New interpolation formula in stable situation for the calculation of diagnostic fields at measurement height László Kullmann with supervision of Jean-Francois Geleyn, Jean-Francois Mahfouf Outline • Description and of the current diagnostic formulas – Paulson, Geleyn88, Canopy • New interpolation formula – determination of the new formula – comparison with Geleyn88 and Canopy • Application in DA – Use the new formula as the TL/AD version of Canopy • Conclusion 12-15 May 2009 ALADIN/HIRLAM WORKSHOP Description of current diagnostic schemes in SURFEX • Paulson scheme – fixed function, extrapolation from lowest model level Ts inconsistency • Geleyn88 scheme – fixed function with one parameter, interpolation between surface, lowest model level underestimation of T2m in stable situation • Canopy scheme (V. Masson) – 6 SBL levels between lowest model level & surface, solving prognostic equation (1d) with LS forcing + turbulence + drag T2m is prognostic (TL/AD problem) 12-15 May 2009 ALADIN/HIRLAM WORKSHOP New interpolation formula neutral s s* 1 z z0 H h z z z0 H L s* z z0 H s ( z ) s (0) ln z0 H stable/unstable z z0 H z h h 0 H L L z 1 ( ) ( ) d L • use prescribed function (like in Paulson scheme) • use the interpolation technique (JFG88) () contains parameter determine from s(zN) s* z N z0 H z N z0 H z0 H s ( z N ) s (0) ln h h z L L 0H s ( z N ) s (0) bn bH z z0 H h N L z h 0 H bn bH L 12-15 May 2009 L f bH , bn ALADIN/HIRLAM WORKSHOP New interpolation formula Geleyn88 function: h ( ) 1 z z z0 H z bH bn h h 0 H zN L L Gratchev et al. function (proposed for stable condition): h ( ) 1 ah 1 1 ch 2 where ah=5, ch=3 too complicated... simplified function (ch=2): z z0 H h L z h 0 H L 12-15 May 2009 h ( ) 1 ah 1 bH bn z ah e 1 ah ln 1 z N a h ALADIN/HIRLAM WORKSHOP z bH bn zN New interpolation formula (2) • The Gratchev formula for wind is too complicated use original formula which already gives good results determines the shape of the profile z [m] • New formula has a tuning parameter (ah) • Determination of ah by fitting to observations big variance: ah [2,20] use the proposed value ah=5 12-15 May 2009 ALADIN/HIRLAM WORKSHOP ah T [K] Comparison of new/old formula AROME forecast 04/12/2007-24/12/2007 only nature tile T2m RMSE T2m BIAS Canopy Geleyn88 New form. RH2m RMSE New formula gives similar results as Canopy 12-15 May 2009 ALADIN/HIRLAM WORKSHOP RH2m BIAS Tested in ALADIN (by Alena Trojakova) RMSE BIAS ah = ah = 5 ah = 3 RMSE 12-15 May 2009 ALADIN/HIRLAM WORKSHOP BIAS Testing the TL/AD of Canopy • Check if new formula is able to describe the TL of Canopy • Canopy scheme is prognostic change in TN does not cause immediate change in T2m – Checking the speed of relaxation • Offline Surfex run – random perturbation of forcing fields – keep forcing fields constant for relaxation period – surface fields are kept constant – Compare TL of new formula with the change in Canopy field: T(t2-1)-T(t1-1) – determine ah by fitting to Canopy profile 12-15 May 2009 ALADIN/HIRLAM WORKSHOP T2m New T2m RH2m wind 10m ah: fitted ah: fitted ah: fitted a h= 1 a h= 1 a h= 1 a h= a h= a h= 12-15T May 2009 Canopy 2m ALADIN/HIRLAM WORKSHOP RH Canopy 2m U10m Canopy AROME 3dVar test • Comparing results using TL/AD of old (G88) and new formula • 6h assimilation cycling • Observations: TEMP, AIREP, AMSU-A, AMSU-B, SYNOP (T2, RH2, U10) • direct obs. operator is the Canopy scheme (from guess) • Ensemble B matrix • Small differences on average, disappears after few hours 12-15 May 2009 ALADIN/HIRLAM WORKSHOP time period: 05/12/2007 – 22/12/2007 rmse T2m bias T2m ah = ah = 5 ah = 1 rmse RH2m 12-15 May 2009 ALADIN/HIRLAM WORKSHOP bias RH2m Conclusion • Determination of new interpolation formula • The new formula gives similar result as Canopy or Paulson in stable case • TL of new formula approximates well the TL of Canopy • Using TL/AD of new formula in assimilation has small impact compared to the old one 12-15 May 2009 ALADIN/HIRLAM WORKSHOP
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