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@ECMWFNEWS!
Updated recommended software versions and information on test data from release candidate added
Specific information on new CAPE and CIN parameters published
A webinar giving an updated overview of Cycle 47r3 with a focus on the scientific developments, the meteorological impact and new products has been scheduled for
13 September 2021, 15:00 UTC
To join please register on the event page.Changes to the grid descriptions of analysis parameters ci and sst
- Implementation moved to 12 October
- Beta test data available now
Recording and slides of the webinar Cycle 47r3 overview and more information on the meteorological impact are now available.
IFS Cycle 47r3 content and implementation timeline announced. The new cycle will be introduced in a first webinar on
6 July 2021 at 8:00 UTC: Join the webinar on Zoom
A recording of the webinar will be made available after the event
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Timeline of the implementation
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Meteorological content
Assimilation
- New RTTOV coefficients for hyperspectral infrared (IR) sounders
- New height reassignment for low level AMVs
- Add representativeness error in the total observation error for Aeolus
- Weak-constraint 4D-Var active in the stratosphere for the EDA system
Observations
- Assimilation of all-sky AMSU-A
Model
- A more consistent formulation of boundary layer turbulence, shallow convection and sub-grid cloud including:
- Simplified and more consistent treatment of sub-grid cloud saturation adjustment
- Consistent treatment of subgrid cloud from boundary layer turbulent mixing without separate statistical cloud scheme
- Consistent computation of mixing height for unstable turbulent boundary layer and convection scheme
- Change from double to single iteration of turbulent mixing scheme
- New method for computing inversion strength based on moist entropy for distinguishing stratocumulus and cumulus cloud
- Limit to convective overshoot based on tropopause stability
- New parametrized deep convection closure with an additional dependence on total advective moisture convergence
- Change from exponential-exponential cloud vertical overlap to random-exponential overlap in closer agreement with observations
- Include vapour deposition process for growth of falling snow particles
- Change from linear to cubic interpolation for cloud liquid, ice, rain and snow semi-Lagrangian departure point calculations, including 3D quasi-monotone limiter
- Interpolation of cloud and precipitation to radiation grid changed from in-cloud to grid-mean
- Inclusion of full supersaturation adjustment in the ensemble SPPT stochastic perturbations
- Mass-weighting and relaxation timescale introduced for ensemble SPPT stochastic perturbations
- Revised simplified moist physics and associated tangent-linear and adjoint
- Bug fix for vertical interpolation of 3D aerosol climatology
- Improved calculation of extinction coefficients for near-surface visibility in fog, rain and snow
- Revised gustiness parametrization
- Improved calculation of the peak wave period for multi-peaked ocean wave spectra
Meteorological impact
2For more details see 47r3 new parameters: CAPE and CIN
Changes to existing GRIB parameters
In Cycle 47r3 the grid descriptions for the surface fields ci and sst in the analysis are now identical to those of the land-sea mask (lsm).
Section 2
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Technical content
Changes to GRIB encoding
The GRIB model identifiers (generating process identification number) for cycle 47r3 1Section 4
Octets
For all parameters in GRIB 2 the Master Tables Version Number will be changed as follows:
Section 1
Octets
David Duncan et al., Assimilation of AMSU-A in all-sky conditions. EUMETSAT/ECMWF Fellowship Programme Research Report, in preparation, 2021