Chapter 3
The Dynamic Iterative Map-Maker Explained

 3.1 How it works
 3.2 The reduction step-by-step
 3.3 The individual models
 3.4 Stopping criteria
 3.5 Masking
  3.5.1 AST Masking
  3.5.2 FLT Masking
  3.5.3 COM Masking
 3.6 Skipping the AST model
 3.7 Specialised configuration files
  3.7.1 dimmconfig_jsa_generic.lis
  3.7.2 dimmconfig_blank_field.lis
  3.7.3 dimmconfig_bright_compact.lis
  3.7.4 dimmconfig_bright_extended.lis
 3.8 Configuration files for solving specific problems

The Dynamic Iterative Map-Maker, hereafter just referred to as the map-maker is the tool you will use to produce SCUBA-2 maps, and is implemented by the Smurf makemap command. It performs all pre-processing steps to clean the data, followed by solving for multiple signal components using an iterative algorithm, and binning the resulting time-series data to produce a final science map.

The makemap command can be invoked in two ways: 1) directly by typing “makemap” in response to a unix shell prompt (see Chapter 5), or 2) indirectly as part of an ORAC-DR recipe (see Chapter 4).

This chapter describes how the map-maker produces a science image from raw SCUBA-2 data. It should be considered essential reading as it provides an understanding of how your reduced image was produced. This is particularly true if you wish to modify the default map-maker parameters. If you prefer to jump straight in to the data reduction go to Chapter 4.

3.1 How it works

The map-maker works by producing individual models of the various components that make up the signal recorded by each bolometer, one component being the required astronomical signal. It models and removes each of the other components in order of decreasing magnitude, ultimately leaving just the astronomical signal plus residual noise. The modelled components are listed in Table 3.1 and described more fully in Section 3.3.

A configuration file should usually be supplied when running makemap directly. This file holds a set of parameter values that control all aspects of the map-maker, including details of the pre-processing steps, which model components to include, parameters that control the determination of each model, and the stopping (or convergence) criteria. If no configuration file is supplied when running makemap1, a set of default parameter values will be used. There are a great number of these parameters, but fortunately not all of them are of interest to the typical user. Appendix H documents the parameters you are more likely to find of interest, including the default value that is assigned to each parameter if you do not give it a value in your configuration file. For a full list of all available parameters, see the appendix “Configuration Parameters” within SUN/258.

It is possible to create a map without supplying a configuration file to makemap (i.e. leaving all configuration parameters set to their default values—“config=def”—when running makemap) but it is not recommeneded since it will not give optimal results for your particular observation. For this reason, specialised configuration files have been developed which are tailored to different science goals, be they detecting faint galaxies or mapping large molecular clouds. A description of these specialised configuration files can be found in Section 3.7.

Note, when using the pipeline to create a map, rather than running makemap directly, the pipeline will always use a configuration file—one of the standard configuration files will be selected if none is specified by you.

3.2 The reduction step-by-step

This section describes the basic map-making process used by the default configuration. It may be modified in many ways by supplying a configuration file containing alternative parameter values.

Figure 3.1 shows the flow chart of the basic map-making process. It is divided into two sections: the pre-processing stage where the data are cleaned, then the iterative stage where the different models are subtracted, a sky map created and the convergence checked.

Initial cleaning and down-sampling
The separate raw data files are first concatenated into a single time series for each sub-array (if possible—see Data Chunking) and have the flat-field from the associated fast-flat scans applied to calibrate the bolometers. This resulting time-series are in units of pW.

These time-series are then re-sampled at a rate that matches the requested pixel size—the equivalent to applying a low-pass filter. Down-sampling saves time and memory usage when running the map-maker, without losing any significant information. The degree of down-sampling applied depends on how fast the telescope was moving during the observation, the requested pixel size. In general, slower scans will be more heavily down-sampled than faster scans, and fast scans may not be down-sampled at all.

A number of cleaning steps are then run: bolometers that have unusually high noise levels are identified and excluded from further processing, any sudden steps in the base-line of each bolometer are identified and corrected, and a polynomial estimate of the base-line is removed from each bolometer.

Iterative steps

Next comes the iterative stage. In each iteration, estimates are produced for each model component. These are removed from the cleaned time-series data and the remaining data values are binned into a map. However, in general, the presence of astronomical signal within the original time series will have upset the estimates of the COM, GAI and FLT models, causing the final map to be inaccurate. But now that we have a map (albeit an inaccurate map), we can sample the map at the position of each bolometer value to get an estimate of the astronomical component within the original time-series data. We then remove this astronomical signal from the original time-series data and re-estimate the models. These new model estimates should be more accurate since they are not so heavily influenced by the astronomical signal. In turn, this allows us to create a more accurate map. We repeat this process until the map does not change significantly with further iterations. Whilst not mathematically rigorous, we expect the process to converge because the astronomical signal is in general much smaller than any of the other components and so each iteration introduces a very small fractional change in the model estimates.

Within each iteration, the first components to be modelled and removed are COM and GAI, which work together to calculate and remove the average signal template of all bolometers, allowing each bolometer to have an arbitrary gain and offset. In addition, the GAI model will flag as unusable any bolometer in which the signal looks very different to the common-mode.

The next model (EXT) applies a multiplicative extinction correction to the data. Following this, the FLT model filters each bolometer time-stream independently to remove low frequencies that correspond to angular scales larger than 600 arc-sec and 300 arc-sec at 450μm and 850μm, respectively.

After these models have been removed, the AST model (i.e. the estimate of the astronomical signal) produced by the previous iteration, is added back onto the remaining time-series data2, and the new values are binned up on the sky to produce a new estimate of the final science map. Since many samples typically contribute to the estimate of the signal in a given pixel, the noise is greatly reduced compared with the time-series data. The variance of each map pixel value is determined from the spread of sample values that contribute to the pixel. The value of this map at the position of each bolometer sample is then found. This forms the new AST model which is removed from the time-streams, leaving just the residual noise.

The NOI model then measures the noise in the residual signals for each bolometer to establish weights for the data as they are placed into the map in subsequent iterations. This is only done on the first iteration. Subsequent iterations re-use the weights established on the first iteration.

Checking convergence

Convergence is checked against the parameters detailed in the configuration file. Convergence is achieved either when the requested number of iterations has been completed, or when the mean change in the map pixel values is less than a specified fraction of a standard deviation (see parameter maptol). If more iterations are required or (in the latter case) the map is still changing significantly, all the model—except for AST—are added back onto the residuals, thus reconstructing the original time-series but without the astronomical signal. This is the signal upon which the model estimates will be based on the next iteration.


Figure 3.1: A flow chart illustrating the dynamic iterative map-maker. Note that for each iteration the AST model is subtracted from the time-series leaving only those contributions to be fitted and removed.

For full details of the map-maker see Chapin et al. (2013) [5].

Model Description

COM Common-mode signal
GAI Gains that scale each bolometer to the common-mode
EXT Extinction correction
FLT Filter that removes low frequencies
AST Astronomical signal
NOI Residual noise

Table 3.1: Table adopted from Chapin et al. (2013). A detailed explanation of each model is given in Section 3.3.

Data Chunking
Chunking occurs when there is insufficient computer memory available for the map-maker to process all the time-series data together, or when there is a gap in the data (e.g. from a missing sub-scan). In these cases, the map-maker divides up the time-series data into a number of “chunks” and produces a map from each chunk independently, before re-combining all the maps at a later stage to create the final map. Ideally you want your data reduced in a single chunk, however this can be unfeasible for large maps.

The more data the map-maker processes at once, the better chance it has of determining the difference between sky signal and background noise.

Information about chunking can be obtained in several ways:

In daisy mode chunking is less of a concern as the entire map area is covered many times in the space of a single observation.

For pong maps chunking is a bigger concern, with the maximum number of chunks that can be tolerated dependent on the number of map rotations. For example, a 40-minute pong map with eight rotations may get divided into three or four chunks. Although not ideal, this will mean that each point is still covered by two or three passes. Fewer passes than this however and the map-maker become less effective.

Be aware that focus observations are intentionally dis-contiguous. If you attempt to make a map from a focus observation, it will be processed in several chunks no matter how much memory your computer has.

3.3 The individual models

The list of models to be evaluated (and removed) by the map-maker, and the order in which they are used during the iterative stage, is given by the modelorder parameter in the configuration file. These models are modular however, so their order may be changed. The default model order is given below.

  modelorder = (com,gai,ext,flt,ast,noi)

The only configuration file not following this model order is the one tailored for blank field maps which does not include a FLT model in the iterative stage but instead includes an equivalent high-pass filter as part of the cleaning stage (see Section 3.7).

Below is an introduction to each model. More complete descriptions of the models and all the associated caveats can be found in Chapin et al. (2013) [5]. Details of each model are controlled by a set of configuration parameters that begin with the name of the model. For instance, all parameters related to the COM model will be of the form “”.



The COM model removes the common-mode signal (the signal that is common to all bolometers), the dominant contributor to this signal being the sky noise. It determines this by simply averaging over all bolometers for each time slice. Bolometers are flagged as bad, (and thus omitted from the final map), if they do not resemble the COM model seen by the majority of the other bolometers.

Extended emission on a scale larger than the array footprint on the sky will contribute a signal indistinguishable from a common-mode signal. This puts an upper limit on the spatial scale of astronomical emission that can be recovered.


GAI model works with COM in removing the common-mode signal. GAI consists of a time-varying scale and offset for each bolometer, which scales the COM model so that it resembles the original bolometer data as closely as possible. It is the scaled version of COM that is removed from the bolometer time-series. In addition, the GAI model identifies any bolometers that looks very different to the common-mode signal, and flags them as unusable.


EXT applies the extinction correction. This is a time-varying scaling factor that is derived from the JCMT water-vapour radiometer. As it deals with 30-second chunks of data, this accounts for varying conditions over a long observation. For more details see Appendix B.


The FLT model acts on the Fourier transform of the bolometer data. High-pass (only allows higher frequencies to pass) and low-pass (only allows lower frequencies to pass) filters can be specified. These cut-off frequencies can either be specified directly in Hz, or as an angular spatial scale in arc-seconds that is subsequently converted into a frequency using the speed at which the telescope is moving. The most important role of this model is to apply a high-pass filter in order to remove the low frequency 1/f noise. Note that extended emission varies slowly over the array; it therefore appears at low frequencies and complicates the choice of a high-pass filter. A further discussion of this matter is given in Section 7.2.


The AST model is generated in conjunction with a science map. Hence, the position of AST in the model order indicates at what stage the astronomical image should be estimated. When the AST model is calculated, the first step is bin the residual time-series data into a map (using nearest-neighbour sampling). Following this, the map is projected back into the time domain (i.e. sampled at the position of every bolometer sample) and removed as the AST model.


NOI should come last in the model order and calculates the RMS noise level in each bolometer. It is only calculated on the first iteration. The same noise levels are then used on all subsequent iterations to weight the bolometer values when binning them into a map. Each bolometer may have a single noise estimate that remains fixed over the whole observation, or may have multiple noise levels, each of which relate to a different part of the observation. See parameters noi.box_size and noi.box_type.

Examples of the time traces for a single bolometer from these models is shown in Figure 3.2. These traces cover a subset of an observation of the secondary calibrator CRL 2688. You can clearly see the dominance of the COM model which is removed first. The FLT model stores the data removed by the high-pass filter. In the AST model, CRL 2688 is clearly seen as positive spikes which appear when the bolometer passes over the source. Finally, the residual signal stored in RES is flat, indicating that most of the signal has been successfully accounted for by the other model components.

3.4 Stopping criteria

The map-maker will stop processing either when the requested number of iterations has been completed OR when the convergence criterion specified in the configuration file is reached.

Option 1: Fixed number of iterations

Specifying the number of iterations in the configuration file is done via the numiter parameter. This is shown below for dimmconfig_jsa_generic.lis.

  numiter = -25

A positive value for numiter means that the requested number of iterations will be executed. A negative value, as in the example above, indicates that no more than this number of iterations should be performed, but that it may stop at fewer if convergence (according to the noise criterion below) has been achieved.

Option 2: Convergence parameter

The convergence criterion is set by the maptol parameter.

When running the map-maker, maptol gives the average normalised change in the value of map pixels between subsequent iterations. Convergence is reached when the mean change across all pixels is less than the parameter maptol. It has units of the noise in the map, thus maptol =0.05 means a mean change in pixel value of <0.05 σ. This option has the advantage of directly assessing the noise in the resulting map.

The map-maker displays the normalised change in pixel values between iterations at the end of each iteration. This value typically drops rapidly to begin with and then flattens out, decreasing increasingly slowly. The printed values can be inspected to check convergence is proceeding as expected. Be aware that setting maptol to much lower than 0.05 will dramatically increase the length of time needed to produce the final map, and may possibly result in convergence never being achieved.

If you wish to perform further checks on the progress of convergence while running the map-maker, you can use the itermap option. This causes the map created by each iteration to be dumped to disk for inspection (see Section 6).


Figure 3.2: These plots show some of the models for a single bolometer, for part of an observation of CRL 2688. From top to bottom: the COM model containing signal common to all bolometers, the FLT model containing residual low-frequency noise missed by COM, the AST model with the astronomical signal showing as a positive spike when this bolometer passes over the source, and the RES model looking (as expected) like white noise.

3.5 Masking

The term masking refers to the inclusion or exclusion of selected bolometer samples from the estimate of specific models, based on the positions of those samples within the output map. Masking can be applied independently to the AST, FLT and COM models, as described in the later sub-sections within this section.

A mask is a selection of pixels within the output map. Normally these pixels form one or more contiguous regions that enclose the areas where significant sub-mm emission is expected (the “source” regions). Pixels outside this mask are referred to as “background pixels”. The use to which such masks are put differs from model to model as described later in model-specific sub-sections.

Masks fall into two broad categories:

Static masks are appropriate in cases where the areas containing significant sub-mm emission are known in advance. If this is not the case, then the mask needs to be based on evidence within the maps created at the end of each iteration, resulting in the masks evolving from iteration to iteration as the maps converge towards the final solution. Such dynamic masks have a potential problem in that they can upset the convergence process by introducing extra flexibility into the algorithm. For this reason, an option is provided to freeze these masks after a fixed number of iterations3 (e.g. see ast.zero_freeze) and this is used within the specialist configuration file dimmconfig_fix_convergence described in Section 3.8.

Each of the three models—AST, FLT and COM —have an equivalent set of parameters to specify the masking (if any) that should be used. Each set starts with the model name, followed by a dot, followed by the parameter name. To enable masking, one or more of these parameters needs to be set to a suitable value to define a mask, as described below.

Static masks can be defined either as circles of specified radius, centred on the source position (suitable for compact sources—see for instance ast.zero_circle), or by an external image that uses special pixel values to indicate the source regions and the background regions (suitable for extended sources—see for instance ast.zero_mask). Within such “external masks” all background pixels should be set to the Starlink bad value (see “Bad-pixel Masking” in SUN/95). Pixels with any other value are treated as source pixels. Section 6.6 describes some ways in which external masks can be generated.

Dynamic masks can be defined in several different ways:

By applying a simple threshold on the S/N ratio within the map created at the end of each iteration (e.g. see ast.zero_snr).
By applying a simple threshold on the S/N ratio as above, and then extending the resulting source regions down to a lower S/N value (e.g. see ast.zero_snrlo). This allows a low S/N threshold to be used (which can sometimes help to avoid negative bowling around the edges of extended sources) without introducing lots of isolated pixels into the mask because of noise spikes in the map.
By applying a threshold on the number of bolometer samples falling in each map pixel (e.g. see ast.zero_lowhits). Because of the scanning strategy used with SCUBA-2 (see Section 2.2), pixels near the edge of the map will receive fewer bolometer samples than those near the centre, and will therefore be noisier. Thus this scheme allows the noisy edges of the map to be masked out. Whilst this is technically a dynamic mask—because the number of samples falling in each pixel could potentially change from iteration to iteration—in fact a mask based on hits per pixel will usually only change very slightly from iteration to iteration.
By using an algorithm that automatically identifies features of a given size in the map, similar to that used by the Kappa ffclean command (e.g. see ast.zero_snr_ffclean). This can be a useful alternative to simple S/N thresholding in cases where bright artificial large-scale structures appear in the map. Such structures will result in artificially large source regions in a simple S/N mask, which may in turn cause the artificial structures to become even brighter and larger in subsequent iterations. Using an ffclean-based mask instead will restrict the mask to the brighter astronomical cores on top of such artificial large-scale structures.

Multiple masks can be used by selecting the appropriate configuration parameters as described above. Whether the combined mask represents the union or intersection of the individual masks is selected using the parameters ast.zero_union, flt.zero_union and com.zero_union. By default, the union is used.

The masks used on the last iteration are stored in the Quality component of the NDF containing the output map. A separate bit of the quality component is used for each model (AST, FLT or COM) that is being masked. These bits can be viewed in various ways—see Section 8.6 and Section 5.3.2.

Be aware that the S/N ratio within individual map pixels depends on pixel size—larger pixels will have higher S/N ratios than small pixels. Therefore masks based on a specific S/N threshold will grow or shrink in area as a function of pixel size. As a rough rule, if you double the pixel size, you should also double the S/N thresholds to get a mask that covers a similar area of the sky.

3.5.1 AST Masking

The iterative map-maker algorithm described earlier in this chapter divides each cleaned bolometer value into four additive parts:

The common-mode signal (COM).
The low frequency background drift in each bolometer (FLT).
The astronomical signal (AST).
The left-over residual noise (RES).

Whilst the value of each model is constrained to some extent by the manner in which the model is calculated, there remains a large degree of degeneracy in the algorithm. In other words, there are many different ways in which each bolometer value can be divided up into the four values listed above. For instance, any arbitrary change in the AST model can be accommodated provided that equal and opposite changes are introduced into the other model values so that the total value of all four components remains the same.

The degeneracy between COM and AST is particularly problematic, since it allows large scale features to appear in the map (on the scale of the sub-array footprint) that are corrected for by equal and opposite features in the COM model. Such features can appear as gradients or “saddles” across the final map.

The purpose of masking the AST model is to apply an extra constraint to the system to help break this degeneracy, and so avoid these large-scale features. It functions by forcing the AST model to zero at the end of each iteration for all samples that fall outside the masked area on the sky (i.e. samples that fall in the “background” areas of the map). Forcing the AST model to zero in this way means that the COM model is more closely constrained.

Whilst this constraint is applied only in the background regions, its effects are also felt part way into the source region because of the way in which the COM model averages over a sub-array footprint. Thus source regions that are much larger than a sub-array will still suffer from the degeneracy between COM and AST, allowing arbitrary large-scale background features to develop within the region, but these features will become weaker as the edges of the mask are approached.

In order to avoid the final map containing zero values in the background region, it is necessary to avoid using AST-masking on the final iteration. For this reason, by default one further iteration is performed—without AST-masking—once the basic iterative algorithm has converged (see ast.zero_notlast).

All the configuration files supplied with Smurf use AST masking, with the exception of dimmconfig_blank_field.

3.5.2 FLT Masking

The FLT model estimates and removes a low frequency background from each bolometer time-stream. To do this it uses an FFT-based high-pass filter. Ringing around sudden transients—such as astronomical sources — is a natural consequence of all such filters, resulting in alternating bright and dark rings around sources in the map. In most cases, the iterative nature of the map-making algorithm eventually results in the rings reducing to a much lower level, as more of the astronomical signal is removed from the time stream on each iteration, causing the ring-inducing transients to become weaker. However, this is not always completely effective, and also slows down convergence.

For these reasons, it is often helpful to mask the FLT model. This causes each bolometer time stream to be blanked out as the bolometer passes over the source regions in the mask. Such blanked sections are replaced by linear interpolation between the data on either side of the blanked section. The effect of this is to remove the transients that cause the ringing in the FLT model, and thus get a better estimate of the low frequency background in each bolometer.

Such masking is most useful at the start of the iterative process, before the bulk of the astronomical signal has been removed from the time-streams. Indeed, if it is allowed to continue for too many iterations it can cause its own problems that tend to slow down convergence. For this reason, if FLT masking is used, it is (by default) limited to two iterations—see flt.zero_niter.

A difficulty with FLT masking is that the FLT model is evaluated before the map is made on each iteration. This means that when the FLT model is evaluated on the first iteration, there is no map available. This is not a problem if a static mask is used, but if a dynamic mask is used, then it is not possible to calculate the FLT mask on the first iteration (subsequent iterations will create the mask on the basis of the map created at the end of the previous iteration). This is a shame since FLT masking is most beneficial on the first few iterations, whilst the bulk of the astronomical signal is still present in the time streams. A scheme to get round this problem is described in Section 3.6.

All the configuration files supplied with Smurf use FLT masking, with the exception of dimmconfig_blank_field.

3.5.3 COM Masking

The value of the COM model at a specific time-slice is the mean of all remaining bolometer values at that time slice. If the COM model is masked, bolometer samples that fall within the source regions defined by the mask are excluded from this mean, thus removing the bias introduced into the mean by bright astronomical sources. This results in the COM model more accurately representing the varying common-mode background value at each time slice. This can help to reduce negative bowling around sources in the map, and can help to reduce the amount of data that is rejected as being too poorly correlated with the common-mode signal.

COM masking has the same difficulty as FLT masking in that the COM model is evaluated before the map is made on each iteration, and so it is difficult to use dynamic masks with COM masking. However, the solution described in Section 3.6 can be used for COM masking as for FLT masking.

Currently, none of the configuration files supplied with Smurf use COM masking.

3.6 Skipping the AST model

As discussed in Section 3.5, FLT masking is most effective on the early iterations (particularly the first iteration). This is because the bulk of the astronomical signal is still present in the time streams and is likely to cause bad ringing if FLT masking is not used. However, since the FLT model is evaluated before the map is made within each iteration, there is no map available to use as the basis for a FLT mask on the very first iteration.

One way to get round this is simply to use a static mask that does not require a map to be available. However, this may not be possible, particularly for extended sources where no a-priori knowledge of the source areas in the sub-mm may be available.

Another scheme is provided by the ast.skip configuration parameter. If ast.skip is set to a positive integer N, the subtraction of the AST model from the time-series that normally occurs at the end of each iteration is not performed on the first N iterations. This means that for the first N iterations, the time-series data remain unchanged, and consequently the models and the resulting map are unchanged. Of itself, this does nothing useful—it merely delays the first useful iteration. However, when combined with FLT masking, it can be very beneficial because it allows a mask to be created before the first “real” iteration occurs (i.e. the first iteration that subtracts off the AST model). This means that the first “real” map will have far less ringing around bright sources than would otherwise be the case. This in turn means that far fewer iterations are required to correct this ringing.

It is also possible to use ast.skip with COM masking, but the benefits are not so noticeable as for FLT masking.

The default value for ast.skip is zero, but the dimmconfig_bright_extended and dimmconfig_jsa_generic configuration files supplied with Smurf both set ast.skip = 5 (and also use FLT masking).

3.7 Specialised configuration files

Maps made by the pipe-line using the REDUCE_SCAN recipe will use dimmconfig_jsa_generic.lis unless some alternative configuration has been specified. This configuration file is intended to provide a reasonably good map for all types of observations. However, compromises have been made to reach that balance, the main one being that some real extended structure is sacrificed in order to avoid introducing artificial large scale structures.

Whilst dimmconfig_jsa_generic.lis is always a good place to start, you will want to follow this up with a specialised configuration that will suit your observation. A few specialised configuration files are supplied with Smurf and can be found in $STARLINK_DIR/share/smurf/.

Note, any parameter for which no value is specified within the supplied configuration will take on the default value listed in Appendix H.

Below is a description of each of the specialised configuration files. The tables following each description list the parameters set by each file. The files themselves are stored in $STARLINK_DIR/share/smurf/—they are simple text files and so can be inspected easily.

3.7.1 dimmconfig_jsa_generic.lis

The dimmconfig_jsa_generic configuration file is designed to handle all science data. This is a good configuration file to start with if you are unsure how to proceed with your data reduction. You may notice that elements of this configuration are common to the other specialised configuration files.

This configuration is optimised to suppress the creation of artificial large scale structure within the final map. Consequently, some real extended emission may be lost if this configuration is used. This goal is achieved by:

Setting flt.filt_edge_largescale) to 200 arc-seconds so that the FLT model uses a heavier than normal filter.
Setting com.perarray to 1, indicating that four separate COM models should be used, one for each sub-array4.
Using a mask to force the AST model to zero in the background regions after each iteration (see parameters ast.zero_snr and ast.zero_snrlo—also see Section 3.5.1).

In addition the S/N threshold for DC steps (dcthresh) is relaxed from 25 in the default file to 100 to avoid problems bright sources triggering the step detection algorithm.

The other major feature of this configuration is that the subtraction of the AST model is skipped on the first five iterations. In conjunction with the use of FLT masking, this helps to speed up convergence and minimise dark rings around bright source (see Section 3.6.


ast.skip = 5

ast.zero_snrlo = 3

ast.zero_snr = 5

com.perarray = 1

dcthresh = 100

flt.filt_edge_largescale = 200

flt.zero_snrlo = 3

flt.zero_snr = 5

maptol = 0.01

numiter = -25

noisecliphigh = 10.0

3.7.2 dimmconfig_blank_field.lis

The dimmconfig_blank_field configuration is tuned for blank field surveys for which the goal is to detect extremely low signal-to-noise point sources within otherwise blank fields.

Applying a high-pass filter (FLT) on each iteration can result in convergence problems when there is little or no signal in the map. Instead, a single, harsher high-pass filter is applied as a pre-processing step (corresponding to 200-arc-sec scales at both 450 μm and 850 μm). There are also more conservative cuts to remove noisy/problematic bolometers. Only 4 (positive) iterations are requested as there is no signal to confuse to models.

The option com.perarray = 1 requires the COM model to be fit to each sub-array independently. This improves the overall fit but with the loss of any structure on scales larger than a single sub-array—not an issue for blank fields.

Figure 3.3 shows the sharp contrast in the output map between reducing data with the default configuration file and using dimmconfig_blank_field.lis.

Blank-field maps commonly have a matched filter applied as part of the post-processing to aid source detection (see Section 8.7), however this is not applied by the map-maker.

pict pict
Figure 3.3: Maps of a deep cosmology field reduced with (left) default parameter values (i.e. no configuration file) and (right) dimmconfig_blank_field.lis



numiter = 4

flt_edge_largescale = 200

spikethresh = 10

modelorder = (com,ext,ast,noi)

com.perarray = 1

3.7.3 dimmconfig_bright_compact.lis

The dimmconfig_bright_compact configuration should be used for producing maps of bright, isolated compact sources that are positioned at the centre of the map (e.g. calibrators).

The addition of the ast.zero_circle parameter is used to constrain the map to zero beyond a radius of 1 arc-min from the source centre (see Section 3.5.1). This strategy helps with map convergence significantly, and can provide good maps of bright sources, even in cases where scan patterns failed to complete in full.

com.perarray is set to 1 indicating that a COM model should be fit separately for each sub-array. This is not advised for extended sources as signal on scales larger than a single sub-array is lost, but is fine for a compact central source. Likewise, the filtering is tighter. The S/N threshold for DC steps (dcthresh) is relaxed from 25 in the default file to 100 to avoid problems associated with bright sources.

The values of the parameters controlling the COM model are modified to relax the test that compares each bolometer to the common mode. This is because the algorithm that compares each bolometer to the common-mode can be fooled by a bright compact source passing across individual bolometers. Likewise the test for DC steps within each bolometer baseline is also relaxed (parameter dcthresh).


numiter = -40

flt.filt_edge_largescale = 200

com.perarray = 1

flt.zero_circle = (0.016666)

ast.zero_circle = (0.0166666666)

noisecliphigh = 10.0

dcthresh = 100

com.corr_tol = 7

com.gain_tol = 7

com.gain_abstol = 5

3.7.4 dimmconfig_bright_extended.lis

pict pict
Figure 3.4: A region towards the Galactic Centre reduced with (left) default parameter values (i.e. no configuration file) (right) dimmconfig_bright_extended.lis.

The dimmconfig_bright_extended configuration is for reducing maps that contain emission that is extended to some degree and contains some bright regions. Here ast.zero_snr is used to constrain the AST model to zero wherever the S/N is lower than 5σ (see Section 3.5.1). numiter has been raised to -40, as more iterations are required to maximise the sensitivity to large dynamic signal ranges in the map.

The other major feature of this configuration is that the subtraction of the AST model is skipped on the first five iterations. In conjunction with the use of FLT masking, this helps to speed up convergence and minimise dark bowls around bright source (see Section 3.6.

Figure 3.4 shows a comparison between maps reduced with the default configuration file and using dimmconfig_bright_extended.lis; the most noticeable difference is the improvement in the bowling around strong sources.


numiter = -40

flt.filt_edge_largescale = 480

ast.zero_snr = 3

ast.zero_snrlo = 2

ast.skip = 5

flt.zero_snr = 5

flt.zero_snrlo = 3

3.8 Configuration files for solving specific problems

Two additional configuration files are available that can be used to supplement your configuration file in order to solve specific problems:

These files provide a few additional settings that should be added to some other configuration in order to achieve the desired fix. For instance, a configuration file containing the following two lines would indicate that values from both dimmconfig_bright_extended.lis and dimmconfig_fix_blobs.lis should be used:


This reads a set of configuration parameter from the dimmconfig_bright_extended.lis file, and then assigns new values for just those parameters defined in dimmconfig_fix_blobs.lis. These values override the values specified in dimmconfig_bright_extended.lis.

The parameters in these files are discussed further Chapter 6.

1i.e. you include “config=def” on the makemap command line.

2This step is omitted on the first iteration since no estimate of AST has yet been created.

3Although by default masks are never frozen.

4By default, a single COM model is used that represents the mean data value across all four sub-arrays.