of
heaviest rainfall. The green colored area has a
moderate amount of rain, while the blue areas
represent the least amount of rain.
Hurricane Andrew, 1992
25QPE Quantitative Precipitation Estimation
0.1 mm/hr
1 mm/hr
15 mm/hr
100 mm/hr
gt150 mm/hr
26Why Radar Can't (Usually) See Tornadoes
- The network of WSR-88D Doppler radars across the
US has certainly proven itself for the ability to
detect severe weather. Tornado warnings, in
particular, are much better now that National
Weather Service forecasters have this fantastic
new (new as of the early 1990s) tool. - But did you know that Doppler radar (usually)
can't see an actual tornado? When Doppler radar
is cited in a tornado warning it is generally
because meteorologists see evidence the storm
itself is rotating. It is a supercell
thunderstorm or at least contains an area of
rotation called a mesocyclone. - When can and when can't Doppler radar see a
tornado? It's math! Let's figure it out. We'll be
looking into two factors - 1) the first is something you learned in school a
loooong time ago - the earth is curved, and - 2) the radar "beam" is 1 degree wide.
27NEXRAD System Today
Gap
28May 3, 1999 Tornado Outbreak in Oklahoma
29NWS has 150 NEXrad radars in US1 in Cayey, PR
30Proposed CASA radar network
31CASA radars will complement NWS radars
Water spout at Mayaguez Beach, PR- Sept 2005
unseen by NEXRAD
32Radar "Beamwidth"
- The geometry of the dish and a few other factors
help determine the pulse volume, which can be
specified in degrees. - NEXRAD radar sends discrete pulses (and spends
99.57 of the time listening for return echoes) - Meteorologists like to use the convenient terms
"beam" and "beamwidth" to describe where the
radar is pointing and the effective resolution of
the air being sampled.
33Antennas
- Antenna is a transition passive device between
the air and a transmission line that is used to
transmit or receive electromagnetic waves.
34Antenna Beamwidth
radians D is the antenna
diameter ? is the wavelength of signal in air
Tradeoff Small wavelengths (high frequencies)
small antennas But small wavelengths attenuate
more
35Beamwidth Size vs. Object Size
- Beamwidth
- What can a radar see? Beamwidth is one
consideration. Earth curvature and height of the
feature is another (addressed on the next page). - For the moment, we'll keep the problem in two
dimensions and ignore height above ground. - The geometry is an isosceles triangle. Be sure to
note which beamwidth you are calculating for
(i.e. 1 degree).
36Beamwidth
0.7 mi 1.4 mi 2.1 mi 2.8 mi
37Object Size
- How wide and tall are various things we want to
see?
Width of Meteorological Objects (i.e. Storms,
Tornadoes)
38Earth Curvature
Fill in the table with values you calculate
0.17 mi 0.35 mi 0.52 mi 0.70 mi 7 mi 16 mi 23
mi 31 mi
39Play related games
40Play the games to learn the basics
- http//whyfiles.org
- http//meted.ucar.edu/hurrican/strike/index.htm
- http//meted.ucar.edu/hurrican/strike/
- http//meted.ucar.edu/hurrican/strike/info_3.htm
- http//www.nws.noaa.gov/om/hurricane/index.shtml
- http//www.nws.noaa.gov/om/edures.htm
41More Games for Kids 4-104
- http//www.nws.noaa.gov/om/reachout/kidspage.shtml
42References
- The COMET project http//www.comet.ucar.edu/
- NASA TRMM
- NCAR (National Center for Atmospheric Research) -
University Corporation for Atmospheric Research
(UCAR) - NOAA Educational Page http//www.nssl.noaa.gov/ed
u/ideas/radar.html - Dave McLaughlin Basics of Radars presentation
- NWS http//www.crh.noaa.gov/fsd/soo/doppler/doppl
er.htm