In this section, each of the preprocessor modules is described, roughly following the default order in which preprocessor functions are applied:
Variable derivation
CMOR check and dataset-specific fixes
Fx variables as cell measures or ancillary variables
Vertical interpolation
Weighting
Land/Sea/Ice masking
Horizontal regridding
Masking of missing values
Ensemble statistics
Multi-model statistics
Time operations
Area operations
Volume operations
Cycles
Trend
Detrend
Unit conversion
Bias
Other
See preprocessor_functions
for implementation details and the exact default order.
The ESMValTool preprocessor can be used to perform a broad range of operations on the input data before diagnostics or metrics are applied. The preprocessor performs these operations in a centralized, documented and efficient way, thus reducing the data processing load on the diagnostics side. For an overview of the preprocessor structure see the Preprocessors
.
Each of the preprocessor operations is written in a dedicated python module and all of them receive and return an instance of iris.cube.Cube
, working sequentially on the data with no interactions between them. The order in which the preprocessor operations is applied is set by default to minimize the loss of information due to, for example, temporal and spatial subsetting or multi-model averaging. Nevertheless, the user is free to change such order to address specific scientific requirements, but keeping in mind that some operations must be necessarily performed in a specific order. This is the case, for instance, for multi-model statistics, which required the model to be on a common grid and therefore has to be called after the regridding module.
The variable derivation module allows to derive variables which are not in the CMIP standard data request using standard variables as input. The typical use case of this operation is the evaluation of a variable which is only available in an observational dataset but not in the models. In this case a derivation function is provided by the ESMValTool in order to calculate the variable and perform the comparison. For example, several observational datasets deliver total column ozone as observed variable (toz), but CMIP models only provide the ozone 3D field. In this case, a derivation function is provided to vertically integrate the ozone and obtain total column ozone for direct comparison with the observations.
To contribute a new derived variable, it is also necessary to define a name for it and to provide the corresponding CMOR table. This is to guarantee the proper metadata definition is attached to the derived data. Such custom CMOR tables are collected as part of the ESMValCore package. By default, the variable derivation will be applied only if the variable is not already available in the input data, but the derivation can be forced by setting the appropriate flag.
variables:
toz:
derive: true
force_derivation: false
The required arguments for this module are two boolean switches:
derive
: activate variable derivationforce_derivation
: force variable derivation even if the variable is directly available in the input data.
See also esmvalcore.preprocessor.derive
. To get an overview on derivation scripts and how to implement new ones, please go to derivation
.
Data preprocessed by ESMValTool is automatically checked against its cmor definition. To reduce the impact of this check while maintaining it as reliable as possible, it is split in two parts: one will check the metadata and will be done just after loading and concatenating the data and the other one will check the data itself and will be applied after all extracting operations are applied to reduce the amount of data to process.
Checks include, but are not limited to:
- Requested coordinates are present and comply with their definition.
- Correctness of variable names, units and other metadata.
- Compliance with the valid minimum and maximum values allowed if defined.
The most relevant (i.e. a missing coordinate) will raise an error while others (i.e an incorrect long name) will be reported as a warning.
Some of those issues will be fixed automatically by the tool, including the following:
- Incorrect standard or long names.
- Incorrect units, if they can be converted to the correct ones.
- Direction of coordinates.
- Automatic clipping of longitude to 0 - 360 interval.
- Minute differences between the required and actual vertical coordinate values
Sometimes, the checker will detect errors that it can not fix by itself. ESMValTool deals with those issues by applying specific fixes for those datasets that require them. Fixes are applied at three different preprocessor steps:
- fix_file: apply fixes directly to a copy of the file. Copying the files is costly, so only errors that prevent Iris to load the file are fixed here. See
esmvalcore.preprocessor.fix_file
- fix_metadata: metadata fixes are done just before concatenating the cubes loaded from different files in the final one. Automatic metadata fixes are also applied at this step. See
esmvalcore.preprocessor.fix_metadata
- fix_data: data fixes are applied before starting any operation that will alter the data itself. Automatic data fixes are also applied at this step. See
esmvalcore.preprocessor.fix_data
To get an overview on data fixes and how to implement new ones, please go to fixing_data
.
The following preprocessors may require the use of fx_variables
to be able to perform the computations:
Preprocessor | Default fx variables |
---|---|
area_statistics<area_statistics> |
areacella , areacello |
mask_landsea<land/sea/ice masking> |
sftlf , sftof |
mask_landseaice<ice masking> |
sftgif |
volume_statistics<volume_statistics> |
volcello |
weighting_landsea_fraction<land/sea fraction weighting> |
sftlf , sftof |
If the option fx_variables
is not explicitly specified for these preprocessors, the default fx variables in the second column are automatically used. If given, the fx_variables
argument specifies the fx variables that the user wishes to input to the corresponding preprocessor function. The user may specify these by simply adding the names of the variables, e.g.,
fx_variables:
areacello:
volcello:
or by additionally specifying further keys that are used to define the fx datasets, e.g.,
fx_variables:
areacello:
mip: Ofx
exp: piControl
volcello:
mip: Omon
This might be useful to select fx files from a specific mip
table or from a specific exp
in case not all experiments provide the fx variable.
Alternatively, the fx_variables
argument can also be specified as a list:
fx_variables: ['areacello', 'volcello']
or as a list of dictionaries:
fx_variables: [{'short_name': 'areacello', 'mip': 'Ofx', 'exp': 'piControl'}, {'short_name': 'volcello', 'mip': 'Omon'}]
The recipe parser will automatically find the data files that are associated with these variables and pass them to the function for loading and processing.
If mip
is not given, ESMValTool will search for the fx variable in all available tables of the specified project.
Warning
Some fx variables exist in more than one table (e.g., volcello
exists in CMIP6's Odec
, Ofx
, Omon
, and Oyr
tables; sftgif
exists in CMIP6's fx
, IyrAnt
and IyrGre
, and LImon
tables). If (for a given dataset) fx files are found in more than one table, mip
needs to be specified, otherwise an error is raised.
Note
To explicitly not use any fx variables in a preprocessor, use fx_variables: null
. While some of the preprocessors mentioned above do work without fx variables (e.g., area_statistics
or mask_landsea
with datasets that have regular latitude/longitude grids), using this option is not recommended.
Internally, the required fx_variables
are automatically loaded by the preprocessor step add_fx_variables
which also checks them against CMOR standards and adds them either as cell_measure
(see CF conventions on cell measures and iris.coords.CellMeasure
) or ancillary_variable
(see CF conventions on ancillary variables and iris.coords.AncillaryVariable
) inside the cube data. This ensures that the defined preprocessor chain is applied to both variables
and fx_variables
.
Note that when calling steps that require fx_variables
inside diagnostic scripts, the variables are expected to contain the required cell_measures
or ancillary_variables
. If missing, they can be added using the following functions:
from esmvalcore.preprocessor import (add_cell_measure, add_ancillary_variable)
cube_with_area_measure = add_cell_measure(cube, area_cube, 'area')
cube_with_volume_measure = add_cell_measure(cube, volume_cube, 'volume)
cube_with_ancillary_sftlf = add_ancillary_variable(cube, sftlf_cube)
cube_with_ancillary_sftgif = add_ancillary_variable(cube, sftgif_cube)
Details on the arguments needed for each step can be found in the following sections.
Vertical level selection is an important aspect of data preprocessing since it allows the scientist to perform a number of metrics specific to certain levels (whether it be air pressure or depth, e.g. the Quasi-Biennial-Oscillation (QBO) u30 is computed at 30 hPa). Dataset native vertical grids may not come with the desired set of levels, so an interpolation operation will be needed to regrid the data vertically. ESMValTool can perform this vertical interpolation via the extract_levels
preprocessor. Level extraction may be done in a number of ways.
Level extraction can be done at specific values passed to extract_levels
as levels:
with its value a list of levels (note that the units are CMOR-standard, Pascals (Pa)):
preprocessors:
preproc_select_levels_from_list:
extract_levels:
levels: [100000., 50000., 3000., 1000.]
scheme: linear
It is also possible to extract the CMIP-specific, CMOR levels as they appear in the CMOR table, e.g. plev10
or plev17
or plev19
etc:
preprocessors:
preproc_select_levels_from_cmip_table:
extract_levels:
levels: {cmor_table: CMIP6, coordinate: plev10}
scheme: nearest
Of good use is also the level extraction with values specific to a certain dataset, without the user actually polling the dataset of interest to find out the specific levels: e.g. in the example below we offer two alternatives to extract the levels and vertically regrid onto the vertical levels of ERA-Interim
:
preprocessors:
preproc_select_levels_from_dataset:
extract_levels:
levels: ERA-Interim
# This also works, but allows specifying the pressure coordinate name
# levels: {dataset: ERA-Interim, coordinate: air_pressure}
scheme: linear_extrapolate
By default, vertical interpolation is performed in the dimension coordinate of the z axis. If you want to explicitly declare the z axis coordinate to use (for example, air_pressure
' in variables that are provided in model levels and not pressure levels) you can override that automatic choice by providing the name of the desired coordinate:
preprocessors:
preproc_select_levels_from_dataset:
extract_levels:
levels: ERA-Interim
scheme: linear_extrapolate
coordinate: air_pressure
If coordinate
is specified, pressure levels (if present) can be converted to height levels and vice versa using the US standard atmosphere. E.g. coordinate = altitude
will convert existing pressure levels (air_pressure) to height levels (altitude); coordinate = air_pressure
will convert existing height levels (altitude) to pressure levels (air_pressure).
If the requested levels are very close to the values in the input data, the function will just select the available levels instead of interpolating. The meaning of 'very close' can be changed by providing the parameters:
rtol
Relative tolerance for comparing the levels in the input data to the requested levels. If the levels are sufficiently close, the requested levels will be assigned to the vertical coordinate and no interpolation will take place. The default value is 10^-7.
atol
Absolute tolerance for comparing the levels in the input data to the requested levels. If the levels are sufficiently close, the requested levels will be assigned to the vertical coordinate and no interpolation will take place. By default, atol will be set to 10^-7 times the mean value of of the available levels.
The vertical interpolation currently supports the following schemes:
linear
: Linear interpolation without extrapolation, i.e., extrapolation points will be masked even if the source data is not a masked array.linear_extrapolate
: Linear interpolation with nearest-neighbour extrapolation, i.e., extrapolation points will take their value from the nearest source point.nearest
: Nearest-neighbour interpolation without extrapolation, i.e., extrapolation points will be masked even if the source data is not a masked array.nearest_extrapolate
: Nearest-neighbour interpolation with nearest-neighbour extrapolation, i.e., extrapolation points will take their value from the nearest source point.
Note
Previous versions of ESMValCore (<2.5.0) supported the schemes linear_horizontal_extrapolate_vertical
and nearest_horizontal_extrapolate_vertical
. These schemes have been renamed to linear_extrapolate
and nearest_extrapolate
, respectively, in version 2.5.0 and are identical to the new schemes. Support for the old names will be removed in version 2.7.0.
- See also
esmvalcore.preprocessor.extract_levels
. - See also
esmvalcore.preprocessor.get_cmor_levels
.
Note
Controlling the extrapolation mode allows us to avoid situations where extrapolating values makes little physical sense (e.g. extrapolating beyond the last data point).
This preprocessor allows weighting of data by land or sea fractions. In other words, this function multiplies the given input field by a fraction in the range 0-1 to account for the fact that not all grid points are completely land- or sea-covered.
The application of this preprocessor is very important for most carbon cycle variables (and other land surface outputs), which are e.g. reported in units of kgC m − 2. Here, the surface unit actually refers to 'square meter of land/sea' and NOT 'square meter of gridbox'. In order to integrate these globally or regionally one has to weight by both the surface quantity and the land/sea fraction.
For example, to weight an input field with the land fraction, the following preprocessor can be used:
preprocessors:
preproc_weighting:
weighting_landsea_fraction:
area_type: land
exclude: ['CanESM2', 'reference_dataset']
Allowed arguments for the keyword area_type
are land
(fraction is 1 for grid cells with only land surface, 0 for grid cells with only sea surface and values in between 0 and 1 for coastal regions) and sea
(1 for sea, 0 for land, in between for coastal regions). The optional argument exclude
allows to exclude specific datasets from this preprocessor, which is for example useful for climate models which do not offer land/sea fraction files. This arguments also accepts the special dataset specifiers reference_dataset
and alternative_dataset
.
Optionally you can specify your own custom fx variable to be used in cases when e.g. a certain experiment is preferred for fx data retrieval:
preprocessors:
preproc_weighting:
weighting_landsea_fraction:
area_type: land
exclude: ['CanESM2', 'reference_dataset']
fx_variables:
sftlf:
exp: piControl
sftof:
exp: piControl
or alternatively:
preprocessors:
preproc_weighting:
weighting_landsea_fraction:
area_type: land
exclude: ['CanESM2', 'reference_dataset']
fx_variables: [
{'short_name': 'sftlf', 'exp': 'piControl'},
{'short_name': 'sftof', 'exp': 'piControl'}
]
More details on the argument fx_variables
and its default values are given in Fx variables as cell measures or ancillary variables
.
See also esmvalcore.preprocessor.weighting_landsea_fraction
.
Certain metrics and diagnostics need to be computed and performed on specific domains on the globe. The ESMValTool preprocessor supports filtering the input data on continents, oceans/seas and ice. This is achieved by masking the model data and keeping only the values associated with grid points that correspond to, e.g., land, ocean or ice surfaces, as specified by the user. Where possible, the masking is realized using the standard mask files provided together with the model data as part of the CMIP data request (the so-called fx variable). In the absence of these files, the Natural Earth masks are used: although these are not model-specific, they represent a good approximation since they have a much higher resolution than most of the models and they are regularly updated with changing geographical features.
In ESMValTool, land-sea-ice masking can be done in two places: in the preprocessor, to apply a mask on the data before any subsequent preprocessing step and before running the diagnostic, or in the diagnostic scripts themselves. We present both these implementations below.
To mask out a certain domain (e.g., sea) in the preprocessor, mask_landsea
can be used:
preprocessors:
preproc_mask:
mask_landsea:
mask_out: sea
and requires only one argument: mask_out
: either land
or sea
.
Optionally you can specify your own custom fx variable to be used in cases when e.g. a certain experiment is preferred for fx data retrieval. Note that it is possible to specify as many tags for the fx variable as required:
preprocessors:
landmask:
mask_landsea:
mask_out: sea
fx_variables:
sftlf:
exp: piControl
sftof:
exp: piControl
ensemble: r2i1p1f1
or alternatively:
preprocessors:
landmask:
mask_landsea:
mask_out: sea
fx_variables: [
{'short_name': 'sftlf', 'exp': 'piControl'},
{'short_name': 'sftof', 'exp': 'piControl', 'ensemble': 'r2i1p1f1'}
]
More details on the argument fx_variables
and its default values are given in Fx variables as cell measures or ancillary variables
.
If the corresponding fx file is not found (which is the case for some models and almost all observational datasets), the preprocessor attempts to mask the data using Natural Earth mask files (that are vectorized rasters). As mentioned above, the spatial resolution of the the Natural Earth masks are much higher than any typical global model (10m for land and glaciated areas and 50m for ocean masks).
See also esmvalcore.preprocessor.mask_landsea
.
Note that for masking out ice sheets, the preprocessor uses a different function, to ensure that both land and sea or ice can be masked out without losing generality. To mask ice out, mask_landseaice
can be used:
preprocessors:
preproc_mask:
mask_landseaice:
mask_out: ice
and requires only one argument: mask_out
: either landsea
or ice
.
Optionally you can specify your own custom fx variable to be used in cases when e.g. a certain experiment is preferred for fx data retrieval:
preprocessors:
landseaicemask:
mask_landseaice:
mask_out: sea
fx_variables:
sftgif:
exp: piControl
or alternatively:
preprocessors:
landseaicemask:
mask_landseaice:
mask_out: sea
fx_variables: [{'short_name': 'sftgif', 'exp': 'piControl'}]
More details on the argument fx_variables
and its default values are given in Fx variables as cell measures or ancillary variables
.
See also esmvalcore.preprocessor.mask_landseaice
.
For masking out glaciated areas a Natural Earth shapefile is used. To mask glaciated areas out, mask_glaciated
can be used:
preprocessors:
preproc_mask:
mask_glaciated:
mask_out: glaciated
and it requires only one argument: mask_out
: only glaciated
.
See also esmvalcore.preprocessor.mask_landseaice
.
Missing (masked) values can be a nuisance especially when dealing with multi-model ensembles and having to compute multi-model statistics; different numbers of missing data from dataset to dataset may introduce biases and artificially assign more weight to the datasets that have less missing data. This is handled in ESMValTool via the missing values masks: two types of such masks are available, one for the multi-model case and another for the single model case.
The multi-model missing values mask (mask_fillvalues
) is a preprocessor step that usually comes after all the single-model steps (regridding, area selection etc) have been performed; in a nutshell, it combines missing values masks from individual models into a multi-model missing values mask; the individual model masks are built according to common criteria: the user chooses a time window in which missing data points are counted, and if the number of missing data points relative to the number of total data points in a window is less than a chosen fractional threshold, the window is discarded i.e. all the points in the window are masked (set to missing).
preprocessors:
missing_values_preprocessor:
mask_fillvalues:
threshold_fraction: 0.95
min_value: 19.0
time_window: 10.0
In the example above, the fractional threshold for missing data vs. total data is set to 95% and the time window is set to 10.0 (units of the time coordinate units). Optionally, a minimum value threshold can be applied, in this case it is set to 19.0 (in units of the variable units).
See also esmvalcore.preprocessor.mask_fillvalues
.
To create a combined multi-model mask (all the masks from all the analyzed datasets combined into a single mask using a logical OR), the preprocessor mask_multimodel
can be used. In contrast to mask_fillvalues
, mask_multimodel
does not expect that the datasets have a time
coordinate, but works on datasets with arbitrary (but identical) coordinates. After mask_multimodel
, all involved datasets have an identical mask.
See also esmvalcore.preprocessor.mask_multimodel
.
Thresholding on minimum and maximum accepted data values can also be performed: masks are constructed based on the results of thresholding; inside and outside interval thresholding and masking can also be performed. These functions are mask_above_threshold
, mask_below_threshold
, mask_inside_range
, and mask_outside_range
.
These functions always take a cube as first argument and either threshold
for threshold masking or the pair minimum
, maximum
for interval masking.
See also esmvalcore.preprocessor.mask_above_threshold
and related functions.
Regridding is necessary when various datasets are available on a variety of lat-lon grids and they need to be brought together on a common grid (for various statistical operations e.g. multi-model statistics or for e.g. direct inter-comparison or comparison with observational datasets). Regridding is conceptually a very similar process to interpolation (in fact, the regridder engine uses interpolation and extrapolation, with various schemes). The primary difference is that interpolation is based on sample data points, while regridding is based on the horizontal grid of another cube (the reference grid). If the horizontal grids of a cube and its reference grid are sufficiently the same, regridding is automatically and silently skipped for performance reasons.
The underlying regridding mechanism in ESMValTool uses iris.cube.Cube.regrid
from Iris.
The use of the horizontal regridding functionality is flexible depending on what type of reference grid and what interpolation scheme is preferred. Below we show a few examples.
The example below shows how to regrid on the reference dataset ERA-Interim
(observational data, but just as well CMIP, obs4MIPs, or ana4mips datasets can be used); in this case the scheme is linear.
preprocessors:
regrid_preprocessor:
regrid:
target_grid: ERA-Interim
scheme: linear
The example below shows how to regrid on a reference grid with a cell specification of 2.5x2.5
degrees. This is similar to regridding on reference datasets, but in the previous case the reference dataset grid cell specifications are not necessarily known a priori. Regridding on an MxN
cell specification is oftentimes used when operating on localized data.
preprocessors:
regrid_preprocessor:
regrid:
target_grid: 2.5x2.5
scheme: nearest
In this case the NearestNeighbour
interpolation scheme is used (see below for scheme definitions).
When using a MxN
type of grid it is possible to offset the grid cell centrepoints using the lat_offset and lon_offset
arguments:
lat_offset
: offsets the grid centers of the latitude coordinate w.r.t. the pole by half a grid step;lon_offset
: offsets the grid centers of the longitude coordinate w.r.t. Greenwich meridian by half a grid step.
preprocessors:
regrid_preprocessor:
regrid:
target_grid: 2.5x2.5
lon_offset: True
lat_offset: True
scheme: nearest
This example shows how to regrid to a regional target grid specification. This is useful if both a regrid
and extract_region
step are necessary.
preprocessors:
regrid_preprocessor:
regrid:
target_grid:
start_longitude: 40
end_longitude: 60
step_longitude: 2
start_latitude: -10
end_latitude: 30
step_latitude: 2
scheme: nearest
This defines a grid ranging from 40° to 60° longitude with 2° steps, and -10° to 30° latitude with 2° steps. If end_longitude
or end_latitude
do not fall on the grid (e.g., end_longitude: 61
), it cuts off at the nearest previous value (e.g. 60
).
The longitude coordinates will wrap around the globe if necessary, i.e. start_longitude: 350
, end_longitude: 370
is valid input.
The arguments are defined below:
start_latitude
: Latitude value of the first grid cell center (start point). The grid includes this value.end_latitude
: Latitude value of the last grid cell center (end point). The grid includes this value only if it falls on a grid point. Otherwise, it cuts off at the previous value.step_latitude
: Latitude distance between the centers of two neighbouring cells.start_longitude
: Latitude value of the first grid cell center (start point). The grid includes this value.end_longitude
: Longitude value of the last grid cell center (end point). The grid includes this value only if it falls on a grid point. Otherwise, it cuts off at the previous value.step_longitude
: Longitude distance between the centers of two neighbouring cells.
ESMValTool has a number of built-in regridding schemes, which are presented in built-in regridding schemes
. Additionally, it is also possible to use third party regridding schemes designed for use with Iris
<iris:index>
. This is explained in generic regridding schemes
.
The schemes used for the interpolation and extrapolation operations needed by the horizontal regridding functionality directly map to their corresponding implementations in iris
:
linear
: Linear interpolation without extrapolation, i.e., extrapolation points will be masked even if the source data is not a masked array (usesLinear(extrapolation_mode='mask')
, seeiris.analysis.Linear
).linear_extrapolate
: Linear interpolation with extrapolation, i.e., extrapolation points will be calculated by extending the gradient of the closest two points (usesLinear(extrapolation_mode='extrapolate')
, seeiris.analysis.Linear
).nearest
: Nearest-neighbour interpolation without extrapolation, i.e., extrapolation points will be masked even if the source data is not a masked array (usesNearest(extrapolation_mode='mask')
, seeiris.analysis.Nearest
).area_weighted
: Area-weighted regridding (usesAreaWeighted()
, seeiris.analysis.AreaWeighted
).unstructured_nearest
: Nearest-neighbour interpolation for unstructured grids (usesUnstructuredNearest()
, seeiris.analysis.UnstructuredNearest
).
See also esmvalcore.preprocessor.regrid
Note
Controlling the extrapolation mode allows us to avoid situations where extrapolating values makes little physical sense (e.g. extrapolating beyond the last data point).
Note
The regridding mechanism is (at the moment) done with fully realized data in memory, so depending on how fine the target grid is, it may use a rather large amount of memory. Empirically target grids of up to 0.5x0.5
degrees should not produce any memory-related issues, but be advised that for resolutions of < 0.5
degrees the regridding becomes very slow and will use a lot of memory.
Iris' regridding <iris:interpolation_and_regridding>
is based around the flexible use of so-called regridding schemes. These are classes that know how to transform a source cube with a given grid into the grid defined by a given target cube. Iris itself provides a number of useful schemes, but they are largely limited to work with simple, regular grids. Other schemes can be provided independently. This is interesting when special regridding-needs arise or when more involved grids and meshes need to be considered. Furthermore, it may be desirable to have finer control over the parameters of the scheme than is afforded by the built-in schemes described above.
To facilitate this, the ~esmvalcore.preprocessor.regrid
preprocessor allows the use of any scheme designed for Iris. The scheme must be installed and importable. To use this feature, the scheme
key passed to the preprocessor must be a dictionary instead of a simple string that contains all necessary information. That includes a reference
to the desired scheme itself, as well as any arguments that should be passed through to the scheme. For example, the following shows the use of the built-in scheme iris.analysis.AreaWeighted
with a custom threshold for missing data tolerance.
preprocessors:
regrid_preprocessor:
regrid:
target_grid: 2.5x2.5
scheme:
reference: iris.analysis:AreaWeighted
mdtol: 0.7
The value of the reference
key has two parts that are separated by a :
with no surrounding spaces. The first part is an importable Python module, the second refers to the scheme, i.e. some callable that will be called with the remaining entries of the scheme
dictionary passed as keyword arguments.
One package that aims to capitalize on the support for unstructured
meshes introduced in Iris 3.2 <iris:ugrid>
is iris-esmf-regrid:index
. It aims to provide lazy regridding for structured regular and irregular grids, as well as unstructured meshes. An example of its usage in an ESMValTool preprocessor is:
preprocessors:
regrid_preprocessor:
regrid:
target_grid: 2.5x2.5
scheme:
reference: esmf_regrid.schemes:ESMFAreaWeighted
mdtol: 0.7
Warning
Just as the mesh support in Iris itself, this new regridding package is still considered experimental.
For certain use cases it may be desirable to compute ensemble statistics. For example to prevent models with many ensemble members getting excessive weight in the multi-model statistics functions.
Theoretically, ensemble statistics are a special case (grouped) multi-model statistics. This grouping is performed taking into account the dataset tags project, dataset, experiment, and (if present) sub_experiment. However, they should typically be computed earlier in the workflow. Moreover, because multiple ensemble members of the same model are typically more consistent/homogeneous than datasets from different models, the implementation is more straigtforward and can benefit from lazy evaluation and more efficient computation.
The preprocessor takes a list of statistics as input:
preprocessors:
example_preprocessor:
ensemble_statistics:
statistics: [mean, median]
This preprocessor function exposes the iris analysis package, and works with all (capitalized) statistics from the iris.analysis
package that can be executed without additional arguments (e.g. percentiles are not supported because it requires additional keywords: percentile.).
Note that ensemble_statistics
will not return the single model and ensemble files, only the requested ensemble statistics results.
In case of wanting to save both individual ensemble members as well as the statistic results, the preprocessor chains could be defined as:
preprocessors:
everything_else: &everything_else
area_statistics: ...
regrid_time: ...
multimodel:
<<: *everything_else
ensemble_statistics:
variables:
tas_datasets:
short_name: tas
preprocessor: everything_else
...
tas_multimodel:
short_name: tas
preprocessor: multimodel
...
See also esmvalcore.preprocessor.ensemble_statistics
.
Computing multi-model statistics is an integral part of model analysis and evaluation: individual models display a variety of biases depending on model set-up, initial conditions, forcings and implementation; comparing model data to observational data, these biases have a significantly lower statistical impact when using a multi-model ensemble. ESMValTool has the capability of computing a number of multi-model statistical measures: using the preprocessor module multi_model_statistics
will enable the user to ask for either a multi-model mean
, median
, max
, min
, std_dev
, and / or pXX.YY
with a set of argument parameters passed to multi_model_statistics
. Percentiles can be specified like p1.5
or p95
. The decimal point will be replaced by a dash in the output file.
Restrictive computation is also available by excluding any set of models that the user will not want to include in the statistics (by setting exclude: [excluded models list]
argument). The implementation has a few restrictions that apply to the input data: model datasets must have consistent shapes, apart from the time dimension; and cubes with more than four dimensions (time, vertical axis, two horizontal axes) are not supported.
Input datasets may have different time coordinates. Statistics can be computed across overlapping times only (span: overlap
) or across the full time span of the combined models (span: full
). The preprocessor sets a common time coordinate on all datasets. As the number of days in a year may vary between calendars, (sub-)daily data with different calendars are not supported. The preprocessor saves both the input single model files as well as the multi-model results. In case you do not want to keep the single model files, set the parameter keep_input_datasets
to false
(default value is true
).
preprocessors:
multi_model_save_input:
multi_model_statistics:
span: overlap
statistics: [mean, median]
exclude: [NCEP]
multi_model_without_saving_input:
multi_model_statistics:
span: overlap
statistics: [mean, median]
exclude: [NCEP]
keep_input_datasets: false
Input datasets may have different time coordinates. The multi-model statistics preprocessor sets a common time coordinate on all datasets. As the number of days in a year may vary between calendars, (sub-)daily data are not supported.
Multi-model statistics also supports a groupby
argument. You can group by any dataset key (project
, experiment
, etc.) or a combination of keys in a list. You can also add an arbitrary tag to a dataset definition and then group by that tag. When using this preprocessor in conjunction with ensemble statistics preprocessor, you can group by ensemble_statistics
as well. For example:
datasets:
- {dataset: CanESM2, exp: historical, ensemble: "r(1:2)i1p1"}
- {dataset: CCSM4, exp: historical, ensemble: "r(1:2)i1p1"}
preprocessors:
example_preprocessor:
ensemble_statistics:
statistics: [median, mean]
multi_model_statistics:
span: overlap
statistics: [min, max]
groupby: [ensemble_statistics]
exclude: [NCEP]
This will first compute ensemble mean and median, and then compute the multi-model min and max separately for the ensemble means and medians. Note that this combination will not save the individual ensemble members, only the ensemble and multimodel statistics results.
When grouping by a tag not defined in all datasets, the datasets missing the tag will be grouped together. In the example below, datasets UKESM and ERA5 would belong to the same group, while the other datasets would belong to either group1
or group2
datasets:
- {dataset: CanESM2, exp: historical, ensemble: "r(1:2)i1p1", tag: 'group1'}
- {dataset: CanESM5, exp: historical, ensemble: "r(1:2)i1p1", tag: 'group2'}
- {dataset: CCSM4, exp: historical, ensemble: "r(1:2)i1p1", tag: 'group2'}
- {dataset: UKESM, exp: historical, ensemble: "r(1:2)i1p1"}
- {dataset: ERA5}
preprocessors:
example_preprocessor:
multi_model_statistics:
span: overlap
statistics: [min, max]
groupby: [tag]
Note that those datasets can be excluded if listed in the exclude
option.
See also esmvalcore.preprocessor.multi_model_statistics
.
Note
The multi-model array operations can be rather memory-intensive (since they are not performed lazily as yet). The Section on Memory use
details the memory intake for different run scenarios, but as a thumb rule, for the multi-model preprocessor, the expected maximum memory intake could be approximated as the number of datasets multiplied by the average size in memory for one dataset.
The _time.py
module contains the following preprocessor functions:
- extract_time: Extract a time range from a cube.
- extract_season: Extract only the times that occur within a specific season.
- extract_month: Extract only the times that occur within a specific month.
- hourly_statistics: Compute intra-day statistics
- daily_statistics: Compute statistics for each day
- monthly_statistics: Compute statistics for each month
- seasonal_statistics: Compute statistics for each season
- annual_statistics: Compute statistics for each year
- decadal_statistics: Compute statistics for each decade
- climate_statistics: Compute statistics for the full period
- resample_time: Resample data
- resample_hours: Convert between N-hourly frequencies by resampling
- anomalies: Compute (standardized) anomalies
- regrid_time: Aligns the time axis of each dataset to have common time points and calendars.
- timeseries_filter: Allows application of a filter to the time-series data.
Statistics functions are applied by default in the order they appear in the list. For example, the following example applied to hourly data will retrieve the minimum values for the full period (by season) of the monthly mean of the daily maximum of any given variable.
daily_statistics:
operator: max
monthly_statistics:
operator: mean
climate_statistics:
operator: min
period: season
This function subsets a dataset between two points in times. It removes all times in the dataset before the first time and after the last time point. The required arguments are relatively self explanatory:
start_year
start_month
start_day
end_year
end_month
end_day
These start and end points are set using the datasets native calendar. All six arguments should be given as integers - the named month string will not be accepted.
See also esmvalcore.preprocessor.extract_time
.
Extract only the times that occur within a specific season.
This function only has one argument: season
. This is the named season to extract, i.e. DJF, MAM, JJA, SON, but also all other sequentially correct combinations, e.g. JJAS.
Note that this function does not change the time resolution. If your original data is in monthly time resolution, then this function will return three monthly datapoints per year.
If you want the seasonal average, then this function needs to be combined with the seasonal_mean function, below.
See also esmvalcore.preprocessor.extract_season
.
The function extracts the times that occur within a specific month. This function only has one argument: month
. This value should be an integer between 1 and 12 as the named month string will not be accepted.
See also esmvalcore.preprocessor.extract_month
.
This function produces statistics at a x-hourly frequency.
- Parameters:
- every_n_hours: frequency to use to compute the statistics. Must be a divisor of 24.
- operator: operation to apply. Accepted values are 'mean', 'median', 'std_dev', 'min', 'max' and 'sum'. Default is 'mean'
See also esmvalcore.preprocessor.daily_statistics
.
This function produces statistics for each day in the dataset.
- Parameters:
- operator: operation to apply. Accepted values are 'mean', 'median', 'std_dev', 'min', 'max', 'sum' and 'rms'. Default is 'mean'
See also esmvalcore.preprocessor.daily_statistics
.
This function produces statistics for each month in the dataset.
- Parameters:
- operator: operation to apply. Accepted values are 'mean', 'median', 'std_dev', 'min', 'max', 'sum' and 'rms'. Default is 'mean'
See also esmvalcore.preprocessor.monthly_statistics
.
This function produces statistics for each season (default: [DJF, MAM, JJA, SON]
or custom seasons e.g. [JJAS, ONDJFMAM]
) in the dataset. Note that this function will not check for missing time points. For instance, if you are looking at the DJF field, but your datasets starts on January 1st, the first DJF field will only contain data from January and February.
We recommend using the extract_time to start the dataset from the following December and remove such biased initial datapoints.
- Parameters:
- operator: operation to apply. Accepted values are 'mean', 'median', 'std_dev', 'min', 'max', 'sum' and 'rms'. Default is 'mean'
- seasons: seasons to build statistics. Default is '[DJF, MAM, JJA, SON]'
See also esmvalcore.preprocessor.seasonal_statistics
.
This function produces statistics for each year.
- Parameters:
- operator: operation to apply. Accepted values are 'mean', 'median', 'std_dev', 'min', 'max', 'sum' and 'rms'. Default is 'mean'
See also esmvalcore.preprocessor.annual_statistics
.
This function produces statistics for each decade.
- Parameters:
- operator: operation to apply. Accepted values are 'mean', 'median', 'std_dev', 'min', 'max', 'sum' and 'rms'. Default is 'mean'
See also esmvalcore.preprocessor.decadal_statistics
.
This function produces statistics for the whole dataset. It can produce scalars (if the full period is chosen) or daily, monthly or seasonal statistics.
- Parameters:
- operator: operation to apply. Accepted values are 'mean', 'median', 'std_dev', 'min', 'max', 'sum' and 'rms'. Default is 'mean'
- period: define the granularity of the statistics: get values for the full period, for each month or day of year. Available periods: 'full', 'season', 'seasonal', 'monthly', 'month', 'mon', 'daily', 'day'. Default is 'full'
- seasons: if period 'seasonal' or 'season' allows to set custom seasons. Default is '[DJF, MAM, JJA, SON]'
- Examples:
Monthly climatology:
climate_statistics: operator: mean period: month
Daily maximum for the full period:
climate_statistics: operator: max period: day
Minimum value in the period:
climate_statistics: operator: min period: full
See also esmvalcore.preprocessor.climate_statistics
.
This function changes the frequency of the data in the cube by extracting the timesteps that meet the criteria. It is important to note that it is mainly meant to be used with instantaneous data.
- Parameters:
- month: Extract only timesteps from the given month or do nothing if None. Default is None
- day: Extract only timesteps from the given day of month or do nothing if None. Default is None
- hour: Extract only timesteps from the given hour or do nothing if None. Default is None
- Examples:
Hourly data to daily:
resample_time: hour: 12
Hourly data to monthly:
resample_time: hour: 12 day: 15
Daily data to monthly:
resample_time: day: 15
See also esmvalcore.preprocessor.resample_time
.
resample_hours:
This function changes the frequency of the data in the cube by extracting the timesteps that belongs to the desired frequency. It is important to note that it is mainly mean to be used with instantaneous data
- Parameters:
- interval: New frequency of the data. Must be a divisor of 24
- offset: First desired hour. Default 0. Must be lower than the interval
- Examples:
Convert to 12-hourly, by getting timesteps at 0:00 and 12:00:
resample_hours: hours: 12
Convert to 12-hourly, by getting timesteps at 6:00 and 18:00:
resample_hours: hours: 12
offset: 6
See also esmvalcore.preprocessor.resample_hours
.
This function computes the anomalies for the whole dataset. It can compute anomalies from the full, seasonal, monthly and daily climatologies. Optionally standardized anomalies can be calculated.
- Parameters:
- period: define the granularity of the climatology to use: full period, seasonal, monthly or daily. Available periods: 'full', 'season', 'seasonal', 'monthly', 'month', 'mon', 'daily', 'day'. Default is 'full'
- reference: Time slice to use as the reference to compute the climatology on. Can be 'null' to use the full cube or a dictionary with the parameters from extract_time. Default is null
- standardize: if true calculate standardized anomalies (default: false)
- seasons: if period 'seasonal' or 'season' allows to set custom seasons. Default is '[DJF, MAM, JJA, SON]'
- Examples:
Anomalies from the full period climatology:
anomalies:
Anomalies from the full period monthly climatology:
anomalies: period: month
Standardized anomalies from the full period climatology:
anomalies: standardized: true
Standardized Anomalies from the 1979-2000 monthly climatology:
anomalies: period: month reference: start_year: 1979 start_month: 1 start_day: 1 end_year: 2000 end_month: 12 end_day: 31 standardize: true
See also esmvalcore.preprocessor.anomalies
.
This function aligns the time points of each component dataset so that the Iris cubes from different datasets can be subtracted. The operation makes the datasets time points common; it also resets the time bounds and auxiliary coordinates to reflect the artificially shifted time points. Current implementation for monthly and daily data; the frequency
is set automatically from the variable CMOR table unless a custom frequency
is set manually by the user in recipe.
See also esmvalcore.preprocessor.regrid_time
.
This function allows the user to apply a filter to the timeseries data. This filter may be of the user's choice (currently only the low-pass
Lanczos filter is implemented); the implementation is inspired by this iris example and uses aggregation via iris.cube.Cube.rolling_window
.
- Parameters:
- window: the length of the filter window (in units of cube time coordinate).
- span: period (number of months/days, depending on data frequency) on which weights should be computed e.g. for 2-yearly: span = 24 (2 x 12 months). Make sure span has the same units as the data cube time coordinate.
- filter_type: the type of filter to be applied; default 'lowpass'. Available types: 'lowpass'.
- filter_stats: the type of statistic to aggregate on the rolling window; default 'sum'. Available operators: 'mean', 'median', 'std_dev', 'sum', 'min', 'max', 'rms'.
- Examples:
Lowpass filter with a monthly mean as operator:
timeseries_filter: window: 3 # 3-monthly filter window span: 12 # weights computed on the first year filter_type: lowpass # low-pass filter filter_stats: mean # 3-monthly mean lowpass filter
See also esmvalcore.preprocessor.timeseries_filter
.
The area manipulation module contains the following preprocessor functions:
- extract_coordinate_points: Extract a point with arbitrary coordinates given an interpolation scheme.
- extract_region: Extract a region from a cube based on
lat/lon
corners. - extract_named_regions: Extract a specific region from in the region coordinate.
- extract_shape: Extract a region defined by a shapefile.
- extract_point: Extract a single point (with interpolation)
- extract_location: Extract a single point by its location (with interpolation)
- zonal_statistics: Compute zonal statistics.
- meridional_statistics: Compute meridional statistics.
- area_statistics: Compute area statistics.
This function extracts points with given coordinates, following either a linear
or a nearest
interpolation scheme. The resulting point cube will match the respective coordinates to those of the input coordinates. If the input coordinate is a scalar, the dimension will be a scalar in the output cube.
If the point to be extracted has at least one of the coordinate point values outside the interval of the cube's same coordinate values, then no extrapolation will be performed, and the resulting extracted cube will have fully masked data.
- Examples:
Extract a point from coordinate grid_latitude with given coordinate value 26.0:
extract_coordinate_points: definition: grid_latitude: 26. scheme: nearest
See also esmvalcore.preprocessor.extract_coordinate_points
.
This function returns a subset of the data on the rectangular region requested. The boundaries of the region are provided as latitude and longitude coordinates in the arguments:
start_longitude
end_longitude
start_latitude
end_latitude
Note that this function can only be used to extract a rectangular region. Use extract_shape
to extract any other shaped region from a shapefile.
If the grid is irregular, the returned region retains the original coordinates, but is cropped to a rectangular bounding box defined by the start/end coordinates. The deselected area inside the region is masked.
See also esmvalcore.preprocessor.extract_region
.
This function extracts a specific named region from the data. This function takes the following argument: regions
which is either a string or a list of strings of named regions. Note that the dataset must have a region
coordinate which includes a list of strings as values. This function then matches the named regions against the requested string.
See also esmvalcore.preprocessor.extract_named_regions
.
Extract a shape or a representative point for this shape from the data.
- Parameters:
shapefile
: path to the shapefile containing the geometry of the region to be extracted. If the file contains multiple shapes behaviour depends on the decomposed parameter. This path can be relative toauxiliary_data_dir
defined in theuser configuration file
.method
: the method to select the region, selecting either all pointscontained by the shape or a single representative point. Choose either 'contains' or 'representative'. If not a single grid point is contained in the shape, a representative point will be selected.
crop
: by default extract_region will be used to crop the data to aminimal rectangular region containing the shape. Set to
false
to only mask data outside the shape. Data on irregular grids will not be cropped.
decomposed
: by defaultfalse
, in this case the union of all the regions in the shape file is masked out. Iftrue
, the regions in the shapefiles are masked out separately, generating an auxiliary dimension for the cube for this.ids
: by default,[]
, in this case all the shapes in the file will be used. If a list of IDs is provided, only the shapes matching them will be used. The IDs are assigned from thename
orid
attributes (in that order of priority) if present in the file or from the reading order if otherwise not present. So, for example, if a file has both`name
andid
attributes, the ids will be assigned fromname
. If the file only has theid
attribute, it will be taken from it and if noname
norid
attributes are present, an integer id starting from 1 will be assigned automatically when reading the shapes. We discourage to rely on this last behaviour as we can not assure that the reading order will be the same in different platforms, so we encourage you to modify the file to add a proper id attribute. If the file has an id attribute with a name that is not supported, please open an issue so we can add support for it.
- Examples:
Extract the shape of the river Elbe from a shapefile:
extract_shape: shapefile: Elbe.shp method: contains
Extract the shape of several countries:
extract_shape: shapefile: NaturalEarth/Countries/ne_110m_admin_0_countries.shp decomposed: True method: contains ids: - Spain - France - Italy - United Kingdom - Taiwan
See also esmvalcore.preprocessor.extract_shape
.
Extract a single point from the data. This is done using either nearest or linear interpolation.
Returns a cube with the extracted point(s), and with adjusted latitude and longitude coordinates (see below).
Multiple points can also be extracted, by supplying an array of latitude and/or longitude coordinates. The resulting point cube will match the respective latitude and longitude coordinate to those of the input coordinates. If the input coordinate is a scalar, the dimension will be missing in the output cube (that is, it will be a scalar).
If the point to be extracted has at least one of the coordinate point values outside the interval of the cube's same coordinate values, then no extrapolation will be performed, and the resulting extracted cube will have fully masked data.
- Parameters:
cube
: the input dataset cube.latitude
,longitude
: coordinates (as floating point values) of the point to be extracted. Either (or both) can also be an array of floating point values.scheme
: interpolation scheme: either'linear'
or'nearest'
. There is no default.
See also esmvalcore.preprocessor.extract_point
.
Extract a single point using a location name, with interpolation (either linear or nearest). This preprocessor extracts a single location point from a cube, according to the given interpolation scheme scheme
. The function retrieves the coordinates of the location and then calls the esmvalcore.preprocessor.extract_point
preprocessor. It can be used to locate cities and villages, but also mountains or other geographical locations.
Note
Note that this function's geolocator application needs a working internet connection.
- Parameters
cube
: the input dataset cube to extract a point from.location
: the reference location. Examples: 'mount everest', 'romania', 'new york, usa'. Raises ValueError if none supplied.scheme
: interpolation scheme.'linear'
or'nearest'
. There is no default, raises ValueError if none supplied.
See also esmvalcore.preprocessor.extract_location
.
The function calculates the zonal statistics by applying an operator along the longitude coordinate. This function takes one argument:
operator
: Which operation to apply: mean, std_dev, median, min, max, sum or rms.
See also esmvalcore.preprocessor.zonal_means
.
The function calculates the meridional statistics by applying an operator along the latitude coordinate. This function takes one argument:
operator
: Which operation to apply: mean, std_dev, median, min, max, sum or rms.
See also esmvalcore.preprocessor.meridional_means
.
This function calculates the average value over a region - weighted by the cell areas of the region. This function takes the argument, operator
: the name of the operation to apply.
This function can be used to apply several different operations in the horizontal plane: mean, standard deviation, median, variance, minimum, maximum and root mean square.
Note that this function is applied over the entire dataset. If only a specific region, depth layer or time period is required, then those regions need to be removed using other preprocessor operations in advance.
The optional fx_variables
argument specifies the fx variables that the user wishes to input to the function. More details on this are given in Fx
variables as cell measures or ancillary variables
.
See also esmvalcore.preprocessor.area_statistics
.
The _volume.py
module contains the following preprocessor functions:
axis_statistics
: Perform operations along a given axis.extract_volume
: Extract a specific depth range from a cube.volume_statistics
: Calculate the volume-weighted average.depth_integration
: Integrate over the depth dimension.extract_transect
: Extract data along a line of constant latitude or longitude.extract_trajectory
: Extract data along a specified trajectory.
Extract a specific range in the z-direction from a cube. This function takes two arguments, a minimum and a maximum (z_min
and z_max
, respectively) in the z-direction.
Note that this requires the requested z-coordinate range to be the same sign as the Iris cube. That is, if the cube has z-coordinate as negative, then z_min
and z_max
need to be negative numbers.
See also esmvalcore.preprocessor.extract_volume
.
This function calculates the volume-weighted average across three dimensions, but maintains the time dimension.
This function takes the argument: operator
, which defines the operation to apply over the volume.
No depth coordinate is required as this is determined by Iris. This function works best when the fx_variables
provide the cell volume. The optional fx_variables
argument specifies the fx variables that the user wishes to input to the function. More details on this are given in Fx variables as
cell measures or ancillary variables
.
See also esmvalcore.preprocessor.volume_statistics
.
This function operates over a given axis, and removes it from the output cube.
- Takes arguments:
- axis: direction over which the statistics will be performed. Possible values for the axis are 'x', 'y', 'z', 't'.
- operator: defines the operation to apply over the axis. Available operator are 'mean', 'median', 'std_dev', 'sum', 'variance', 'min', 'max', 'rms'.
Note
The coordinate associated to the axis over which the operation will be performed must be one-dimensional, as multidimensional coordinates are not supported in this preprocessor.
See also esmvalcore.preprocessor.axis_statistics
.
This function integrates over the depth dimension. This function does a weighted sum along the z-coordinate, and removes the z direction of the output cube. This preprocessor takes no arguments.
See also esmvalcore.preprocessor.depth_integration
.
This function extracts data along a line of constant latitude or longitude. This function takes two arguments, although only one is strictly required. The two arguments are latitude
and longitude
. One of these arguments needs to be set to a float, and the other can then be either ignored or set to a minimum or maximum value.
For example, if we set latitude to 0 N and leave longitude blank, it would produce a cube along the Equator. On the other hand, if we set latitude to 0 and then set longitude to [40., 100.]
this will produce a transect of the Equator in the Indian Ocean.
See also esmvalcore.preprocessor.extract_transect
.
This function extract data along a specified trajectory. The three arguments are: latitudes
, longitudes
and number of point needed for extrapolation number_points
.
If two points are provided, the number_points
argument is used to set a the number of places to extract between the two end points.
If more than two points are provided, then extract_trajectory
will produce a cube which has extrapolated the data of the cube to those points, and number_points
is not needed.
Note that this function uses the expensive interpolate
method from Iris.analysis.trajectory
, but it may be necessary for irregular grids.
See also esmvalcore.preprocessor.extract_trajectory
.
The _cycles.py
module contains the following preprocessor functions:
amplitude
: Extract the peak-to-peak amplitude of a cycle aggregated over specified coordinates.
This function extracts the peak-to-peak amplitude (maximum value minus minimum value) of a field aggregated over specified coordinates. Its only argument is coords
, which can either be a single coordinate (given as str
) or multiple coordinates (given as list
of str
). Usually, these coordinates refer to temporal categorised coordinates iris.coord_categorisation
like year, month, day of year, etc. For example, to extract the amplitude of the annual cycle for every single year in the data, use coords: year
; to extract the amplitude of the diurnal cycle for every single day in the data, use coords: [year, day_of_year]
.
See also esmvalcore.preprocessor.amplitude
.
The trend module contains the following preprocessor functions:
linear_trend
: Calculate linear trend along a specified coordinate.linear_trend_stderr
: Calculate standard error of linear trend along a specified coordinate.
This function calculates the linear trend of a dataset (defined as slope of an ordinary linear regression) along a specified coordinate. The only argument of this preprocessor is coordinate
(given as str
; default value is 'time'
).
See also esmvalcore.preprocessor.linear_trend
.
This function calculates the standard error of the linear trend of a dataset (defined as the standard error of the slope in an ordinary linear regression) along a specified coordinate. The only argument of this preprocessor is coordinate
(given as str
; default value is 'time'
). Note that the standard error is not identical to a confidence interval.
See also esmvalcore.preprocessor.linear_trend_stderr
.
ESMValTool also supports detrending along any dimension using the preprocessor function 'detrend'. This function has two parameters:
dimension
: dimension to apply detrend on. Default: "time"method
: It can belinear
orconstant
. Default:linear
If method is linear
, detrend will calculate the linear trend along the selected axis and subtract it to the data. For example, this can be used to remove the linear trend caused by climate change on some variables is selected dimension is time.
If method is constant
, detrend will compute the mean along that dimension and subtract it from the data
See also esmvalcore.preprocessor.detrend
.
Converting units is also supported. This is particularly useful in cases where different datasets might have different units, for example when comparing CMIP5 and CMIP6 variables where the units have changed or in case of observational datasets that are delivered in different units.
In these cases, having a unit conversion at the end of the processing will guarantee homogeneous input for the diagnostics.
Conversion is only supported between compatible units! In other words, converting temperature units from degC
to Kelvin
works fine, while changing units from kg
to m
will not work.
However, there are some well-defined exceptions from this rule in order to transform one quantity to another (physically related) quantity. These quantities are identified via their standard_name
and their units
(units convertible to the ones defined are also supported). For example, this enables conversions between precipitation fluxes measured in kg m-2 s-1
and precipitation rates measured in mm day-1
(and vice versa). Currently, the following special conversions are supported:
precipitation_flux
(kg m-2 s-1
) --lwe_precipitation_rate
(mm day-1
)
Hint
Names in the list correspond to standard_names
of the input data. Conversions are allowed from each quantity to any other quantity given in a bullet point. The corresponding target quantity is inferred from the desired target units. In addition, any other units convertible to the ones given are also supported (e.g., instead of mm day-1
, m s-1
is also supported).
Note
For the transformation between the different precipitation variables, a water density of 1000 kg m-3
is assumed.
See also esmvalcore.preprocessor.convert_units
.
This function can be used to weight data using the bounds from a given coordinate. The resulting cube will then have units given by cube_units * coordinate_units
.
For instance, if a variable has units such as X s-1
, using accumulate_coordinate
on the time coordinate would result on a cube where the data would be multiplied by the time bounds and the resulting units for the variable would be converted to X
. In this case, weighting the data with the time coordinate would allow to cancel the time units in the variable.
Note
The coordinate used to weight the data must be one-dimensional, as multidimensional coordinates are not supported in this preprocessor.
See also esmvalcore.preprocessor.accumulate_coordinate.
The bias module contains the following preprocessor functions:
bias
: Calculate absolute or relative biases with respect to a reference dataset
This function calculates biases with respect to a given reference dataset. For this, exactly one input dataset needs to be declared as reference_for_bias: true
in the recipe, e.g.,
datasets:
- {dataset: CanESM5, project: CMIP6, ensemble: r1i1p1f1, grid: gn}
- {dataset: CESM2, project: CMIP6, ensemble: r1i1p1f1, grid: gn}
- {dataset: MIROC6, project: CMIP6, ensemble: r1i1p1f1, grid: gn}
- {dataset: ERA-Interim, project: OBS6, tier: 3, type: reanaly, version: 1,
reference_for_bias: true}
In the example above, ERA-Interim is used as reference dataset for the bias calculation. For this preprocessor, all input datasets need to have identical dimensional coordinates. This can for example be ensured with the preprocessors esmvalcore.preprocessor.regrid
and/or esmvalcore.preprocessor.regrid_time
.
The bias
preprocessor supports 4 optional arguments:
bias_type
(str
, default:'absolute'
): Bias type that is calculated. Can be'absolute'
(i.e., calculate bias for dataset X and reference R as X − R) orrelative
(i.e, calculate bias as$\frac{X - R}{R}$ ).denominator_mask_threshold
(float
, default:1e-3
): Threshold to mask values close to zero in the denominator (i.e., the reference dataset) during the calculation of relative biases. All values in the reference dataset with absolute value less than the given threshold are masked out. This setting is ignored whenbias_type
is set to'absolute'
. Please note that for some variables with very small absolute values (e.g., carbon cycle fluxes, which are usually < 10 − 6 kg m − 2 s − 1) it is absolutely essential to change the default value in order to get reasonable results.keep_reference_dataset
(bool
, default:False
): IfTrue
, keep the reference dataset in the output. IfFalse
, drop the reference dataset.exclude
(list
ofstr
): Exclude specific datasets from this preprocessor. Note that this option is only available in the recipe, not when usingesmvalcore.preprocessor.bias
directly (e.g., in another python script). If the reference dataset has been excluded, an error is raised.
Example:
preprocessors:
preproc_bias:
bias:
bias_type: relative
denominator_mask_threshold: 1e-8
keep_reference_dataset: true
exclude: [CanESM2]
See also esmvalcore.preprocessor.bias
.
In the most general case, we can set upper limits on the maximum memory the analysis will require:
Ms = (R + N) x F_eff - F_eff
- when no multi-model analysis is performed;
Mm = (2R + N) x F_eff - 2F_eff
- when multi-model analysis is performed;
where
Ms
: maximum memory for non-multimodel moduleMm
: maximum memory for multi-model moduleR
: computational efficiency of module; R is typically 2-3N
: number of datasetsF_eff
: average size of data per dataset whereF_eff = e x f x F
wheree
is the factor that describes how lazy the data is (e = 1
for fully realized data) andf
describes how much the data was shrunk by the immediately previous module, e.g. time extraction, area selection or level extraction; note that for fix_dataf
relates only to the time extraction, if data is exact in time (no time selection)f = 1
for fix_data so for cases when we deal with a lot of datasetsR + N \approx N
, data is fully realized, assuming an average size of 1.5GB for 10 years of 3D netCDF data,N
datasets will require:
Ms = 1.5 x (N - 1)
GB
Mm = 1.5 x (N - 2)
GB
As a rule of thumb, the maximum required memory at a certain time for multi-model analysis could be estimated by multiplying the number of datasets by the average file size of all the datasets; this memory intake is high but also assumes that all data is fully realized in memory; this aspect will gradually change and the amount of realized data will decrease with the increase of dask
use.
Miscellaneous functions that do not belong to any of the other categories.
This function clips data values to a certain minimum, maximum or range. The function takes two arguments:
minimum
: Lower bound of range. Default:None
maximum
: Upper bound of range. Default:None
The example below shows how to set all values below zero to zero.
preprocessors:
clip:
minimum: 0
maximum: null