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

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Presentation on theme: "1st Progress meeting ELDAS The ELDORADO surface radiation system Bart vd Hurk & Dirk Meetschen et al (see ELDAS web-page)"— Presentation transcript:

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

2 1st Progress meeting ELDAS 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 1st Progress meeting ELDAS ELDORADO steps (1) 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 2.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 1st Progress meeting ELDAS ELDORADO steps (2) 3.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 6UTC9UTC12UTC

5 1st Progress meeting ELDAS ELDORADO steps (3) 4.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  SWnet TOA 5.Adjust total cloud cover to METCLOCK value by scaling cloud cover profile Cumulative cloud cover MetClock obs First guess Scaled scaling factor height

6 1st Progress meeting ELDAS ELDORADO steps (4) 6.Adjust liquid water content similarly in order to match SWnet TOA Non-linear relation: 2 iterations applied Only applied to cloudy model gridpoints 7.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 1st Progress meeting ELDAS Total cloud cover

8 1st Progress meeting ELDAS TOA SWnet

9 1st Progress meeting ELDAS 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 1st Progress meeting ELDAS 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 1st Progress meeting ELDAS 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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