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Description of the upgrade

Cycle upgrade 47r3 will bring improvements to the assimilation and observations usage and a significantly improved physical basis for moist processes, necessary to facilitate further development of the Integrated Forecasting System (IFS) and future application at convection-permitting resolutions.

The upgrade will bring more accurate upper air fields, particularly tropical winds, as well as precipitation in convective regimes. Several new convection-related products will be available and systematic errors are reduced for wind gusts and visibility for fog and precipitation.



Implementation scheduled for 06 UTC run on 5 Oct 2021, TBC


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#IFS47r3 #newfcsystem @ECMWF



NEWS!

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..


Timeline of the implementation

implementation-timeline-47r3

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

  • Extratropical upper-air geopotential and wind in the first few days of the forecast improved by 1-2%
  • Tropical upper-air winds throughout the medium-range improved by 1-4%
  • Tropical upper-air temperature improved in HRES, but degraded CRPS in ENS due to small (~0.2K) increase in bias. Low level temperatures (including 850hPa and 2m) temperature approximately neutral versus observations but degraded versus analysis over subtropical ocean.
  • Tropical Cyclones: Small improvement in position and central pressure absolute error
  • Improved MJO prediction and amplitude
  • More realistic precipitation PDF in strongly convective regimes
  • Increased convective precipitation (reduced dry bias) in arid regions
  • Increase in small scale structure for cloud and precipitation but total cloud cover degraded
  • Reduced biases for wind gusts and for visibility in fog, rain and snow

New and changed parameters

New parameters

The table contains the list of parameters expected to be available with the model implementation. They will be available as part of the test data.

Param IDShort NameNameunitsComponent & typeGRIB editionLevel typeMARSAdded to CatalogueecChartsDissemination
228045trppTropopause pressurePaHRES FC
2sfc(tick)(tick)TBDTBC
228020degm10l-10 degrees C isothermal level (atm)mHRES/ENS FC1sfc(tick)(tick)TBDTBC
228131u10nNeutral wind at 10 m u-componentm s-1ENS FC1sfc(tick)(tick)TBDTBC
228132v10nNeutral wind at 10 m v-componentm s-1ENS FC1sfc(tick)(tick)TBDTBC
228231mlcape50Mixed-layer CAPE in the lowest 50 hPaJ kg-1HRES/ENS FC2sfc(tick)(tick)TBDTBC
228232mlcin50Mixed-layer CIN in the lowest 50 hPaJ kg-1HRES/ENS FC2sfc(tick)(tick)TBDTBC
228233mlcape100Mixed-layer CAPE in the lowest 100 hPaJ kg-1HRES/ENS FC2sfc(tick)(tick)TBDTBC
228234mlcin100Mixed-layer CIN in the lowest 100 hPaJ kg-1HRES/ENS FC2sfc(tick)(tick)TBDTBC
228235mucapeMost-unstable CAPEJ kg-1HRES/ENS FC2sfc(tick)(tick)(tick)TBC
228237mudlpDeparture level of the most unstable parcel expressed as PressurePaHRES/ENS FC2sfc(tick)(tick)TBDTBC
260290catClear air turbulence (CAT)m2/3 s-1HRES FC2ml(tick)(tick)TBDTBC

Technical content

Changes to GRIB encoding

The GRIB model identifiers (generating process identification number) for cycle 47r3 will be changed as follows:

GRIB 1
Section 1
Octets
GRIB 2
Section 4
Octets
eccodes key ComponentModel identifier
47r2
47r3
6 14  generatingProcessIdentifierAtmospheric model152153
6 14  generatingProcessIdentifierOcean wave model117118

Software

To handle all output from Cycle 47r3 ecCodes 2.22.1 will be required. The relevant versions of Magics and Metview will be announced closer to the availability of test data.

Availability of 47r3 test data

The release candidate test data and products, which are expected to be made available in September 2021, will be generated daily, shortly behind operational high resolution and ensemble runs and based on the operational dissemination requirements. The availability of the test data does not follow any strict schedule.

Resources

Cycle 47r3 overview
Presentation slides
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