Quality of Weather Radar Wind Profiles Iwan Holleman KNMI - PowerPoint PPT Presentation

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Quality of Weather Radar Wind Profiles Iwan Holleman KNMI

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VAD1-2: Fourier expansion of radial velocity as a function of azimuth : ... Binning of scan data in 8 azimuth sectors: neighboring empty sectors are not allowed ... – PowerPoint PPT presentation

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Title: Quality of Weather Radar Wind Profiles Iwan Holleman KNMI


1
Quality of Weather Radar Wind Profiles Iwan
Holleman (KNMI)
  • Introduction of VAD technique in early 60s
  • Development of VVP technique in late 70s
  • Strong effort in retrieval of divergence and
    other non-linear parameters
  • Hardly any comparison or verification studies
    focused on horizontal wind field
  • This study Focus on high quality and high
    availability of horizontal wind vectors

2
Velocity Azimuth Display (VAD)
ff20.4 m/s dd217 deg
3
Retrieval Techniques
  • VAD1-2 Fourier expansion of radial velocity as a
    function of azimuth
  • Vrad(?) a0/2 b1?sin? a1?cos?
  • b2?sin2? a2?cos2? ...
  • VVP1-3 Use all available volume scan data for a
    given height layer at once
  • Assumption of linear wind model at radar site
  • U(x,y,z) u0 x ?u/?x y ?u/?y (z-z0) ?u/?z
  • V(x,y,z) v0 x ?v/?x y ?v/?y (z-z0) ?v/?z
  • W(x,y,z) w0 (z-z0) ?w/?z

4
Implementation and Quality Control
  • Volume scan data are input to retrieval
    techniques
  • Application of minimum and maximum range
  • Removal of radial velocities close to zero
  • Binning of scan data in 8 azimuth sectors
    neighboring empty sectors are not allowed
  • Linear fit using Singular Value Decomposition
    (SVD)
  • VAD parameters per height layer are determined
    using weighted average
  • Removal of radial velocity outliers and re-run of
    wind model fit

5
Verification against radiosonde
std.dev. 2 m/s
  • Profiles from1 October 2001 till1 July 2002
  • 22610 profiles on 268 days

T. Andersson RMS of 3-4 m/s for VAD
6
Availability of VVP1 profiles
40
std.dev. 2 m/s
28
19
7
VVP1 versus wind speed
WMO simultaneous and within 5 km
  • WMO requirements for upper-air wind observations

8
VVP1 versus radiosonde
  • Verification of speed and direction
  • Both radiosonde and Hirlam model data as
    reference

9
VVP1 against Hirlam
10
Example of Wind Profiles
  • 6 October 2003
  • Doppler Radar and Hirlam analyses

11
Conclusions
  • VVP wind profile retrieval algorithms perform
    better than VAD algorithms
  • Most simple VVP algorithm provides highest
    quality and availability horizontal wind data
  • Availability is reasonable in boundary layer
    (?40)
  • Retrieved wind vectors meet the WMO quality
    requirements
  • Improvements for Rainbow VP2 module algorithms,
    output, and quality control

Acknowledgment Hans Beekhuis, Herman Wessels and
Sylvia Barlag
12
Profiles during Bird Migration
  • 28 October 2001
  • Doppler Radar and Hirlam analyses
  • Std.dev. 2.0 or 1.8 m/s

Birds?
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