Cloud Layer Overlap and the Influence of Vertical and Temporal - - PowerPoint PPT Presentation

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Cloud Layer Overlap and the Influence of Vertical and Temporal - - PowerPoint PPT Presentation

Cloud Layer Overlap and the Influence of Vertical and Temporal Resolution of Radar Data Oliver Sievers Markus Quante GKSS Research Center Institute for Coastal Research D-21502 Geesthacht Outline Cloud Layer Overlap Cloud Layer Overlap


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SLIDE 1

Cloud Layer Overlap and the Influence of Vertical and Temporal Resolution of Radar Data

Oliver Sievers Markus Quante GKSS Research Center Institute for Coastal Research D-21502 Geesthacht

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SLIDE 2

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Outline

  • Cloud Layer Overlap
  • Influence of Data Resolution
  • Radar / Ceilometer Comparison
  • Conclusions & Outlook
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SLIDE 3

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Cloud Layer Overlap: Introduction

Current Models:

  • Random Overlap
  • Maximum Overlap

) , max(

max b a c

c C =

b a b a rand

c c c c C − + =

  • > True Overlap?

Combined Cloud Cover as function

  • f level separation for all overlap

models (mean values over 30mins / 60mins)

  • Vert. cont. / non-cont. clouds
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Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Combined Cloud Cover

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SLIDE 5

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Combined Cloud Cover

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SLIDE 6

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Combined Cloud Cover

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SLIDE 7

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Combined Cloud Cover

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SLIDE 8

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Overlap Parameter α

Combined Cloud Cover not useable to describe cloud

  • verlap

Needed: Parametrisation of true overlap as function of

  • verlap models

=> Overlap Parameter α

rand true

C C C ) 1 (

max

α α − + =

α=-1 α=0 α=+1

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SLIDE 9

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Overlap Parameter α

Full Resolution (82.5 m / 5secs) 30 mins mean CC

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SLIDE 10

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Overlap Parameter α

Full Resolution (82.5 m / 5secs) 30 mins mean CC 60 mins mean CC

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SLIDE 11

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Earlier Publication

From: Hogan and Illingworth, 2000, QJR Meteorol. Soc., 126, 2903-2909 Used resolution: rough cloudmask about 2 mins / 360 m / 60 mins average

BBC: no convergence at random overlap for large level separation, exponentiell fitting is „dared“ - but full resolution!

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SLIDE 12

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Overlap Parameter α

60 mins mean CC Res: 82.5 m / 5 sec

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SLIDE 13

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Overlap Parameter α

60 mins mean CC Res: 82.5 m / 5 sec Res: 330 m / 2 min

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SLIDE 14

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Overlap Parameter α

60 mins mean CC Res: 82.5 m / 5 sec Res: 330 m / 2 min Res: Res: 330 m / 5 sec

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SLIDE 15

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Overlap Parameter α

60 mins mean CC Res: 82.5 m / 5 sec Res: 330 m / 2 min Res: 82.5 m /2 min Res:

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SLIDE 16

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Radar and Ceilometer Disagreement

Ceilometer n/a Cloud-Free Cloudy Cloud-Free 0.8 % 18.9 % 5.4 % Radar Cloudy 1.3 % 25.2 % 48.4 %

Values relative to Radar profiles (259.370)

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SLIDE 17

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Radar and Ceilometer Disagreement

Ceilometer n/a Cloud-Free Cloudy Cloud-Free 0.8 % 18.9 % 5.4 % Radar Cloudy 1.3 % 25.2 % 48.4 %

Values relative to Radar profiles (259.370)

  • Thin clouds?
  • Very low clouds?
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Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Example for thin layer

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Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Ceilometer cloud base distribution w/o radar cloud

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SLIDE 20

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Radar and Ceilometer Disagreement

Ceilometer n/a Cloud-Free Cloudy Cloud-Free 0.8 % 18.9 % 5.4 % Radar Cloudy 1.3 % 25.2 % 48.4 %

Values relative to Radar profiles (259.370)

  • Thin clouds?
  • Very low clouds?
  • ???
  • Very high (=Ice-) clouds?
  • Insects?
  • ???
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SLIDE 21

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Difficult cloud for ceilometer

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SLIDE 22

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Radar cloud base vs. thickness (w/o ceilometer)

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SLIDE 23

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Summary

  • High clouds
  • Thin clouds
  • Insects (?)
  • Overlapping of layers
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SLIDE 24

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Conclusions

  • Cloud overlap depends on used resolution
  • For vert. cont. clouds:
  • Overlap parameter decreases with level separation
  • Using full resolution, decrease is appr. linear
  • Reducing data to mean 2-minutes-value increases α
  • Reducing vert. res. to 330 m gives a exponentiell

decrease for increasing level sparation & converging at random overlap

  • Vertical non-cont. clouds are appr. random overlapped
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SLIDE 25

Oliver Sievers, CLIWA-NET-Workshop, 16.-19.12.2002, Madrid

Cloud Layer Overlap

Conclusions (cont.) & Outlook

  • Radar fails to see thin clouds
  • In boundary layer many radar signals remain (in 20% of all

cases w/o ceilometer cloud, isolated pixels in lowest range gate exist) Outlook:

  • Modify Cloudmask
  • Check Ceilometer Accuracy vs. Temperature
  • Cloud Classification