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Description of the upgrade

Cycle 36r4 included a new cloud parametrization scheme and new surface analysis schemes for snow and soil moisture.

Implemented: 09 November 2010  

Datasets affected

  • HRES
  • ENS

Resolution

Unchanged

HorizontalVertical

Horizontal (unchanged)
  • Atmospheric
    • HRES: TL1279
    • ENS: Leg A TL399
  • Wave
    • HRES: 0.36 degrees
    • ENS: 0.5 degrees
    • LAW: 0.1 degrees

Vertical (unchanged)
  • Atmospheric
    • HRES: L91
    • ENS: L62

Meteorological content

  • Five-species prognostic microphysics scheme, introducing cloud rain water content, and cloud ice water content as new model variables.
  • Retuning and simplification of convective entrainment/detrainment and land/sea dependent threshold for precipitation
  • Retuning of subgrid-scale orographic gravity wave drag
  • Adjustment to diffusion in stable boundary Iayers near the surface
  • All-sky improvements of microwave radiance assimilation
  • Adaptation to neutral wind of the observation operator for scatterometer data
  • New soil-moisture analysis scheme (SEKF, simplified ensemble Kalman filter)
  • New snow analysis based on 0I (Optimum Interpolation), and upgrade of NESDIS snow cover data to 4 km resolution.
  • Monthly varying climatology of leaf area index (LAI) based on MODIS data
  • The 4D-Var of the Early Delivery suite performs 2 rather than 3 updates of the outer loop
ENS
  • Revision of stochastically perturbed physical tendencies
  • Introduction of spectral stochastic backscatter scheme
  • Retuned initial perturbation amplitudes

Meteorological impact

  • Benefit in terms of objective scores in the medium range in both hemispheres, particularly in the upper troposphere.
  • positive verification for winds against observations, whereas verification against analyses tends to be negative in the shorter range, which can be explained by higher variability in the analysed wind fields.
  • improved snow analysis issues that affected the analysed snow depth on the 2009/2010 winter
  • modifications to the stable boundary layer improve the diurnal cycle of 2m temperature, especially some reduction of the night-time cold bias over Europe
  • improved tropospheric humidity analysis
ENS
  • improved probabilistic scores in the extra-tropics
  • better tuned spread-skill relationship - especially for 500 hPa geopotential height in the earlier forecast ranges (days 1-5)

New and changed parameters

New parameters

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Resources

ECMWF Newsletter: See Newsletter 126

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