severe weather seminar spring 2011 [email protected]

19
Operational Use of Spectrum Width Severe Weather Seminar Spring 2011 [email protected]

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Page 1: Severe Weather Seminar Spring 2011 Pat.spoden@noaa.gov

Operational Use of Spectrum Width

Severe Weather Seminar

Spring 2011

[email protected]

Page 2: Severe Weather Seminar Spring 2011 Pat.spoden@noaa.gov

What is Spectrum Width?

• One of the 3 base moments available with WSR-88D

• Measures the variability of movement within a bin

• With super-high resolution, there is much we can see

• Not available on the web – GR software only – Color scales important, as always

Page 3: Severe Weather Seminar Spring 2011 Pat.spoden@noaa.gov

Spectrum Width

• Spectrum Width depicts a measure of velocity dispersion. It provides a measure of the variability of the mean radial velocity estimates due to wind shear, turbulence, and/or the quality of the velocity samples. It is used to estimate turbulence associated with boundaries, thunderstorms, mesocyclones.

Page 4: Severe Weather Seminar Spring 2011 Pat.spoden@noaa.gov

Spectrum Width

Low Spectrum Width High Spectrum Width

Both situations can be helpful…

Page 5: Severe Weather Seminar Spring 2011 Pat.spoden@noaa.gov

Low Spectrum Width

• Depicts a smooth flow• Supercell• May 2, 2010

Page 6: Severe Weather Seminar Spring 2011 Pat.spoden@noaa.gov

Low Spectrum Width

Low, or smoothvalues

Page 7: Severe Weather Seminar Spring 2011 Pat.spoden@noaa.gov

Low Spectrum Width

Rear FlankDowndraft

Page 8: Severe Weather Seminar Spring 2011 Pat.spoden@noaa.gov

Low Spectrum Width

Tornado is now“cutoff” and soon dissipates

Page 9: Severe Weather Seminar Spring 2011 Pat.spoden@noaa.gov

Damage Map

Tornado RFD wind damage

Page 10: Severe Weather Seminar Spring 2011 Pat.spoden@noaa.gov

High Spectrum Width

Distant Supercell

May 2, 2010

EF0 Tornado in northern Butler

Image from 10-15mintues prior to touchdown

Page 11: Severe Weather Seminar Spring 2011 Pat.spoden@noaa.gov

High Spectrum Width

Page 12: Severe Weather Seminar Spring 2011 Pat.spoden@noaa.gov

Other Uses

• TBSS – Three Body Scatter Spike

Page 13: Severe Weather Seminar Spring 2011 Pat.spoden@noaa.gov

1949 @ 9.9 (19,500 ft)

August 14, 2010

-Signature seen5-10 minutesprior to 65-70mph microburst.

Page 14: Severe Weather Seminar Spring 2011 Pat.spoden@noaa.gov

1954 Cross Section

Page 15: Severe Weather Seminar Spring 2011 Pat.spoden@noaa.gov

• It is not always clear nor easy to locate the true “leading edge.”

• Strong winds can push storms upshear which may complicate the matter

Next Question

Where is the “leading edge”

??

Page 16: Severe Weather Seminar Spring 2011 Pat.spoden@noaa.gov

• Use Spectrum Width or Velocity productSolutions

Page 17: Severe Weather Seminar Spring 2011 Pat.spoden@noaa.gov

Where is the “leading edge?”

Where you thought?

Page 18: Severe Weather Seminar Spring 2011 Pat.spoden@noaa.gov

Another way to help spot interfaces and mesovortices – use SPECTRUM WIDTH!

Page 19: Severe Weather Seminar Spring 2011 Pat.spoden@noaa.gov

Spectrum Width

• Depicts turbulence within the range bin.• Low values suggest “smooth flow”

– RFDs, inflow

• High values suggest turbulent flow– Boundaries– Potential of tornadic signatures with weak

rotation