Issue 
A&A
Volume 517, July 2010



Article Number  A70  
Number of page(s)  9  
Section  Astronomical instrumentation  
DOI  https://doi.org/10.1051/00046361/200913803  
Published online  10 August 2010 
Atmospheric turbulence in phasereferenced and widefield interferometric images
Application to the Square Kilometre Array
I. MartíVidal^{1,2}  J. C. Guirado^{2}  S. JiménezMonferrer^{2}  J. M. Marcaide^{2}
1  MaxPlanckInstitut für Radiastronomie, Auf dem Hügel 69, 53121 Bonn, Germany
2 
Dpt. Astronomia i Astrofísica, Universitat de València, Dr. Moliner 50,
46100 Burjassot, Spain
Received 3 December 2009 / Accepted 2 April 2010
Abstract
Phase referencing is a standard calibration procedure in radio
interferometry. It allows us to detect weak sources by using
quasisimultaneous observations of closeby sources acting as
calibrators. However, atmospheric turbulence may introduce strong
differences in the optical paths of the signals of the target and
calibrator and affect, or even waste, phase referencing in cases
of relatively large calibratortotarget separations and/or bad
weather. The situation is similar in widefield interferometric
observations. We present the results of a Monte Carlo study
of the astrometric precision and sensitivity of an interferometric
array (a realization of the Square Kilometre Array, SKA) in
phasereferenced and widefield observations. These simulations can be
extrapolated to other arrays by applying the corresponding corrections.
We consider several effects from the turbulent atmosphere
(i.e., ionosphere and wet component of the troposphere) and also
from the antenna receivers. We study the changes in dynamic range and
astrometric precision as a function of observing frequency, source
separation, and strength of the turbulence. We find that, for
frequencies between 1 and 10 GHz, it is possible to
obtain images with high fidelity, although the atmosphere strongly
limits the sensitivity of the instrument compared to the case with no
atmosphere. Outside this frequency window, the dynamic range of the
images and the accuracy of the source positions decrease. We also find
that, even if a good model of the atmospheric turbulence (with an
accuracy of 99%) is used in the imaging, residual effects from the
turbulence can still limit the dynamic ranges of deep,
highcontrast (
10^{5}10^{6}), images.
Key words: atmospheric effects  techniques: high angular resolution  techniques: interferometric  telescopes
1 Introduction
It is wellknown that groundbased astronomical observations are affected by the atmosphere. Changes in the atmospheric opacity produce a bias in the source flux density, while changes in the refraction index distort the shape of the electromagnetic frontwave of the source. This distortion translates into a deformation of the observed source structure and/or a variation in the relative positions of all sources observed in a given field. For astronomical devices based on interferometry, atmospheric effects can be accurately modelled if the atmosphere above each element of the interferometer (hereafter, station) remains unchanged over the whole portion of the sky being observed. In these cases, the observed visibilities can be calibrated using stationbased algorithms, which are relatively simple and computationally inexpensive (e.g. Readhead & Wilkinson 1978).
Figure 1: Array distribution used in our simulations (empty and filled squares). Axes are relative longitude (horizontal axis) and latitude (vertical axis) in km. Left, the whole array. Center, a zoom into the core. Right, a zoom into the inner core. The stations marked with empty squares were removed from the array in a second run of our simulations, to check the dependence of the results on different array distributions (see text). 

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However, when the spatial variations in the atmosphere are significant within the observed portion of the sky, as happens if there is atmospheric turbulence, the opacity and dispersive effects cannot be modelled as a single timedependent stationbased complex gain over the field of view. Unless more complicated calibration algorithms are used (e.g., van der Tol 2007), the effects of these errors on the image are difficult to correct. In this paper, we study the effects that a turbulent atmosphere may introduce in interferometric observations. We focus our study on the effects produced by turbulence in the dynamic range and astrometric accuracy after a phasereferenced calibration between a strong (calibrator) source and a weak source, located a few degrees away. This study is numerically equivalent to the study of the deformation of a widefield interferometric image at any point located at a given distance from the center of the field (i.e., the phase center of the image). In both cases, the phases introduced by the atmosphere in the signal of each antenna for the different pointing directions are the same, so the effects of the atmosphere in Fourier space (and therefore on the sky plane) will also be the same.
The results reported here are an extended version of those previously reported in the SKA memo by MartíVidal et al. (2009). In the next section, we describe the details of the array distribution used, as well as the characteristics of the simulated observations. In Sect. 3, we describe how the noise from the atmosphere and the receivers was added to the visibilities and in Sect. 4 describe the procedures followed in our Monte Carlo analysis. In Sect. 5, we present the main results obtained; in Sect. 6, we summarize our conclusions.
2 Array geometry and sensitivity
We simulated an interferometric array similar to the planned station distribution of the Square Kilometre Array (SKA). We simulated a total of 200 stations distributed in the following way: 50% are randomly distributed within a circle of 5 km radius (inner core); 25% are distributed outside this circle out to a distance of 150 km (core), following 5 equiangular spiral arms; the remaining antennae are distributed following the same spiral arms, but out to a distance of 3000 km from the inner core. This array distribution is similar to that used in Vir Lal, Lobanov & JiménezMonferrer (2009). The curvature of the Earth surface was taken into account in our simulations. We show the resulting array distribution in Fig. 1. We also repeated all the simulations reported here, but after subtracting a subset of 100 (randomly selected) stations from the array, to check the sensitivity of the main conclusions of this paper to different array distributions (see Appendix A). In Fig. 1, we also show the modified array after subtracting the 100 stations.
2.1 Sensitivity and bandwidth
We simulated interferometric observations using 16 different frequencies, spanning logarithmic bins from 150 MHz to 24 GHz. This is the theoretical frequency window of the SKA. According to Jones (2004), the maximum observing bandwidth of the SKA will be around 25% of the central observing frequency (up to a maximum bandwidth of 4 GHz for all frequencies above 16 GHz). This (maximum) frequencydependent bandwidth translates in our simulations into a changing sensitivity of the SKA as a function of frequency.
The sensitivities of the simulated stations were also chosen to be similar to those of the SKA, which were taken from Jones (2004). These values are set for an elevation of 45 degrees and differ from those given in Schilizzi et al. (2007), but the use of the values given in Schilizzi et al. (2007), instead, does not affect the main conclusions of this paper. We interpolated the sensitivities given in Table 1 of Jones (2004) to the frequencies used in our simulations. In Fig. 2, we show the station sensitivities used.
Figure 2: Station sensitivities (i.e., effective areas over system temperatures) used in our simulations. 

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2.2 Source position
We set the target source coordinates to be those of the zenith of the array center and the calibrator to an hour angle of 0 degrees, also with respect to the array center. This positioning of the sources minimizes the optical paths of the signals through the atmosphere (since both, source and calibrator, are at maximum elevations), thus enhancing the quality of the phasereferenced observations. The results given in this paper should be interpreted by taking this into account.
If the source were located far from the zenith, the mapping function of the tropospheric delay and the finite width of the ionosphere would increase the effect of turbulence on the phasereferenced visibilities of the target. In addition, the uv coverage of the interferometer would have shorter projected baselines in declination, thus decreasing the synthesized resolution in declination. Therefore, placing the sources at maximum elevations is a key limiting factor of the simulations reported here, especially if they are to be compared to real observations.
3 Noise model
We simulated phasereferencing observations in the following way: we assumed that the calibrator source is sufficiently strong to allow for a perfect antennagain calibration at its location; we then determined the image of the target source by computing the differential antennagain errors expected at the target location. Therefore, under the effect of atmospheric turbulence, these results depend on the calibratortotarget separation.
We implemented two kinds of atmospheric turbulence. The first
turbulence was associated with the ionosphere (the free electron
content, which introduces dispersion in the radiation) and the other
turbulence was associated with the wet troposphere (the water
vapour, close to the Earth surface, which is not in a state of
thermodynamic equilibrium). The effect of ionospheric turbulence on the
signal phase varies as ,
affecting the lowfrequency observations; the effect of the wet troposphere on the phase varies as ,
affecting the highfrequency observations. The dry troposphere (which
is more homogeneously distributed over each station than the wet
troposphere) was not considered in our simulations, since it can be
easily modelled and removed from the data to a level lower than the
effects coming from the water vapour and the ionosphere. Models of the
turbulence from the ionosphere and troposphere can be found in many
publications (e.g., Thomson et al. 1991).
Here, suffices to say that this turbulence follows a Kolmogorov
distribution. This distribution has a phase structure function
given by
(1) 
where is the phase added by the turbulent screen to the signal of a source located at . The brackets <...> represent averaging over all pointing directions located at a distance from the point at . The Kolmogorov distribution is fractallike, so both the ionosphere and wet troposphere have essentially the same phase distribution, despite a global scaling factor between them.
The global factors for both distributions (ionosphere and troposphere) were computed according to the typical values of ionospheric and tropospheric conditions. For the ionosphere, the Fried length (i.e., distance in the ionosphere for which the structure function rises to 1 rad^{2}) was set to be 3 km at 100 MHz. For the wet troposphere, we set the parameter C^{2}_{n} L (i.e., the integral of the profile of C^{2}_{n} along the zenith direction) to be 10^{11} m^{1/3} (see Eq. (13.100) and Table 13.2 of Thomson et al. 1991); this value translates into a Fried length of 3 km for a frequency of GHz. Since the Kolmogorov distribution is selfsimilar, it is possible to adapt the results here reported to any other atmospheric conditions (see Sect. 5.3), by scaling accordingly the source separation to the Fried length of the ionosphere (for lowfrequency observations) or the wet troposphere (for highfrequency observations). We note that the selfsimilarity of the tropospheric turbulence does not apply on very large scales (the typical baseline lengths in VLBI observations), since there is a saturation in the power spectrum of the distribution (see, e.g., Thomson et al. 1991). However, this is not important to our analysis, since we did not use the absolute phase of the signal coming from a given direction in the sky, but computed the differential effects at each station from two different (closeby) directions, which depend on shortscale turbulence. Therefore, the saturation of tropospheric turbulence on large scales does not affect our results.
Figure 3: Example of a turbulent phase screen with Kolmogorov statistics. The grey scale shows variations in opticalpath phases, normalized between 1 and 1 radians. The final values of the phases depend (given the selfsimilarity of the distribution) on a global factor related to the observing frequency and the ionospheric and/or wet tropospheric conditions. 

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We computed the differential effects from the turbulent atmosphere in two ways. For the antennas of the core (within the central 300 km), we generated synthetic phase screens for the ionosphere and troposphere. We show an example of one such screen in Fig. 3. We notice that this figure could represent either ionospheric or tropospheric turbulence in our modelling, just by scaling the screen by the corresponding factor. Two different screens were generated in each Monte Carlo simulation. The screen for simulating the ionosphere was placed at at a height of 300 km and the screen for simulating the troposphere at a height of 5 km. For the antennas out of the core, we computed the term separately. We proceeded in this way (i.e., we generated a phase screen only for the core antennas, thus without generating a much larger screen for the whole array), because the distances between stations outside the core are large enough to ensure that the crosscorrelation of turbulence above different stations is negligible compared to the correlation between turbulence on the calibrator and turbulence on the target source at the same station. This numerical strategy also accelerated our simulations.
We note that we did not introduce any time evolution in the turbulent phase screens in our simulations. Any evolution of the turbulence could dramatically affect the observations if the acquisition times were longer than the coherence time of the signal, which depends on the evolution of the turbulence and the observing frequency. However, for snapshotlike observations, of the order of a fraction of a minute or so, we could consider, as a good first approximation, a constant turbulence phase screen.
Noise from the receivers was added to our model by generating a
random Gaussian noise in both the real and imaginary parts of the
visibilities. The mean deviation, ,
of the Gaussian noise added to the visibilities was (e.g., Thomson et al. 1991, Eq. (6.43)):
(2) 
where k is the Boltzmann constant, is the relative loss of signal caused by the correlator quantization (we used ), is the observing bandwidth, is the observing time, and S_{A} is the sensitivity of the stations (collecting area over system temperature, shown in Fig. 2).
4 Estimate of dynamic range and astrometric precision
We simulated different sets of phasereferenced observations. In all cases, the observations were snapshots of duration t_{0} = 60 s. Longer observing times, t, would, in principle, increase the dynamic ranges and astrometric precisions shown in all the following sections as , as long as the changing atmosphere (and, therefore, the changing source positions and shapes) did not introduce important smearing effects in the images after the combination of all visibilities.
In our first series of simulations, we generated visibilities of targets with flux densities of 0.1, 1, and 10 Jy for a separation of 5 degrees between target and calibrator. A total of 1500 simulations were performed for each flux density and frequency. We used such a large separation between calibrator and target, because these simulations of phasereferenced observations can also be applied to the study of deformations of widefield images affected by a turbulent atmosphere.
In a second series of simulations, we studied the effects of the atmosphere as a function of calibratortotarget separation. We simulated 1500 observations at 1420 MHz (i.e., the hydrogen line) of a source with 1 Jy for different separations from the calibrator (26 degrees).
In a third run of simulations, we used only one Kolmogorov screen (which can represent either ionospheric or tropospheric turbulence, depending on the observing frequency) with different Fried lengths, to study the scalability of the simulations for different source separations and/or atmospheric conditions.
In all these simulations, we added the noise from both the atmosphere and the receivers. For each simulated phasereference image, obtained by applying uniform weighting to the visibilities, the brightness peak was found and the corresponding point source was subtracted from the visibilities. To subtract the point source, the brightness peak was shifted to the phase center of the image by multiplying the visibilities by the corresponding planewave factor in Fourier space. The flux density of the point source was then estimated to be the average of the real part of the resulting visibilities, and the resulting pointsource model was subtracted from the data. Afterwards, a Fourier inversion of the new visibilities produced an image of the residuals, from which the rootmeansquare (rms) of all the pixels was computed. On the one hand, the deviation of the brightness peak from the image center was assumed to be the astrometry error in that image. On the other hand, the source peak divided by the rms of the residuals was taken to be the dynamic range. In Fig. 4, we show the distribution of astrometric deviations and dynamic ranges for the case of a target source of 1 Jy observed at 1420 MHz (which corresponds to an interferometric beam of 13 mas) located at 5 degrees from the calibrator. When the distributions such as those shown in Fig. 4 were obtained, we computed the standard deviation in the astrometric corrections and the mean value of dynamic ranges for each source flux density, frequency, and separation. The first quantity was our estimate of the astrometric uncertainty, and the second quantity was an estimate of the achievable dynamic range.
Figure 4: Distribution of right ascension shifts a) and dynamic ranges b) of 1500 snapshot phasereferenced images, simulated at 1420 MHz, for a 1 Jy target source located at 5 deg from its calibrator. The calibrator source is located at an hour angle of 0 and the target source is located at the zenith of the array center. 

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5 Results
5.1 Observing frequency and signal decoherence
If the atmospheric turbulence is not taken into account and only the noise from the receivers is added to the visibilities, our simulations reproduce the dynamic ranges given by Eq. (6.53) of Thomson et al. (1991), as expected. In addition, the noise from the receivers does not introduce considerable changes in the source position of the phasereferenced images (changes of the order of 10 as or lower).
When the turbulent ionosphere and wet troposphere are added to the simulations, the dynamic range of the images is notably affected, especially at low ( ) and high ( ) frequencies. In Fig. 5, we show phasereferenced images of a 1 Jy source, located 5 deg. from its calibrator, observed at 0.5, 5, and 15 GHz. It can be readily seen that the inclusion of effects from the atmospheric turbulence produces an important extra noise in the images at 0.5 and 15 GHz, but not at 5 GHz.
Figure 5: Simulated phasereference images of a 1 Jy source located at 5 deg from its calibrator. Noise from the receiving system (top) and, additionally, noise due to the turbulent atmosphere (bottom) have been added to the visibilities. 

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Following the algorithm described in Sect. 4, we obtained the astrometric uncertainties and dynamic ranges shown in Fig. 6. At very low frequencies (below 500 MHz), the ionosphere prevents a clear and precise detection of all sources, regardless of their flux densities. At higher frequencies, the astrometric uncertainty decreases notably (mainly because of the dependence of ionospheric effects on ) and is limited only by diffraction and sensitivity between 1 and 10 GHz (this frequency window depends slightly on the source flux density, as can be seen in the figure). For higher frequencies, the wet troposphere begins to affect the astrometric uncertainty, which increases to around 10 mas at the highest frequencies. We find that the highest astrometric accuracy, at least for reasonably welldetected sources, is achieved for frequencies around 4 GHz. This is where the ionospheric and (wet) tropospheric components are roughly equal.
Figure 6: Astrometric accuracy a) and dynamic range b) as a function of frequency, in the case of atmospheric turbulence and a separation of 5 degrees between calibrator and target. The calibrator source is located at an hour angle of 0 and the target source is located at the zenith of the array center. Different lines correspond to different target source flux densities (10 Jy, continuous line; 1 Jy, dashed line; 0.1 Jy, dotted line). 

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The dynamic range of the phasereferenced images is limited
considerably by the atmosphere. When the atmosphere adds noise to the
visibility phases, an additional rms is added to the residual images,
which depends on the visibility amplitudes, thus limiting the
achievable dynamic range regardless of the flux density of the source.
That is, when the source flux density is higher, the noise of
the image is also higher. This limitation is, of course, more
important for the brightest sources. In our case, the brightest
source has a flux density of 10 Jy. For this source, the maximum dynamic range achieved is only 110, which is times
smaller than the dynamic range that would be obtained without the
atmosphere. This situation can also be understood in another way. The
rms of the final image can be divided into two components, which are
added in quadrature. One component,
,
comes from the receiver noise and is independent of the source flux density. The other component,
,
comes from the atmospheric refraction and is equal to a percentage of the source flux density (
,
where S is the source flux density and
depends on the atmospheric refraction). Hence, the dynamic range, D, is
For high flux densities ( ), the achievable dynamic range will saturate to a value that depends on the atmospheric conditions (i.e., ) and is independent of both the source flux density and the sensitivity of the stations. As seen in Fig. 6, despite the large difference between the simulated flux densities (1 and 10 Jy), the dynamic range saturates to a value of 100.
5.2 Angular separation and signal decoherence
The results shown in the previous subsection correspond to a
separation of 5 degrees between source and calibrator. These
results change when the angular separation changes. We computed
astrometric uncertainties and dynamic ranges for a source with a flux
densitity of 1 Jy
located at 26 degrees from its calibrator. Noise from the
atmosphere and the receivers was taken into account in these
simulations. We used an observing frequency of 1420 MHz
(the hydrogen line) which is inside the frequency window where the
atmospheric effects are minimised. Therefore, all the astrometric
errors derived were small (of the order of a few mas), allowing us
to use image sizes small enough to sample the beam with more pixels (30 pixels) using a grid of 1024
1024 pixels. This fine gridding of the beam allowed us to determine the location of the image
peak more accurately and, therefore, obtain a more precise estimate of the astrometric error. The
results obtained are shown in Fig. 7.
In that figure, we also plot two analytical (phenomenological) models
for the estimate of the increase in astrometric uncertainty and the
loss of dynamic range (i.e., degree of signal decoherence) as a
function of angular separation. On the one hand, the phenomenological
model proposed for the estimate of loss of dynamic range is
where D is the dynamic range, is the angular separation between target and calibrator, D_{0} is the dynamic range without atmosphere (i.e., when the calibratortotarget separation, , tends to 0), and k and are two parameters related to the atmospheric conditions, source flux density, and observing frequency. This equation is just Eq. (3), but setting .
As can be seen, this model agrees well with the simulations. We obtain 10^{5} deg and 0.06.
Figure 7: Effects of targettocalibrator separation in the quality of the phasereference images. Dots: simulated astrometric accuracy a) and dynamic range b) for observations at 1420 MHz and a target flux density of 1 Jy. Lines: proposed phenomenological models. 

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On the other hand, the proposed phenomenological model for the increase in the astrometric uncertainty is
where is the astrometric uncertainty, is the diffraction limit (i.e., half the size of the beam), and k' and are two parameters also related to the atmospheric conditions, source flux density, and observing frequency. We fit k' = 0.57 0.04 deg and 0.05. From a different approach to treat the noise from the atmosphere limited to VLBA and EVN arrays, Pradel et al. (2006) obtained a similar dependence of with .
We note that when we change D_{0} by D in Eq. (5), the newly fitted k' and are 1.03 0.09 and 0.07 0.06, respectively. This new value of is compatible with zero. In other words, the diffraction limit divided by the dynamic range of the image is an excellent estimator of the astrometric uncertainty, at least for the range of simulated calibratortotarget separations at 1.4 GHz (which falls within the frequency window where the atmospheric effects are minimized).
For calibratortotarget separations larger than 6 degrees, the situation changes. We simulated phasereferenced images for calibratortotarget separations of up to 12 degrees, and found that the model of dynamic range given by Eq. (4) remains valid, but the astrometric uncertainty increases more rapidly, with = 2.38 0.08 ( , if we change D_{0} by D in Eq. (4)). This last reproduces the astrometric uncertainties well for large source separations, but the fit is poorer for separations smaller than 56 degrees.
5.3 Scalability of the results and use of turbulence models in the data calibration
In the previous subsections, we have reported the effects of
atmospheric turbulence in phasereferenced (and widefield)
interferometric images using fixed values for the Fried lengths of the
Kolmogorov distributions of the ionosphere and wet troposphere. Since
the Kolmogorov distribution is selfsimilar, the results presented
can be scaled and adapted to other atmospheric conditions. These
simulations can also be used to estimate the limiting dynamic range and
astrometric uncertainty if an a priori model of the tropospheric
and/or ionospheric turbulence is used in the imaging. In these
cases, the effective Fried length,
,
to compare to our simulations can be estimated to be
(6) 
where r_{0} is the Fried length of the real turbulence and the other factor is related to the fractional precision of the turbulence model, is the phase computed from the turbulence model at a given point in the sky and is that corresponding to the real turbulence, and the brackets <...> represent averaging over the field of view. If the a priori model of the ionospheric electron distribution is accurate to a given precision level, the effective Fried length to use for the ionosphere will be that corresponding to the residual turbulence (i.e., the difference between the model and the real turbulence). For instance, a model of the ionospheric electron content with a 99% accuracy, has an effective Fried length of ; if the accuracy increases to 99.9%, . In Fig. 8, we show , the maximum dynamic range (i.e., for a source with an infinite flux density, so in Eq. (3)) as a function of parameter , which we define as
Figure 8: Maximum dynamic range as a function of (see Eq. (7)) and for a 1scan snapshot of 60 s. 

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where h is the height of the phase screen and
is the calibratortotarget separation
(or half the size of the widefield image). Equation (7) can be used with Fig. 8
to compute the maximum achievable dynamic range for many different
combinations of source separations, atmospheric conditions, and
observing frequencies (
for the ionosphere and
for the trosposphere). We note, however, that Fig. 8
has been generated using only one Kolmogorov screen, so it is
applicable to ionospheric dispersion (for low frequencies) or
tropospheric dispersion (for high frequencies), but not to a situation
where ionospheric and tropospheric effects are similar. In these cases,
and as a first approximation, we could set
(8) 
where and are the (effective) Fried lengths of the ionosphere and troposphere, respectively, and and are the heights of each phase screen. Also shown in Fig. 8 is the fitting model
where D_{1} = 48.38 0.10 and 0.002. Figure 8 illustrates how difficult is to obtain a highcontrast image with a wideangle coverage at very low (or high) frequencies. For instance, an image of 10 10 degrees with a dynamic range of 10^{6} at a frequency of 500 MHz (which translates into 10^{5}) would require, for the ionospheric screen used in the previous subsections, a model of the ionospheric turbulence distribution with an uncertainty lower than 3 10^{5} (observing time of 1 min). If the observing time increases to 10 h, the minimum required uncertainty in the model of the ionosphere would increase to 7 10^{4}, but such a high precision has to be maintained during the whole set of observations. If the dynamic range decreases to 10^{5}, the required minimum uncertainty in the ionosphere model decreases to 7 10^{3} (i.e., 0.7%) for an observing time of 10 h.
Figure 9: Peak flux density of the phasereferenced image, relative to the real peak flux density of the source, as a function of (see Eq. (7)) and for a 1scan snapshot of 60 s. 

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For a more comprehensive representation of our results, we show in Fig. 10 how the achievable dynamic range (computed from Eq. (9)) depends on the uncertainty in the model of atmospheric turbulence used in the data calibration. We show this relationship for different observing frequencies and calibratortotarget separations. For instance, a dynamic range 10^{4}in observations at 100 MHz for a calibratortotarget separation of 1 deg (i.e., the same for a widefield image of 2 2 deg) would require a turbulence model with an accuracy of % for an observing time of 60 s. This requirement would relax to an accuracy of 9798% for an observing time of 6000 s (provided the dynamic range increases as the square root of the observing time).
Figure 10: Maximum dynamic range as a function of the uncertainty in the model of the atmospheric turbulence for a 1scan snapshot of 60 s. 

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For completeness, we also computed the loss in the recovered flux
density of the source caused by the turbulent atmosphere.
In Fig. 9,
we show the ratio of peak flux densities of the phasereferenced images
to those computed without accounting for the effects of atmospheric
turbulence. For dynamic ranges of 4050, the loss of flux density
can be as large as 25%. The phenomenological model (also shown in
the figure) used to fit the data is
where D_{2} = 0.32 0.02 and 0.01.
The applicability of Eqs. (9) and (10) is not restricted to the array used in the simulations reported here. The exponents and depend only on the structure of the atmospheric turbulence and are thus independent of the interferometer used in the observations. However, the parameters D_{1} and D_{2} also depend on the stations of the interferometer. Therefore, Eqs. (9) and (10) can be adapted to any other interferometer by finding the correct values of D_{1} and D_{2}. As an example of this generalization of Eqs. (9) and (10), MartíVidal et al. (2010) studied the achievable dynamic range in phasereferenced observations preformed by the Very Long Baseline Array (VLBA) at 8.4 GHz and 15 GHz. This study was based on quasisimultaneous observations of 13 sources located at separations ranging from 1.5 to 20.5 degrees. These authors were able to model the dynamic ranges obtained in the phasereferenced images and the loss of recovered flux densities (by comparing phasereferenced images to images obtained from selfcalibrated visibilities) using Eqs. (9) and (10) with values for D_{1} and D_{2} different to those reported here, but using the same values reported here for the exponents and .
6 Conclusions
We have presented Monte Carlo estimates of the sensitivity and astrometric precision of an interferometric array, with a station distribution similar to that of the planned SKA, as a function of observing frequency, flux density, and source separation. These results can also be applied to other array distributions by taking into account the corresponding correction factors. Our estimates are based on simulations of snapshot phasereferenced observations, in which we take into account several effects including those of the turbulent atmosphere and the finite temperature of the receivers. We have found that the astrometric uncertainty strongly depends on the observing frequency and smoothly increases as the source separation increases. For frequencies below 1 GHz, ionospheric effects dominate and the astrometry uncertainties (when the source is detectable) can be as large as 1 as. For frequencies between 1 and 10 GHz (these values slightly depend on the source flux density), atmospheric effects are minimal and we roughly reach the theoretical astrometric precision of the interferometer. Above these frequencies, the wet troposphere begins to have an important effect and the astrometric uncertainty increases to 10 mas for the highest simulated frequency (25 GHz). The dynamic range of the images is strongly limited by atmospheric turbulence at all frequencies and for all flux densities (it can decrease, in the worst cases, by several orders of magnitude).
We have proposed analytical models for the loss of dynamic range, astrometric accuracy, and recoverable flus density as a function of distance between calibrator and target source. These expressions may also be used to estimate the deformations and local dynamic ranges of widefield images as a function of distance to the image phase center (i.e., the point in the sky where the data correlation is centered).
We thank Ed Fomalont for his very useful comments and suggestions. I.M.V. is a fellow of the Alexander von Humboldt Foundation. This work has been supported by the European Community Framework Programme 6, Square Kilometre Array Design Studies (SKADS), contract number 011938. This work has also been partially founded by grants Prometeo 2009/104 of the GVA and AYA200913036CO22, AYA200614986CO201, and AYA200508561C03 of the Spanish DGICYT.
Appendix A: Complementary simulations: different number of stations and array sensitivities
Our simulations are based on a given realization of the SKA. However, the main structure of the array distribution used in our simulations is not exclusive to the SKA. Other interferometric arrays, such as ALMA or LOFAR, are being built with similar station distributions, consisting of a compact core and several extensions along the shape of spiral arms. Hence, our study can be extended to those arrays by taking into account the difference between the number of stations and the station sensitivities.
Figure A.1: Ratios of dynamic ranges obtained with our original array and those obtained with a subarray of 100 stations a) and an array with half the sensitivity of the original array b). Different lines correspond to different target source flux densities (10 Jy, continuous line; 1 Jy dashed line; 0.1 Jy, dotted line). 

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The amount of noise added to the data is proportional to the number of stations, since each station receives the signal through the turbulent atmosphere. However, in cases of clear source detections (D > 2030), the dynamic range does not depend (or the dependence is weak) on the thermal noise of the receivers (see Sect. 5.1). Therefore, to estimate the achievable dynamic range for an array with a different number of stations, the results shown in Fig. 6 should be divided by N/N', where N is the number of stations used in our simulations (N= 200) and N' is the number of stations of the other array. This is true for detections with a relatively large dynamic range (D>2030). For weak sources, the noise from the receivers may also contribute to the rms of the residual images, so the factor to apply in these cases should be , where is the thermal noise of the stations used in our simulations and is that of the other array.
We repeated the simulations described in Sect. 5.1 using different arrays to compare the results with those obtained with the original array. On the one hand, we created a smaller array by subtracting 100 stations (those marked with empty squares in Fig. 1) from the original array. On the other hand, we created another array with all the 200 stations, but decreasing their sensitivity by a factor of 2. We show the results obtained in Fig. A.1. Special care must be taken interpretating these figures, given that the computed ratios of dynamic ranges are only meaningful when the detections of the sources are clear (i.e., when no spurious noise peaks appear stronger than the source). This is true for D > 2030, which corresponds approximately to frequencies between 1 and 10 GHz (although it depends slightly on the source flux density, see Fig. 6).
By taking these considerations into account, we find that the ratio of dynamic ranges for an array with 100 stations falls between 0.7 and 0.5 compared to the array with 200 stations. The expected value is 0.5 (since N' = 0.5 N and ). Other factors, such as the different coverages of Fourier space by both arrays, may affect the dynamic range of the images, thus increasing the ratio in some cases. For an array with lower station sensitivities (but the same number of stations), the ratio of dynamic ranges falls between 0.75 and 1 for the strongest sources (as expected, since N' = N and the noise from the receivers is muchsmaller than the noise from the atmosphere), but is close to 0.5 for the weakest source (also as expected, since the thermal noise from the receivers begins to dominate in this case).
References
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All Figures
Figure 1: Array distribution used in our simulations (empty and filled squares). Axes are relative longitude (horizontal axis) and latitude (vertical axis) in km. Left, the whole array. Center, a zoom into the core. Right, a zoom into the inner core. The stations marked with empty squares were removed from the array in a second run of our simulations, to check the dependence of the results on different array distributions (see text). 

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In the text 
Figure 2: Station sensitivities (i.e., effective areas over system temperatures) used in our simulations. 

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In the text 
Figure 3: Example of a turbulent phase screen with Kolmogorov statistics. The grey scale shows variations in opticalpath phases, normalized between 1 and 1 radians. The final values of the phases depend (given the selfsimilarity of the distribution) on a global factor related to the observing frequency and the ionospheric and/or wet tropospheric conditions. 

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In the text 
Figure 4: Distribution of right ascension shifts a) and dynamic ranges b) of 1500 snapshot phasereferenced images, simulated at 1420 MHz, for a 1 Jy target source located at 5 deg from its calibrator. The calibrator source is located at an hour angle of 0 and the target source is located at the zenith of the array center. 

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In the text 
Figure 5: Simulated phasereference images of a 1 Jy source located at 5 deg from its calibrator. Noise from the receiving system (top) and, additionally, noise due to the turbulent atmosphere (bottom) have been added to the visibilities. 

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In the text 
Figure 6: Astrometric accuracy a) and dynamic range b) as a function of frequency, in the case of atmospheric turbulence and a separation of 5 degrees between calibrator and target. The calibrator source is located at an hour angle of 0 and the target source is located at the zenith of the array center. Different lines correspond to different target source flux densities (10 Jy, continuous line; 1 Jy, dashed line; 0.1 Jy, dotted line). 

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In the text 
Figure 7: Effects of targettocalibrator separation in the quality of the phasereference images. Dots: simulated astrometric accuracy a) and dynamic range b) for observations at 1420 MHz and a target flux density of 1 Jy. Lines: proposed phenomenological models. 

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In the text 
Figure 8: Maximum dynamic range as a function of (see Eq. (7)) and for a 1scan snapshot of 60 s. 

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In the text 
Figure 9: Peak flux density of the phasereferenced image, relative to the real peak flux density of the source, as a function of (see Eq. (7)) and for a 1scan snapshot of 60 s. 

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In the text 
Figure 10: Maximum dynamic range as a function of the uncertainty in the model of the atmospheric turbulence for a 1scan snapshot of 60 s. 

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In the text 
Figure A.1: Ratios of dynamic ranges obtained with our original array and those obtained with a subarray of 100 stations a) and an array with half the sensitivity of the original array b). Different lines correspond to different target source flux densities (10 Jy, continuous line; 1 Jy dashed line; 0.1 Jy, dotted line). 

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In the text 
Copyright ESO 2010
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