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IMPROVED RAINFALL RATES FROM POLARISATION RADAR

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... but as rain gets heavier the mean size of the drops increase. ... Zdr = 10 log(Zh/Zv) gives us drop shape and hence size, D. Suppose Z is constant. ... – PowerPoint PPT presentation

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Title: IMPROVED RAINFALL RATES FROM POLARISATION RADAR


1
IMPROVED RAINFALL RATES FROM POLARISATION
RADAR IS THE EXTRA INFORMATION FROM ZDR REAL?
Anthony Illingworth, IAC, Exeter, 7 April 2004
ZDR
Z
2
Simple Z-R relationship
  • Z 200R1.6
  • This is equivalent to assuming constant drop
    concentration, but as rain gets heavier the mean
    size of the drops increase.
  • In fact drop concentrations do change so the
    sinple Z-R relationship is in error.
  • Z ND 6 R N D 3.67

3
Z and Zdr give us N and D
  • Zdr 10 log(Zh/Zv) gives us drop shape and hence
    size, D.
  • Suppose Z is constant.
  • N higher than normal, so drops smaller, Zdr below
    normal, so R higher than normal for this Z
  • N lower than normal, so drops larger, Zdr higher
    than normal and so R lower than normal for this Z.

4
PLOT OF Z AND ZDR AT EACH GATE FOR PPI
Black line const N Z 200 R1.6 Is spread
around line due to changes in drop spectra? Red
line is for 1mm/hr, What is R for each Z/Zdr? Z
and R both scale with N, So if Z is xdB gtred
line Then R is xdB gt1mm/hr.
High N
x
x
Low N
5
FOR A GIVEN Z WE OBSERVE A SPREAD OF ZDR IS
THIS REAL INFORMATION ON DROP SPECTRA?
  • NATURAL CHANGES IN ZdR DUE TO CHANGES IN DROP
    SPECTRA ARE QUITE SMALL
  • Zdr IS QUITE DIFFICULT TO MEASURE.
  • Any imperfections in our system (e.g. antenna)
    could lead to an artificial spread in values of
    Zdr for a given Z.
  • If this is so, then using Z and Zdr may give
    worse values of of R than from Z alone.

6
FOR EACH 5dB SPREAD IN Z, CALC R FOR ALL THE
Z/ZDR POINT, FIND MEAN SPREAD OF R
e.g. Z from 35 to 40dBZ 14,000 data
points Average R 10.8mm/hr Average fractional
change for each point ? 38. i.e average R error
from Z alone is 38, use of Zdr reduces this.
High N
Low N
7
IS THIS ZdR SPREAD REAL OR INSTRUMENTAL??
Lee and Zawadski calculate Z and R from use one
minute observed spectra. For given Z individual
spectra have an R 32 different from average R
for that Z. For Chilbolton data the average
spead or R for a given Z for this scane is Z
from 20-25dBZ 1mm/hr 35 to 40dBZ
25-30dBZ 2.5mm/hr ?36
30-35dBZ 5.1mm/hr ?36 35-40dBZ
10.8mm/hr ?38 40-45dBZ 26.6mm/hr ?29
45-50dBZ 50.9mm/hr ?
26 CONSISTENT WITH DISDROMETER
Quality check for data is Zdr spread correct?
8
Conclusion
  • A study of the observed spread of Z and ZDR at
    each gate from the new Kent radar would provide a
    useful check on the data quality.
  • It would confirm if the values of ZDR being
    measured reflect the true variability in mean
    raindrop size or are artificially broadened by
    some radar instrumental artefact.
  • This should be done as soon as data in rainfall
    is available.
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