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Table of Contents
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Input definition

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Input data may be specified either by giving a path in the Source parameter or by giving a GRIB-based data object in the Data parameter. Note that you should specify either Source or Data, not both.

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It is up to the user to specify if the input consists of wind fields. Set this appropriatelly in order to perform the correct processing.

Possible options are:

  • U/V to u/v

Converts pairs of Cartesian components vector fields (spectral) U/V to (gridded) u/v. This option is required if regridding wind fields on/to a rotated grid.

Note: assumes that the input come in pairs of alternating U/V.

  • vo/d to u/v

Converts pairs of (spectral) vo/d fields into (spectral) U/V or (gridded) u/v. In case of gridded output, scaling by the cosine of their latitudes is applied (as above.)

Note: assumes that the input come in pairs of alternating vo/d.

  • Off (default)
Each processed field is treated individually.

Spectral to grid inverse transform

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Select one of the predefined names from the following:

  • 1km (default)
binary-based LSM sourced from MODIS Land Water Mask MOD44W (see reference)
  • 10min
binary-based LSM at high resolution (legacy, pre-climate files version 15)
  • O1280
GRIB-based IFS supporting climate files version 15, on this specific grid
  • O640
(as above, for this grid)
  • O320
(as above, for this grid)
  • N320
(as above, for this grid)
  • N256
(as above, for this grid)
  • N128
(as above, for this grid)

LSM File Input/Output

Provide the path to an input/output LSM GRIB file.

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Activates a nabla (differential) operator processing on the fields. Possible options are:

  • Scalar Gradient
Scalar field gradient (∇)
  • Scalar Laplacian
Scalar field Laplacian (∇2)
  • UV Gradient
Vector (u/v) field gradient (∇)
  • UV Divergence
Vector (u/v) field divergence (∇⋅)
  • UV Vorticity
Vector (u/v) field vorticity or curl (∇×)
  • Off (default)
no differential processing

Nabla Poles Missing Values

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