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The ELDORADO surface radiation system

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Interpolate cloud fields at 3hrly intervals to ELDAS 0.2 grid ... Store and interpolate resulting downward LW and SW surface fluxes as best estimate ... – PowerPoint PPT presentation

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Title: The ELDORADO surface radiation system


1
The ELDORADO surface radiation system
  • Bart vd Hurk Dirk Meetschen et al
  • (see ELDAS web-page)

2
Principle
  • Generating 3-hrly LW SW surface downward
    radiative fluxes
  • ELDAS grid resolution
  • Combining METEOSAT data and RT calculations from
    the ECMWF model
  • Simplified data assimilation technique
  • Brief verification using routine SW stations in
    The Netherlands

3
ELDORADO steps (1)
  • Create initial field of cloud cover liquid
    water profile
  • Continuous simulation using LAM version of ECMWF
    model at 0.5?, started daily from interpolated
    ECMWF analysis
  • Interpolate cloud fields at 3hrly intervals to
    ELDAS 0.2? grid
  • Create METEOSAT-derived cloud cover field at
    ELDAS grid
  • METCLOCK cloud mask product
  • Cloud cover average mask of 5?3 METEOSAT pixels
    surrounding target location

4
ELDORADO steps (2)
  • Create METEOSAT net TOA SW radiation at ELDAS
    resolution
  • Sensor irradiance ? net TOA flux
  • Extra time/space/month-dependent calibration
    factor, derived from monthly averaged clear sky
    TOA SW flux generated by LAM

6UTC 9UTC 12UTC
5
ELDORADO steps (3)
  • Reshuffle model columns for relocation of
    cloudy/cloud-free atmospheric columns
  • For each target location, select model column
    with the smallest value of
  • J a distance b ?albedo c ?SWnetTOA
  • Adjust total cloud cover
  • to METCLOCK value
  • by scaling cloud
  • cover profile

MetClock obs
height
scaling factor
First guess Scaled
Cumulative cloud cover
6
ELDORADO steps (4)
  • Adjust liquid water content similarly in order to
    match SWnetTOA
  • Non-linear relation 2 iterations applied
  • Only applied to cloudy model gridpoints
  • Store and interpolate resulting downward LW and
    SW surface fluxes as best estimate
  • When either METCLOCK or SW-obs are absent use
    first guess
  • Archived METEOSAT/METCLOCK data covers only part
    of the ELDAS domain

7
Total cloud cover
8
TOA SWnet
9
Surface verification
  • ? 30 Routine stations in Netherlands
  • Only downward shortwave
  • Daily totals
  • First guess affected by erroneous daily reset to
    cloudfree conditions at 0 UTC probably little
    cloud spin-up in morning hours

10
  • Statistics
  • April/May 2000
  • this dataset
  • first guess 37 W/m2
  • ELDORADO 12 W/m2
  • Bias of ERA40 over
  • SGP ARM observations
  • (April-May 1999)
  • clear sky 31 W/m2
  • overcast 26 W/m2
  • all cond. 17 W/m2

11
Still to do
  • Further validation
  • BSRN stations (hardly available via www-service,
    but Lindenberg-data are ordered)
  • Validation plan
  • Cleaning the archive
  • Replace missing time slots by first guess
  • Fill area outside METEOSAT domain with first
    guess
  • Interpolation to ELDAS grid
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