1 ground based meteorological radars presented by: david franc noaas national weather service...
TRANSCRIPT
![Page 1: 1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005](https://reader035.vdocument.in/reader035/viewer/2022062511/551540ed55034685568b4e92/html5/thumbnails/1.jpg)
1
Ground BasedMeteorological Radars
Presented By:
David Franc
NOAA’s National Weather Service
September 2005
![Page 2: 1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005](https://reader035.vdocument.in/reader035/viewer/2022062511/551540ed55034685568b4e92/html5/thumbnails/2.jpg)
2
Operational Functions Primary use is for operational
meteorology, research and navigation. Important functions include: Severe storm tracking Flash Flood Warnings Air Traffic Safety
![Page 3: 1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005](https://reader035.vdocument.in/reader035/viewer/2022062511/551540ed55034685568b4e92/html5/thumbnails/3.jpg)
3
How do Meteorological Radars impact your life? Routine weather forecasts Severe weather and flash flood warnings Aviation and maritime safety
Personal travel safety Safe, timely transport of personal and commercial
goods Agriculture – your source of food Power management Highway management Water management
![Page 4: 1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005](https://reader035.vdocument.in/reader035/viewer/2022062511/551540ed55034685568b4e92/html5/thumbnails/4.jpg)
4
Spectrum Allocations Meteorological radars operate under the
radiolocation and radionavigation services Three bands identified for ground-based
meteorological radars in the Radio Regulations 2 700-2 900 MHz: Relevant Footnote 5.423 5 600-5 650 MHz: Relevant Footnote 5.452 9 300-9 500 MHz: Relevant Footnote 5.475
![Page 5: 1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005](https://reader035.vdocument.in/reader035/viewer/2022062511/551540ed55034685568b4e92/html5/thumbnails/5.jpg)
5
Frequency Band Selection Radar range inversely proportional to
frequency Increased propagation loss for higher
frequency bands Precipitation absorption Unambiguous range-velocity product
Other considerations Spatial resolution
![Page 6: 1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005](https://reader035.vdocument.in/reader035/viewer/2022062511/551540ed55034685568b4e92/html5/thumbnails/6.jpg)
6
Propagation and Absorption Propagation losses increase as frequency
increases Radar propagation path is two way
Many meteorological radars used for precipitation estimation Cannot estimate rainfall in a storm if radar
returns are absorbed by the storm
![Page 7: 1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005](https://reader035.vdocument.in/reader035/viewer/2022062511/551540ed55034685568b4e92/html5/thumbnails/7.jpg)
7
Unambiguous Range-Velocity Doppler radar performance limited by the unambiguous
range/velocity product
Where,
Ra = Unambiguous range
Va = Unambiguous velocity
As frequency increases, the maximum range or maximum observable velocity, or both must decrease.
Technology to overcome range/velocity limitations degrade radar performance in other ways
Ra Vac8
Ra Va
![Page 8: 1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005](https://reader035.vdocument.in/reader035/viewer/2022062511/551540ed55034685568b4e92/html5/thumbnails/8.jpg)
8
Comparison of the BandsGeneral Trends:
System Cost: Highest- 2700-2900 MHz
Lowest- 9300-9500 MHz
System Complexity: Highest-2700-2900 MHz
Lowest- 9300-9500 MHz
Operating Range: ~450 km- 2700-2900 MHz
~200 km- 5600-5650 MHz
>75 km- 9300-9500 MHz
Severe Weather
Performance Rating: Highest - 2700-2900 MHz
Lowest - 9300-9500 MHz
![Page 9: 1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005](https://reader035.vdocument.in/reader035/viewer/2022062511/551540ed55034685568b4e92/html5/thumbnails/9.jpg)
9
Meteorological Radar Products Radar generates three base data products:
Reflectivity Mean Radial Velocity Spectrum Width
Base products used to produce many high level products Examples: rainfall estimates, wind shear detection,
precipitation type, aircraft icing levels…
![Page 10: 1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005](https://reader035.vdocument.in/reader035/viewer/2022062511/551540ed55034685568b4e92/html5/thumbnails/10.jpg)
10
Example of Meteorological Radar Volume Scan
![Page 11: 1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005](https://reader035.vdocument.in/reader035/viewer/2022062511/551540ed55034685568b4e92/html5/thumbnails/11.jpg)
11
Sharing Study Considerations
Antenna movement
Antenna pattern
Protection criteria
![Page 12: 1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005](https://reader035.vdocument.in/reader035/viewer/2022062511/551540ed55034685568b4e92/html5/thumbnails/12.jpg)
12
Antenna Movement Antenna moves to conduct a volume scan
Antenna will step through 2 to 10 elevations Full 360 rotation performed at each elevation
May take 10 to 15 minutes to complete entire volume scan
Dynamic simulations require much longer run times in comparison to radars rotating at a constant elevation
![Page 13: 1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005](https://reader035.vdocument.in/reader035/viewer/2022062511/551540ed55034685568b4e92/html5/thumbnails/13.jpg)
13
Antenna Patterns Pencil beam antenna pattern Standard ITU-R parabolic antenna patterns
not applicable ITU-R patterns too broad for pencil beam Typically result in over estimation of
interference
![Page 14: 1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005](https://reader035.vdocument.in/reader035/viewer/2022062511/551540ed55034685568b4e92/html5/thumbnails/14.jpg)
14
Antenna Pattern ComparisonComparison of Measured Antenna Pattern to F.1245 Calculated Pattern
(Radar G - M.1464-1)
-20
-10
0
10
20
30
40
50
-180 -160 -140 -120 -100 -80 -60 -40 -20 0 20 40 60 80 100 120 140 160 180
Offset Angle from Main Beam(degrees)
Ant
enna
Gai
n (d
Bi)
Measured
F.1245
![Page 15: 1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005](https://reader035.vdocument.in/reader035/viewer/2022062511/551540ed55034685568b4e92/html5/thumbnails/15.jpg)
15
Antenna Pattern ComparisonComparison of Measured Antenna Pattern to F.1245 Calculated Pattern
(Radar G - M.1464-1)
0
5
10
15
20
25
30
35
40
45
50
-5 -4 -3 -2 -1 0 1 2 3 4 5
Offset Angle from Main Beam (degrees)
An
tenn
a G
ain
(dB
i)
Measured
F.1245
![Page 16: 1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005](https://reader035.vdocument.in/reader035/viewer/2022062511/551540ed55034685568b4e92/html5/thumbnails/16.jpg)
16
Protection Criteria Protection criteria published in 3 ITU-R
recommendations 2700-2900 MHz: M.1464 5600-5650 MHz: M.1638 9300-9500 MHz: M.[8B.8-10GHZ]
Criteria in M.1464 based on testing Criteria in M.1638 and M.[8B.8-10GHZ]
currently based on basic radar theory
![Page 17: 1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005](https://reader035.vdocument.in/reader035/viewer/2022062511/551540ed55034685568b4e92/html5/thumbnails/17.jpg)
17
Protection Criteria (continued) Testing to determine criteria (refer to Annex 3 of
M.1464) Inject interference signal at known level relative to
radar noise floor Alternate interference free and interference- injected
volume scans Collect the radar base data products - compare
interference and interference free base data of each resolution cell
Lowest interference level causing out of spec. base data results is protection criteria.
![Page 18: 1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005](https://reader035.vdocument.in/reader035/viewer/2022062511/551540ed55034685568b4e92/html5/thumbnails/18.jpg)
18
Future Trends Sensitivity
Met radars currently process returns 3 to 6 dB below noise floor
Minimum signal to interference ratio (Smin/I) Lower memory and processing costs - radars
processing signals further below noise floor Lower usable S/N leads to lower required I/N
Phased array antennas Allow other volume scan strategies Can periodically return to an area of concern in
atmosphere during a volume scan
![Page 19: 1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005](https://reader035.vdocument.in/reader035/viewer/2022062511/551540ed55034685568b4e92/html5/thumbnails/19.jpg)
19
Future Trends (continued) Radar networks integrating radars using two or
more frequency bands Low frequency- good storm performance at long
range Higher frequency- gap filler radars where short range
(mitigating cone of silence) or high resolution performance is needed
Increased automation Mode selection Severe weather signature detection
![Page 20: 1 Ground Based Meteorological Radars Presented By: David Franc NOAAs National Weather Service September 2005](https://reader035.vdocument.in/reader035/viewer/2022062511/551540ed55034685568b4e92/html5/thumbnails/20.jpg)
20
Conclusion Meteorological radars operate differently and
produce different products than other radar types The differences need to be considered when
conducting sharing studies Limitations of physics dictate frequency band use Meteorological radars with higher sensitivity –
lead to greater interference sensitivity