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The new EVLA correlator is extremely powerful in its spectral capabilities. Up to 4 million channels can be observed with a spectral resolution in the Hz regime. Here is a guide to access that spectral line power.

VLA spectral line guide

   Contents
   INTRODUCTION
   SYSTEM SPECIFICATIONS
       Receivers and IF System
       The Local Oscillator Chain
       The Correlator
           Total Number of Channels 
       Some Advanced Spectral Line Topics
           Creative Use Of The Spectral Line System
           High Accuracy Spectral Line Polarization Observations
           The Lag Spectrum, Gibbs Phenomenon and Hanning Smoothing 
       Continuum Observations in Line Mode 
   OBSERVATIONAL CONSIDERATIONS
       Amplitude and Phase Calibration
       Bandpass Calibration
       Continuum Subtraction
       Interference
       Bandwidth and Time Smearing
       Determining the Observing Frequency
           Doppler tracking and dopset
               Velocity Definition
               Summing Velocities
               Velocity Rest Frame 
           Running dopset
           Setting the LO Chain: loser 
       System Temperature Corrections
           Changes In T$_{sys}$ With Elevation (T$_{spill}$)
           Contributions to T$_{sys}$ From Strong Lines 
   REFERENCES
   Bandwidth and Number of Channels
       Normal Mode
       On-line Hanning Smoothing Option 


EVLA Spectral Line Observing

This guide is to help understand and setting up spectral line observations at the EVLA. The new, wide bandwidths of the EVLA allow users to observe up to 8GHz spectral bandwidth at a time. This will result in extreme continuum sensitivity. The EVLA sesntitivy of spectral lines, however, is almost the same as with the VLA. Where the EVLA capabilities really make the difference is in the number of channels and flexibility of the spectral line setups. The EVLA can

  • observe multiple lines at the same time
  • deliver continuous spectral coverage up to a full width 8GHz
  • access 1GHz or 2GHz chinks of each receiver band and place correlator subbands on it
  • use up to 64 subbands at a time which almost act like 64 independent correrlators, independently tunable, with different spectral bandwidths, different channel numbers, and different polarization product coverage
  • derive the frequency from the velocity of a line (Doppler Setting)
  • Dynamically schedule the observations to use the best weather conditions to high frequency, high scientific impact projects
  • Post-processing: The CASA package the main data reduction software for EVLA and ALMA and contains cutting edge data reduction code with continuum and spectral line processing being the main focus. The software and reference guides can be obtained on the CASA homepage and the CASAguides wiki contains guides on EVLA spectral line data reduction as well as some hints, tipes & tricks on using CASA and the visulaization tools, such as the casa viewer that are designed to display spectral data cubes

Line Rest Frequencies

There are a number of online tools available that help spectral line observers. To start with, the rest frequency of the sopectral line needs to be determined. This can be done with Splatalogue which contains data from the Lovas catalog, the JPL/NASA molecular database], the Cologne Database for Molecular Spectroscopy and others. Note that in addition to molecular line transitions, splatalogue also contains radio recombination lines.

Observing Frequency and Velocity Definitions

The first step is to determine the observing frequency of the spectral line. This is derived from the radial velocity of the source and the rest frequency of the spectral line.

A full relativistic calculation shows that the velocity is determined via . This is called the relativistic velocity. This equation is a bit cumbersome to use and in astronomy to different approximations are typically used instead:

  • Optical Velocity ( is the redshift of the source)
  • Radio Velocity

The radio and optical velocities are not identical. At low velocities that difference is small but and diverge more and more for large values.

At significant redshifts, it is possible to place the zero point of the velocity frame into the source via

The redshifted can now be used as the input rest frequency for the observations. The velocites that are derived based on such a redshifted rest frequency will then also be correctly scaled for the spread of the velocity scale that is due to the redshift.

Velocity Frames

The earth rotates, revolves around the sun, rotates around the galaxy, moves within the Local Group, and shows motion against the cosmic microwave background. If one measures a velocity is is therefore necessary to correct for such motions and define the frame to which the velocities are measured to.


There are various rest frames which might be appropriate. The following table lists their name, the motion for which one has to correct in order to reduce an observed velocity to that particular rest frame, and the magnitude of the velocity correction. Each subsequent rest frame is obtained by adding the effects of the preceding ones:

Rest Frame NameRest FrameCorrect forMax amplitude [km/s]
TopocentricTelescopeNothing0
GeocentricEarth CenterEarth rotation0.5
Earth-Moon BarycentricEarth+Moon center of massMotion around Earth+Moon center of mass0.013
HeliocentricCenter of the SunEarth oribtal motion30
BarycentricEarth+Sun center of massEarth+Sun center of mass0.012
Local Standard of Rest (LSR)Center of Mass of local starsSolar motion relative to nearby stars20
GalactocentricCenter of Milky WayMilky Way Rotation230
Local Group BarycentricLocal Group center of massMilky Way Motion100
VirgocentricCenter of the Local Virgo superclusterLocal Group motion300
Cosmic Microwave BackgroundCMBLocal Supercluster Motion600

The velocity frame should be chosen to what is appropriate for the science. Three frames are commonly used:

  • Topocentric this is the frame that the sky (observing frequency) uses. It is also the standard for visibilities in the measurement set
  • Local Standard of Rest is the native output of images in CASA. Note that there are two varieties of LSR: the kinematic LSR (LSRK) and the dynamic (LSRD) definitions for the kinematic and dynamic centers, respectively. The standard used in almost all cases is LSRK and most likely the older LSR naming is identical to the mode modern LSRK definition.
  • Barycentric is a common frame, too and has virtually replaced the older heliocentric standard. Given the small difference between them, they were frequently used interchangeably.

A full list of reference frames that CASA supports is provided in the CASA reference Manual and Cookbook and also on the casaguides.nrao.edu webpage The most commonly used rest frames are heliocentric (to be precise, barycentric is used at the VLA) and local standard of rest (LSR). LSR is generally used in Galactic astronomy and heliocentric in extragalactic astronomy, although the latter is often reduced to galactocentric.

Doppler Correction

A telescope operates typical at a fixed sky frequency (Topocentric velocity frame). Any spectral line will thus shift during a typical observation campaign. Within a single observation, the rotation of the earth dominates and the line may shift up to ~0.5 km/s (see above). observing campaigns that span longer times, may see spectral lines to shift in frequency by up to 30km/s due to the earth motion around the sun.

Side note: As a rule of thumb, 1 MHz in frequency corresponds to km/s for the line at a wavelegth of in mm. E.g. At a wavelength of 7mm, 1 MHz corresponds to about 7 km/s in velocity.

Using this rule of thumb, a line may shift about up to 5MHz in Q-band and up to 0.15MHz in L-band over the course of a year. This needs to be taken into account when setting up the observations. There are different ways to do this:

  • use the same sky frequency for all observations. The shift of the line is accommodated by a wide bandwidth that covers the line and its width at any time of the observation campaign. The data is later regridded in CASA to a common LSRK or BARY velocity frame. The sky frequency of an observation can be computed with the Dopset tool for a given time. One may find the LST dates on the EVLA Schedule Page.
  • calculate a different, but fixed sky frequency for each observation. This is called Doppler Setting and offered by OPT (currently only in OSRO mode). The line shift is then minimized to the rotation of the earth (0.5 km/s max). This small shift is corrected again by post processing.
  • change the sky frequency continuously to keep the line at the same position in the band. This is called Doppler tracking and was standard for the VLA. The EVLA does NOT support Doppler tracking. The WIDAR correlator offers enough bandwidth and spectral channels to cover any line shift and post-processing regridding needs. A non-variable sky frequency delivers also a more robust calibration and system stability.

The post-processing regridding of the line in CASA can be either done directly during imaging in the task clean, or alternatively with the task cvel. This will require that spectral features need to be sampled with at least 4 channels to be correctly reproduced.

Gibbs Phenomenon and Hanning smoothing

For very sharp features, a Fourier transform can prominently display a sinc function, a channel by channel fluctuation of the amplitude. If this is apparent in the data, smoothing adjacent channels will reduce or even eliminate the effect. The smoothing kernel to be used is a Hanning smoothing function which sports a triangular kernel with the central channel being weigthed by 0.5 and the two adjacent channels by 0.25. After Hanning smoothing, however, the channels are not independent anymore and one can eliminate every other channel without losing signal to noise.

In the VLA days, the correlator design could show the Gibbs phenomenon relatively prominently and frequently Hanning smoohting was applied online during the observations to accommodate for the effect and to save disk space. The Gibbs phenomenon is much less common for the EVLA due to a better correlator design of WIDAR. Only very strong maser or rfi sources may exhibit the typical "ringing" feature of the Gibbs phenomenon. In addition, data can be stored rather cheaply so there's no need for data size reduction via Hanning smoothing anymore. As a consequence, the EVLA does not support online Hanning smoothing. If Hanning smoothing is required, it has to be performed in post-processing, e.g. with the CASA task hanningsmooth.

Sensitivity Calculation

The sensitivity of spectral line data is best calculated with the EVLA exposure calculator. This JAVA tool allows you to enter sensitivity limits and provides the required time on source given a frequency, weather, weighting scheme, polarization products, and bandwidth of the observations. The Bandwidth should be the velocity of the resolution that is required to perform the science. This may or may not be the width of individual spectral channels. Overheads need to be added according to our EVLA frequently asked questions webpage. We like to refer to the low frequency guide and high frequency guide for further advise on how to set up the observations, depending on the receiver band to be used.

The WIDAR Correlator

The WIDAR correlator at the EVLA is very flexible and provides a number of setup options that are relevant for spectral line observing.

Basebands

Let's start with the basics: A signal from the telescope enters the WIDAR and during that path, it is passing analog filters that define the basebands. The basebands are actually baseband pairs to cover the L and R polarizations and are the most fundamental spectral ranges for any observations with WIDAR. In the 8-bit mode, WIDAR features two independably tuneable basebands (dubbed AC0 and BD0) with 1 GHz bandwidth each. Using the 3-bit samplers, there are 4 baseband pairs (A1C1, A2C2, B1D1, B2D2), each of them 2GHz wide.

As a second step, the basebands enter digital filters, 128MHz wide, the fixed 128MHz subbands.

WIDAR correlator baseband with subbands



Fixed 128MHz Subbands and 128 MHz "Suckouts"

After the analog filter that define the basebands, the signal enters the correlator and is split into fixed, 128MHz wide subbands. They are placed adjacently to cover the full width of the basebands. As each fixed 128MHz subband has some filter shape with soft corners, the sensitivity of the EVLA drops to about half its value between any two fixed 128MHz subbands. These frequency ranges are called "128 MHz Suckouts". There are a few options to account and interpolate over the suckouts:

  • Easiest method is to avoid them in your spectral setup. Try to set the baseband frequency in a way such that any interesting lines do not fall in the suckouts. We have a couple of tools that help, please check the spectral line section of the EVLA RSRO Observing Preparation Guidelines
  • Observe with two basebands shifted by 10-64MHz apart. This will ensure that at one of the baseband covers the suckouts of the other baseband with full sensitivity. An example is given in the figures. To get more channels, one can consider to use single polarizations on the basebands.


Baseband with 128MHz suckouts

rms noise in a blank field as a function of frequency for one baseband consisting of 8 contiguous sub-bands. Note the increased rms noise at the subband edges.


Shifted baseband setup to substitute suckout channels

rms noise in a blank field as a function of frequency for two basebands consisting of 8 contiguous sub-bands, where the basebands are separated by one-half of the subband width. Wherever signal in one baseband is compromised by edge effects, data from the other subband are substituted.

Narrow Subbands

For every baseband, there can be a maximum of 64 subbands. Fundamentally, each narrow subband can be between 128 MHz and 31.25 kHz wide and contains 64 channels when all four RR, LL, RL, LR polarization products are required (full polarization), 128 channel in dual polariation mode (RR & LL), and 216 channelf for single, RR or LL polarization products. The two tables below display the options and the corresponding velocity widths and channelizations:

  • Full polarization
Sub-band BW (MHz) Number of channels/poln product Channel width (kHz) Channel width (km/s at 1 GHz) Total velocity coverage per sub-band (km/s at 1 GHz)
128 64 2000 600/ν(GHz) 38,400/ν(GHz)
64 64 1000 300 19,200
32 64 500 150 9,600
16 64 250 75 4,800
8 64 125 37.5 2,400
4 64 62.5 19 1,200
2 64 31.25 9.4 600
1 64 15.625 4.7 300
0.5 64 7.813 2.3 150
0.25 64 3.906 1.2 75
0.125 64 1.953 0.59 37.5
0.0625 64 0.977 0.29 18.75
0.03125 64 0.488 0.15 9.375
  • Dual Polarization
Sub-band BW (MHz) Number of channels/poln product Channel width (kHz) Channel width (km/s at 1 GHz) Total velocity coverage (km/s at 1 GHz)
128 128 1000 300/ν(GHz) 38,400/ν(GHz)
64 128 500 150 19,200
32 128 250 75 9,600
16 128 125 37.5 4,800
8 128 62.5 19 2,400
4 128 31.25 9.4 1,200
2 128 15.625 4.7 600
1 128 7.813 2.3 300
0.5 128 3.906 1.2 150
0.25 128 1.953 0.59 75
0.125 128 0.977 0.29 37.5
0.0625 128 0.488 0.15 18.75
0.03125 128 0.244 0.073 9.375


WIDAR Tuning Restrictions

The baseband (pairs) cannot be entirely independently tuned. The following restrictions apply:

  • 3bit samplers can only be used in C-band or above, where the instantaneous frequency width of the receiver is larger than 2GHz.
  • In Ka band, only one baseband can be below 32GHz and that must be BD
  • The A1C1 baseband frequency can have a separation of max. 4GHz from the A2D2 baseband. B1D1 and B2D2 have the same restriction of 4GHz separation max.

For the narrow subbands:

  • Narrow subbands can not go across a 128MHz suckout frequency. Any narrow subband needs to be entirely within a 128MHx fixed subband.

(??? Michael to comment - what other restrictions are there ???)

Correlator Baselineboards

Correlator baselineboards (BlBs) are independent units that can be used for separate subbands. WIDAR has 64 BlB pairs (for the polarizations) and thus supports a maximum of 64 subbands.

Baselineboard Stacking

If not all 64 subbands are used, the remaining BlBs can be used to obtain more channels per subband. This method is called "baselineboard stacking" and each additional BlB for a subband adds another 64 channels in full and 128 channels in dual polarization modes. in OPT, this can be set via the BlB.BPS dropdown menu that is available for each subband. Baselineboard stacking is extremely useful as it allows to go to wider bandwidths in each subband but yet maintain a high number of channels. E.g. the full 2GHz bandwidth of the 8bit samplers can be covered by 16 128MHz subbands, each with 128 channels dual polarization as of the table above. The 16 subbands, however, only require 16 BlBs and another 48 are available for baselineboard stacking. One can thus use 4 BlBs for each subbands, quadrupling the number of channels from 128 to 512, or reducing the channel widths from 1MHz to 0.25 MHz over the full 2 GHz frequency range. This method works for any subband bandwidth essentially providng a very high spectral resolution for smaller subbands.

Recirculation

Another way to get more spectral channels for a given subband is called "recirculation". Recirculation uses the fact that the correlator has more computing capability when the data averaged in time. The basic correlator dump time is 1s. If this is doubled to 2s, WIDAR can produce twice as many channels as listed in the tables above. 4s would allow 4 times the number of channels. This setup, however, is not available right now in OPT and EVLA staff needs to be contacted.

Data Rate Limits

Baselineboard stacking, recirculation, and time resolution, however, can add up to an extremely high data rate in the correlator. The EVLA currently supports data rates of up to 75MB/s. The OPT instrument configuration calculates them based on the spectral line setup and the limit of 65 MB/s should not be exceeded.

Planning and Setup

The Proposal Submission Tool (PST)

Setting up a Spectral Observation using the Observation Preparation Tool (OPT)

The Observation Preparation Tool (OPT) is the web-based interface to create scheduling blocks (SBs) for the EVLA. An SB is a block of time during an observation is run. A full project may constitute of several SBs. To access the OPT, go to my.nrao.edu and click on the Obs Prep tab, followed by Login to the Observation Preparation Tool. You may need to register at my.nrao.edu if you do not yet have an account. Please also read the OPT webpage that contains the latest information on the OPT as well as a comprehensive OPT manual.


Frequency Setup

One of the most important parts of the setup is to chose the appropriate frequency setup for WIDAR. In the OPT, click on the Instument Configuration tab. The most advanced setting is currently the RSRO setting (File -> Create New -> RSRO Configuration). This opens a page for the frequecnsy setup as shown in the figures.

  • Enter a name and select the receiver in the top panel. This will adjust the available frequency range described below the drop down menu. The 1dB and 3dB ranges describe the roll-off behaviour of the receiver sensitivity at the edges. If the frequency to be observed is close to the edges of the receiver, one may check if the next higher or lower frequency receiver is more suitable
  • Baseband Tuning: Select the position of the basebands. For the 8bit samplers, one can choose 2 basebands, each with a width of 1GHz. The center frequencies will go into the AOCO box for frequency 1 and into the B0D0 box for frequency 2. For 3bit samplers, one can choose 4 basebands, each 2 GHz wide. Here the center frequencies need to placed into the A1C1, A2C2, B1D1, and B2D2 boxes. A1C1 and A2C2 cannot be more than 4GHz apart, and the same restrictions apply to B1D1 and B2D2. Note that additional freqeuny restrictions may apply and the OPT/ICT will issue a clear warning or error message for those cases. The graphical panel above the input boxes shows the position of the two or four basebands. They are displayed as pairs to accommodate the R and L polarization inputs that may later be converted into single, dual, or full polarization products.
  • Integration Time: this defines how data is dumped from the correlator backend into data files. A larger integration time will reduce the data volume. In addition, larger values can be chosen to take advantage of recirculation. On the other hand, time smearing effects, rfi excision, or time resolution may demand smaller integration times. It is important though, to not exceed the maximum data rate of 75 MB/s and the integration time parameter is a good way to stay below this threshold for observations that demand large number of spectral channels.
  • The total data rates are displayed in the Configuration Summary. The same panel also shows the number of baseline boards that are used in the setup. Remember that a maximum of 64 baseline boards are available. During commissioning, it is advisable to not use all baseline boards, in case that a couple of them are being worked on. Also remember that the maximum supported data rate is currently 75MB/s. If you require higher data rates, please contact NRAO staff.
  • Subband Setup: Depending on the baseband setup, the Subband Configuration panel sports tabs for each of the basebands selected. Under each tab one can now select the individual subbands. Up to 64 subbands are available: click Add subband to create a subband setting, where one can select the frequency range from a "Sky Range" drop-down menu. The Offset Freq from Center shows the placement of the subband with respect to the baseband center. For small bandwidths, the drop-down menu is not available as there are too many choices and the placement needs to be entered by hand in the Offset Freq from Center box. Currently, the subbands are not independently tuneable yet (it is under commissioning) and the subbands will snap on a frequency grid defined by the subband bandwidth. Now select the number of polarization products and the number of channels will be displayed in the Spectral Points box. The comments box can be used to describe the setup, e.g. by entering the transitions that should afll in that subband. Those entries are not used anywhere outside OPT (??? rest frequencies for OSRO ???). The delete button removes the subband if is is no longer required, and Bulk Edit is used for bulk editing of many subbands (see the OPT guide on this feature). Note: if you chose subbands with different bandwidths, contact NRAO staff as the script currently need manual editing after OPT submission
  • If not all subbands are used, one can use the remaining baseline boards to obtain a higher spectral resolution for those in the Subband Configuration panel. Select a higher number in the BL.BPS drop-down panel. During commissioning, we recommend to use 2,4,8, etc. BlBs here but in principle any of the options in the drop down menu should work.
  • Recirculation: please contact NRAO staff if you need this setup
  • Independently tuning the subbands: Please contact NRAO staff for this feature


OPT - Instrument Configuration: Baseband Settings


OPT - Instrument Configuration: Subband Settings

Doppler Setting

Doppler setting will calculate the sky frequency of your observation, based on the time of the observation, the velocity, position and rest frequency of a source and line. Contradictory to to Doppler tracking, Doppler setting calculates this once for each baseband at the start of the observation and the frequency will stay the same for the entire run of the SB. Every subsequent run of the SB will perform a recalculation of the sky frequency. Doppler setting is currently only supported in OSRO mode, RSRO observers need to calculate their own sky frequency (which is usually not too difficult given that the movement of the earth shifts the line by max. 30 km/s over a year, 0.5 km/s over a day - a velocity range that can under almost any circumstances be accommodated for by the wide bandwidths of WIDAR). To use, first select Rest in the baseband frequency setup section of the OPT/ICT. All velocities will then be calculated against the center baseband frequency which may or may not be the rest frequency of your spectral line. Supply the reference position (a source from a catalog can be chosen, typically this will be your target source) and the velocity with their frames in the Doppler Setting section in the OPT/ICT. In the future this feature may be available for each subband separately but for now it will shift the baseband frequency and shift all subbands along with it.

Bandpass Setup

All observations with the EVLA - even those with the goal of observing continuum - require bandpass calibration. A bandpass calibrator should be bright enough, or observed long enough, so that the bandpass calibration does not significantly contribute to the noise in the image. This implies that, for a bandpass calibrator with flux density Scal observed for a time tcal and a science target with flux density Sobj observed for a time tobj, should be greater than . How many times greater will be determined by one's science goals and the practicalities of the observations, but should be greater by at least a factor of two. For extremely narrow channels or very weak bandpass calibrators, those typical flux requirements can lead to extremely large integration times. As an alternative one may then chose to interpolate in frequency, or to fit a polynomial across all channels in post-processing (bandtype=BPOLY in CASA's bandpass task.


The bandpass calibrator should also be a point source or have a well-known model. At low frequencies, the absolute flux density calibrators (3C48, 3C147, or 3C286) are quite bright and in many cases can double as the bandpass calibrator. However, at high frequencies, these sources have only moderate flux densities of ~0.5-3 Jy, translating into a potentially noisy bandpass solution.

The stability of bandpasses as a function of time is of concern for high-dynamic-range spectral work. We have found that most antennas show bandpasses that are stable to a few (~2-4) parts in a thousand over a period of several (~4-8) hours.

Dramatic jumps in the bandpass structure (of order a few parts in a hundred) can occur at attenuator changes. The observer can track down such attenuator changes in their data using the switched power information; the On - Off power ('PDIF' in AIPS) will show a clear discontinuity. For this reason, it behooves the spectral line observer to observe a bandpass calibrator at least twice during their observations. Multiple observations will provide a check that all is well on most antennas and a mechanism for identifying any "problem" antennas. However, we do not expect that interpolating in time between consecutive bandpass solutions will bear much fruit for the observer. The low-level variations observed on some antennas tend to not be smooth functions of time and will likely not be corrected with interpolation.

If there is only one observation of the bandpass calibrator, the observer should be careful to minimize the number of shadowed antennas, as an antenna without a bandpass determined for it will essentially be flagged for the rest of the observation.

We have shown that one can transfer the bandpass from a wide subband onto a narrow subband if the wide bandpass frequency range covers that narrow one. This may be good to the per cent level. But we advise to use that option only when absolutely necessary.

Phase/Complex Gain Calibration

The complex gain (phase/gain) calibration is the same for a spectral line observation as for any other observation. Ideally one should stick with the correlator setup for the target and the complex gain calibrator. For weak calibrators, however, it is possible to use wider bandwidths for the phase calibrator and then transfer the phases to the source. For that to work, both the narrow and wide subbands need to be at exactly the same center frequency. Different centers will introduce a phase offset between them. (??? check with Vivek ???)

Continuum Subtraction

The continuum of an observation can be either subtracted in the uv plane (uvcontsub in CASA) or in the image domain (imcontsub). In most cases, the uv-domain is preferred but for high dynamic range imaging, or imaging close or beyond the edge of the FWHM of the primary beam, it may be advisable to subtract the continuum using line-free channels in the image cube. Both methods have in common that the continuum can only be determined accurately when enough line-free channels are observed that are necessary to derive a good model of the continuum. If a the continuum sources exhibit significant spectral slope or even curvature, it is advisable to go to even larger bandwidth covering more line-free frequency space and to sample the continuum with many channels to ensure that a reasonable higher-order fit can be obtained and subtracted from the line+continuum data.


High Dynamic Range Imaging

For very strong and narrow spectral features (typically thousands of Jy srong sources), one may see the Gibbs phenomenon (ringing) and Hanning smoothing may need to be applied (see above). This needs to be done in post-processing. The effect, however, can be reduced by using a higher spectral resolution such that the ringing effects beat against each other, effectively reduce the zig-zag pattern that appears on alternating, neighboring channels when the peak is within a single spectral channel.

Zeeman Observing

please contact NRAO local staff if you plan to perform Zeeman observations. This mode is currently in the commissioning phase.

Spectral Line Observing

Current->Revised OSS Guidelines

  • An Overview of the EVLA

(last paragraph) The EVLA correlator will be extremely powerful and flexible. Details of the correlator configurations being offered for EVLA early science during the period Sep 2011 - Dec 012 (a full D→A configuration cycle) are described in Correlator Configurations. It is important to realise that the EVLA correlator is fundamentally a spectral line correlator. The days of separate “continuum” and “spectral line” modes of the VLA correlator are over, and all observations with the EVLA will be “spectral line.” This has implications for how observations are set up, and users who may be used to continuum observing with the VLA are strongly advised to consult Correlator Configurations.

  • Limitations on Imaging Performance

(Sidelobes from Strong Sources) An extension of the previous section is to very strong sources located anywhere in the sky, such as the Sun (especially when a flare is active), or when observing with a few tens of degrees of the very strong sources Cygnus A and Casseopeia A. Image degradation is especially notable at lower frequencies, shorter configurations, and when using narrow-bandwidth observations (especially in spectral line work) where chromatic aberration cannot be utilized to reduce the disturbances. In general, the only relief is to include the disturbing sources in the imaging, or to observe when these objects are not in the viewable hemisphere.

  • Correlator Configurations

All observations with the EVLA correlator should be treated as traditional VLA spectral line observations, in that they will require observation of a bandpass calibrator. They may also require observation of a delay calibrator. Users should contact NRAO staff for advice on setting up observations with the EVLA correlator.

Post-Processing Guidelines

please see our extensive EVLA turoials on the CASAguides wiki for examples of how to process EVLA spectra line data.