Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt...

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Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really Do Have The Most Advanced TV Radar! AMS San Antonio 2007

Transcript of Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt...

Page 1: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville

James-Paul Dice Meteorologist WHNT-TVWalt Peterson Senior Atmospheric Scientist UAH

We Really Do Have The Most Advanced TV Radar!

AMS San Antonio 2007

Page 2: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

ARMOR: Advanced Radar for Meteorological and Operational Research.

• Location : Huntsville Intl. Airport• Altitude (antenna MSL): 194 m• Transmit frequency: 5625 MHz (C Band)• Peak Power: 350 kW• Pulse width: 0.8 s • Maximum PRF: 1000 s-1

• Antenna Diameter 3.7 m (12 ft CF Parabolic)• Antenna Beam width: 1.0o

• First side-lobe: -23 to -24 dB• Maximum rotation rate: 6 rpm• Transmit polarization: Simultaneous H and V, or H• Receive polarization: SIGMET dual-channel; H and V• Signal Process: SIGMET RVP/8• Variables: Z, V, W, ZDR, DP, KDP, hv, LDR

Partners: UAH, NASA, NSSTC, WHNT-TV

Deployed in Huntsville by the NWS in 1977 as a local warning radar (WSR-74C) then refurbished and upgraded to Doppler in 1991.

Radar donated to UAH in 2002 and upgraded to dual-polarimetry using the SIGMET Antenna Mounted Receiver 11/04. Renamed: ARMOR.

Page 3: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

A UNIQUE COLLABORATION

RESEARCH OPERATIONS

Page 4: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

9/23/04 WSR-74C disassembly 10/29-11/05 ARMOR Reassembly

Page 5: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

The Science behind ARMOR

Many of these slide courtesy of

Dr. Walt Peterson

Senior Atmospheric Scientist

University of Alabama Huntsville

Page 6: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

ConventionalRadar (NEXRAD)

PolarimetricRadar (ARMOR)

POLARIMETRIC RADAR?

Courtesy NSSL

Page 7: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

The Basics:

By looking at the difference between Hor. Polarized Z and

Vert. polarized Z we can determine size and shape of

hydrometeors

Page 8: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.
Page 9: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

Is it really that simple??

Page 10: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

Don’t I wish it were!

But…

Unfortunately, it isn’t!

Page 11: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

Remember when you learned storm relative velocity..VIL…ETC?

Page 12: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

Remember when you learned storm relative velocity..VIL…ETC?

Well get ready for some new terms like

Differential ReflectivityLinear Depolarization Ratio

Page 13: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

Polarimetric Variables1. Reflectivity factor Z at horizontal polarization

- Measure of size and concentration of scatters

(dominated by SIZE)

2. Differential reflectivity ZDR

- Measure of median drop diameter→ SIZE/SHAPE

- Useful for rain / hail / snow discrimination→ SIZE/SHAPE/PHASE

3. Differential phase ΦDP (Specific Differential Phase- KDP)

- Efficient for accurate rainfall estimation→ NUMBER/SHAPE

- Immune to radar miscalibration, attenuation, and partial beam blockage

4. Cross-correlation coefficient ρhv

- Indicator of mixed precipitation → SHAPE/PHASE

- Efficient for identifying nonmeteorological scatterers

Research:

NCAR, CSU, NASA, UND, DLR, BMRC, NOAA-ETL

ARMOR

Operational:

NEXRAD, TV

vs

Small ZDR Large ZDR

Page 14: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

• More accurate rainfall estimation (10-20% max accumulation error as opposed to 200-300%).

• Why? Because we collect information on drop size/shape/concentration and are able to mitigate hail contamination. (Kdp most useful!)

• Identification of precipitation types and discrimination between

meteorological and non-meteorological scatterers

• Improvement in radar data quality: Calibration is more consistent using using polarimetric variables

Advantages of Dual-Polarization Radar

vs

Small ZDR Large ZDRSmall drops Large drops

vs

Hail Rain

vs

Insects Rain

Mitigates the multiple Z-R issues! Estimating rainfall by assuming a standard drop size works, but rather poorly!

Page 15: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

• Spherical shape and tumbling of hail results in low ZDR’s (a ZDR “hole”).

• Large drop recirculation on edge of echo vault at x=25 km, z=2-3 km.

• Drop column clearly extends into sub-freezing portion of cloud- the hail process

ZDR in Range-Height mode …………..(ARMOR has this scanning capability and this mode provides an early look into the development of intense storms)

ZH

ZH

ZDR

ZDR

0 15 30 45 60

0 15 30 45 60

-1 0 1 2 3 4 5

-1 0 1 2 3 4 5

ZH

ZH

ZDR

ZDR

ZH

ZH

ZDR

ZDR

0 15 30 45 60

0 15 30 45 60

-1 0 1 2 3 4 5

-1 0 1 2 3 4 5

“ZDR Column” in developing convection

“ZDR Hole” in Hail

Page 16: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

61+ dBZ in cells: Hail or Rain?ARMOR: 1541 UTC 12/09/04

ZDR

>3.5 dB ZDR: Big rain drops or melting hail

Page 17: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.
Page 18: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

Squall Line on ARMOR from IRIS display

Page 19: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

Squall Line on ARMOR from IRIS display (velocity)

Page 20: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.
Page 21: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.
Page 22: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

The Television Side- Explaining all this to our viewers!

Page 23: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

ARMOR Operates Like No Other TV Radar

• The radar alternates between a traditional Doppler mode and a multi-elevation polarimetric scan. This flexibility means more data into our office.

• Traditional radar measurements (reflectivity and Traditional radar measurements (reflectivity and velocity) are available at all times.velocity) are available at all times.

• Radar alternates its operation between a live .5Radar alternates its operation between a live .5oo surveillance scan and a 3 elevation volumetric scan at surveillance scan and a 3 elevation volumetric scan at .7.7oo,1.3,1.3oo, and 2.0, and 2.0o. o. Other volume scans and sector Other volume scans and sector scans are easily tasked to the radar.scans are easily tasked to the radar.

• Following each volume scan, a hydrometeor Following each volume scan, a hydrometeor identification algorithm produces a product.identification algorithm produces a product.

Page 24: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.
Page 25: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

ARMOR in WHNT WX OfficeARMOR in WHNT WX Office

Sigmet IRIS Workstation

FasTrac VIPIR

Page 26: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

ARMOR and KHTX Side-by-Side Comparison December 10, 2004

Page 27: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

December 10, 2004 Hail Event

61 dBZ with VIL ~30 kg/m2

Page 28: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

-1.8 -0.9 0.1 1.0 1.9 2.9 3.6 -15 - 5 5 15 25 35 45

dBZ ZDR

ARMOR: 12/10/04 17:55:06 EL=1.3o

Rain

55+ dBZ

Hail

55+ dBZ

Rain

2 to 3.5 dB

Hail

-1 to 0.5 dB

Hail

-1.5 to 0.5 dB

Rain/Hail

-0.5 to 2 dB Rain/Hail

40-55 dBZ

Hail

50-55 dBZ

Page 29: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

Ground-truth Report of Dime-Size Hail

Owens Crossroads, Alabama.

Page 30: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

The Good

• We have the only one in TV (For a few more hours!!)

Page 31: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

The Good

• We have the only one in TV (For a few more hours!!)

• Hydro Meteor ID Really Works! (Limited evaluations so far.)

Page 32: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

The Good

• We have the only one in TV (For a few more hours!!)

• Hydro Meteor ID Really Works!

• RVP8 Processor is Big Improvement

Page 33: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

The Good• We have the only one in TV (For a few more hours!!)• Hydro Meteor ID Really Works!

• RVP8 Processor is Big Improvement

• Future Products Look Very Promising (3d Hydro ID in real time?)

Page 34: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

The Bad

•How do you explain it to viewers?(I am open to suggestions!)

•Difficult to interpret in real time. (Algorithims are the key)

•Not a turn key system..Graphics are made for science not TV.

Page 35: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

Advantages of Dual Polarization

• Improved Hail Detection (fewer false alarms)

• Hydrometeor Identification works well! (an improved algorithm now available.)

• Possible Tornado Debris Detection to Improve Warnings (close to radar)

• Greatly Improved Rainfall estimates.

Summary

Page 36: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

Internet Sites with info on Dual Polarization

Radar

http://www.nssl.noaa.gov/briefings/vol5_no3/polarimetric.html

On NSSL Web Site-by Alexander Ryzhkov

Excellent site by Kevin Scharfenberg at

http://cimms.ou.edu/~kscharf/pol/

Page 37: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.

Armor is on the Web! (Including Hydro. ID)

http://www.nsstc.uah.edu/ARMOR/webimage/

Page 38: Dan Satterfield, Chief Meteorologist WHNT-TV, Huntsville James-Paul Dice Meteorologist WHNT-TV Walt Peterson Senior Atmospheric Scientist UAH We Really.