Versions Compared

Key

  • This line was added.
  • This line was removed.
  • Formatting was changed.

...

Section

Proposed resolution changes

Atmospheric model

 

 
 HRESENS
Leg ALeg B / C
 
Current
Upgrade
Current
Upgrade
Current
Upgrade
Spectral
TL1299
TCO1279
TL639
TCO639
TL319
TCO319
Gaussian grid
N640
N1280
N320
N320
N160
N320
Horizontal grid resolution
~16 km
~9 km
~30 km
~xx km
~60 km
~xx km
Dissemination (LL)
0.125
TBC
0.25
TBC
0.5
TBC

Model Level
Vertical resolution

137
137
91
91
91
91
  • There will be no change in the number and definition of the pressure levels.
  • The horizontal resolution of the ENS re-forecasts will be increased to match that of ENS.
  • The horizontal resolution of the two ENS constant-resolution forecasts provided for calibration and validation purposes will be increased:

 

 
 ENS calibration / validation
High resolutionLow resolution
 
Current
Upgrade
Current
Upgrade
Spectral
TL639
TCO639
TL319
TCO319
Gaussian grid
N320
N640
N160
N320
Horizontal grid resolution
~50 km
~xx km
~60 km
~xx km

Model Level
Vertical resolution

91
91
91
91

Wave model

 HRESENS
Leg ALeg B / C
 
Current
Upgrade
Current
Upgrade
CurrentUpgrade
Lat/Long
0.25
0.125
0.5
0.25
0.5
0.25
Horizontal grid resolution~28km~14km ~55km~28km~55km~28km
Dissemination (LL)
0.25
TBC
0.5
TBC
0.5
TBC
Frequencies
36
36
30
30
25
25
Directions
36
36
24
24
12
12

...

Section
Column

Gaussian grids

Naming convention

The Gaussian grids are defined by the quadrature points used to facilitate the accurate numerical computation of the integrals involved in the Fourier and Legendre transforms. The grids are labelled by N where N is the number of latitude lines between the pole and the equator.  For example, for the N640 Gaussian grid, there are 640 lines of latitude between the pole and the equator giving 1280 latitude lines in total.

The grid points in latitude, θk, are given by the zeros of the Legendre polynomial or order N:  PN0k=sinθk) = 0A consequence of this is that a Gaussian grid has:

  • latitude lines which are not equally spaced;
  • no latitude points at the poles;
  • no line of latitude at the equator;
  • latitude lines which are symmetric about the equator.

Regular (or full) Gaussian grid

A regular Gaussian grid has the following characteristics:

  • there are 4N longitude points along each latitude circle;
  • the longitudinal resolution in latitude-longitude is given by 90o/N;
  • the points get closer together (i.e. more crowded) as the latitude increases towards the poles;
  • the total number of grid points is 8N2.

Reduced (or quasi-regular) Gaussian grid

A reduced Gaussian grid:

  • has the same number of latitude lines (4N) as the corresponding regular Gaussian grid;
  • has a decreasing number of longitude points towards the poles;
  • has a quasi-regular grid spacing in distance at each latitude;
  • provides a uniform CFL (Courant–Friedrichs–Lewy) condition.

Up to and including IFS cycle 41r1, ECMWF has used a standard reduced Gaussian grid.  This has 4N longitude points at the latitude nearest to the equator, with the number of longitude points reducing in blocks as the latitudes approach the poles.

With the horizontal resolution increase at IFS cycle 42r1, ECMWF introduces a slightly different form of the reduced Gaussian grid which is referred to as the octahedral reduced Gaussian grid or, more simply, the octahedral grid.

Column

N48 regular Gaussian grid

N48 standard reduced Gaussian grid

...