Supplementary Material to:

An Introduction to Radio Astronomy

4th edition Cambridge University Press 2019   

Last updated 4/12/2021


 

Chapter 11: Further Interferometric Techniques  

 

 

Interferometer Arrays at mm wavelengths

 

 

alma.jpg

 

 

ALMA:  the Atacama Large Millimetre Array is located on the Llano de Chajnantor in Chile at an altitude  of5000metres; its receivers cover bands in the frequency range 84-950GHz. The main array comprises 50 × 12-m antennas which can be moved into different configurations from compact (baselines to 150m) to extended (baselines to 16 km). The Atacama Compact Array (ACA) is a subset of four 12-meter antennas and twelve 7-meter antennas which are closely separated to improve ALMA’s ability to study objects witha large angular size.  www.almaobservatory.org/

 

 

 

               
sma.PNG

 

SMA:  the Smithsonian Submm-wave Array on Mauna Kea, Hawaii (altitude 4080metres) has 8×6-m antennas which can be configured to provide baselines up to 783m. The receivers cover the wavelength range 1.7 to 0.7 mm (180-418GHz) in three bands. www.cfa.harvard.edu/sma/

 

 

                    
noema.jpg

 

NOEMA: the Northern Extended Millimetre Array of the Institut de Radio Astronomie Millimetrique is located on the Plateau de Bure in the French Alps (altitude 2550metres). When completed in 2019 it will have 12 × 15-m antennaswhich can be moved on E-W and N-S tracks to provide baselines up to 760m. (The image shows the 6 original antennas in an extended configuration). Four suites of receivers cover atmospheric windows from 3mm to 0.8mm (72-373GHz).  http://iram-institute.org/EN/noema-project.php



Interferometer Arrays at Long wavelengths

 

 

lofar.jpg

 

 LOFAR: the international Low-Frequency Array is centred in the Netherlands (maximum baselines 100 km) with (in 2017) external partner stations in Germany, France, UK, Sweden, Poland and Ireland (maximum baselines1500 km). It operates in two bands: LOFAR-low (10-80GHz) uses low-cost droop dipoles; LOFAR-high (120-240GHz) is built up from ”tiles” made up from 4×4 bowtie dipoles (Section 8.1.3). A typical station consists of 96 low-band antennas and 48 high-band antenna tiles. There are 18 ”core” stations and 18 ”remote” within the Netherlands and (currently) 8 international stations. Each ”station” can produce one or more beams which can be cross-correlated with the equivalent beams from other sites to form an aperture synthesis array. The latter system relies on broad band optical fibre data links with the digital correlation carried out via software in a high performance computer rather than in purpose designed electronics. www.lofar.org/

 

 

 

mwa.jpg

 

MWA: the Murchison Widefield Array  is located in Western Australia near the plannedsite of the SKA-low telescope. It consists of 2048 dual-polarization bowtie dipoles (Section 8.1.3) optimized for the frequency range 80-300MHz. As in LOFAR-high they are arranged in tiles of 4×4 dipoles giving a field of view of 25at 150MHz. The majority of the  original 128 tiles are distributed within a 1.5 km core region so as to provide high imaging quality at a resolution of several arcminutes. A phase 2 expansion which doubled the number of tiles to 256 (and the number of dipoles to 4096) was commissioned in April 2018  http://www.mwatelescope.org/telescope.

An update on the status and performance of the MWA can be found at:

https://arxiver.moonhats.com/2019/10/08/science-with-the-murchison-widefield-array-phase-i-results-and-phase-ii-opportunities-ima/

 

 

 

 

lwa.jpg

 

LWA: the Long Wavelength Array has been developed by the University of New Mexico and a consortium of US partners. There are two sites: in New Mexico close to the JVLA (run by University of New Mexico) and in Owens Valley California (run by Caltech).  At each site there is currently a single ”station” consisting of 256 linearly polarized crossed dipole elements distributed over a 100 m diameter area and sensitive to the frequency range 10-88 MHz (New Mexico) and 27-85 MHz (0wens Valley). http://www.phys.unm.edu/~lwa/index.html  and  http://www.tauceti.caltech.edu/LWA/

 

 

ska-low.jpg

 

SKA1-low: (artist’s impression)The SKA low frequency aperture array (LFAA) will be located in Western Australia and is designed to cover the frequency band 50 – 350 MHz. It will consist of ~130,000 fixed antennas spread between ~500 stations with a maximum distance between stations of 65 km. At the lowest frequency its total collecting area will be ~0.4 km2 https://www.skatelescope.org/lfaa/


 

Very Long Baseline Interferometer Networks

 

 


 

 

VLBA: the Very Long Baseline Array of the USA is a dedicated facility consisting of 10 × 25-m identical telescopes. Their locations extend at northern latitudes from New Hampshire to the state of Washington, and at southern latitudes from St Croix in the Virgin Islands to the island of Hawaii.The central correlator is located at the NRAO Science Operations Centre,Socorro, New Mexico. www.science.nrao.edu/facilities/vlba


 

 


 

 

EVN: The European VLB Network is a cooperative arrangement of radio telescopes in the UK, Netherlands, Germany, Italy, Poland, Russia, Ukraine, China and Japan with other antennas joining from time to time. The central correlation facility is the Joint Institute for VLBI in Europe (JIVE) at Dwingeloo, The Netherlands. Periodically the EVN and the VLBA cooperate to form a world-wide network. At the time of writing the EVN operates in real-time fibre-connected mode for 25% of the total time allocated for EVN operation; this percentage will grow with time. www.evlbi.org/


 


 

East Asian VLBI Network the Japanese VLBI Network (JVN) and the Japanese dedicated astrometric array (VERA) with its dual-beam antennas work independently. VERA will also work in cooperation with the Korean VLBI Network (KVN) to form the kaVA.

www.miz.nao.ac.jp/en/content/project/east-asia-vlbi-network

and https://radio.kasi.re.kr/eavn/main_eavn.php

 

 

Australian VLB Array: consists of the Australia Telescope Compact Array and single dishes at Parkes, Tidbinbilla, Hobart Ceduna and Perth. It is the only VLBI array in the southern hemisphere  www.atnf.csiro.au/vlbi/

 

 

IVS: the International VLBI Service for Geodesy and Astrometry coordinates global VLBI resources for positional VLBI. At various times this includes 45 antennas sponsored by 40 organizations located in 20 countries.The IVS Coordinating Center is located at Goddard Space Flight Centerin Greenbelt, MD. The next generation coordinated facility ”VLBI2010” is planned to have more small fast-slewing antennas and a much enhanced multi-band receiving system  https://ivscc.gsfc.nasa.gov/

 

 

GMVA: The Global mm-wave VLBI Array is a cooperative arrangement of many mm-wave telescopes under the auspices of five different internationalorganisations. They come together about twice per year to make coordinatednetwork observations.

https://www3.mpifr-bonn.mpg.de/div/vlbi/globalmm/

   

 

EHT: the Event Horizon Telescope https://eventhorizontelescope.org is another international coordinated network of independent telescopes, it includes the phased-up ALMA. The purpose is to make ultra-high resolution observations at 1.3mm wavelength with a particular target being the massive black hole at the centre of the Milky Way and the giant elliptical galaxy M87. In April 2019 the EHT consortium published the first images showing the “black hole shadow” of the SMBH in the nucleus of M87 – see references and further details in Supp. Mat. Chapters 9, 11 & 16.

 

Space VLBI

                                            

VSOP/HALCA:   was the first dedicated space VLBI project . The 8-m antenna was launched by Japan’s Institute for Space and Astronautical Sciences in 1997 and operated until late 2005. The orbit took the antenna from 12,000 to 27,000 km above the Earth’s surface providing resolutions  about 3 times higher at a given wavelength than Earth-based arrays. https://science.nasa.gov/missions/halca

 

 

RadioAstron:  http://www.asc.rssi.ru/radioastron/

is the second dedicated space VLBI project led by the Astro Space Center of the Lebedev Physical Institute in Moscow, Russia. The spacecraft was launched in July 2011 and operated until January 2019. The reflector is 10m in diameter and the orbit takes it out to 350,000 km from the Earth thus providing resolutions > 30 times those available in Earth-based arrays.  A review of the role of RadioAstron in AGN studies is given by Bruni et al (2019)    https://arxiv.org/abs/1904.00814

Gurvits (2019) has reviewed the history of space VLBI from concepts to operational missions: see https://arxiv.org/abs/1905.11175

 

 

Special purpose arrays

 

https://chime-experiment.ca/images/backgrounds/bg6.jpg

 

 

 

 

 

 

 

 

 

 

 

 

 

CHIME The Canadian Hydrogen Intensity Mapping Experiment is located in Penticon, British Columbia Canada. It consists of four adjacent 20m x 100m cyclindrical reflectors orientated north-south. The focal axis of each cylinder is lined with 256 dual-polarization antennas covering the frequency range 400-800 MHz and giving it a very wide field of view. Its main targets are baryon acoustic oscillations (BAO) which are diagnostics of Dark Energy and sources of Fast Radio Bursts (FRBs).  An outline explanation of the experiment and of its beamforming and image formation capabilities can be found at: https://chime-experiment.ca/.

 

HERA The Hydrogen Epoch of Reionization Array is designed for a frequency range 50-225 MHz to observe large scale structure at epochs around the Epoch of Reionization.  It will consist of 331 x 14 meter diameter non-tracking dishes pointing vertically and packed into a hexagonal grid 310 m in diameter. HERA is being constructed in the Karoo desert of South Africa with completion expected in Q4 2020 see  https://reionization.org/

 

HIRAX The Hydrogen Intensity and Real-time Analysis eXperiment aims to map the southern sky in continuum and redshifted neutral hydrogen emission in the band 400-800 MHz to look for baryon acoustic oscillations (BAO) which are diagnostics of Dark Energy and sources of Fast Radio Bursts (FRBs).  It will consist of ~1000x 6m non-tracking dishes and will be located in the Karoo desert of South Africa; see https://www.acru.ukzn.ac.za/~hirax/

 

TIAN-LAI The Tian-Lai Project is situated in north west China and is aimed at using 21cm intensity mapping to detect baryon acoustic oscillations see http://tianlai.bao.ac.cn/


                              

Techniques in Aperture Synthesis: resources

 

 

 

Spectral Lines

 

http://www.astron.nl/eris2017/Documents/ERIS2017_L11_Johnston.pdf

 

https://science.nrao.edu/science/meetings/2018/16th-synthesis-imaging-workshop/talks/Pihlstrom_Spectral_Line.pdf

 

 

Polarisation

 

https://science.nrao.edu/science/meetings/2018/16th-synthesis-imaging-workshop/talks/Schinzel_Polarization.pdf

 

http://www.astron.nl/eris2017/Documents/ERIS2017_L13_Marti-Vidal.pdf

 

 

 

Millimetre wave interferometry

 

http://www.astron.nl/eris2017/Documents/ERIS2017_L6_Pietu.pdf

 

https://science.nrao.edu/science/meetings/2018/16th-synthesis-imaging-workshop/talks/Friesen_ALMA_OT.pdf

 

 

 

Mosaicing:

 

https://www.atnf.csiro.au/research/radio-school/2012/lectures/thu/ListerStaveley-Smith_mosaicing_2012.pdf

 

https://science.nrao.edu/science/meetings/2018/16th-synthesis-imaging-workshop/talks/Mason_Mosaicking.pdf

 

Detailed discussion of practicalities :  https://science.nrao.edu/facilities/vla/docs/manuals/obsguide/modes/mosaicking

 


A set of pointings to cover a large field of view

 

The circles represent the FWHM of the antenna primary beam (all identical) and the pointing centres are separated by 0.5 FWHM.  A central beam e.g. number 25 is surrounded by a hexagonal pattern of beams 18,24,31,32,26,19.  Another example is the beam number 10 surrounded by beams  11,4,3,9,16,17.  A mosaiced image made with such a pattern is shown in Supp. Mat. Chapter 16 under “Faint Radio Sources” (courtesy T. Muxlow).

 

 


 

 

 

Filling in short spacings with single dish data

 

These two presentations both have illustrations of using a single dish to fill in lack of short spacings in correlation interferometers

 

https://www.atnf.csiro.au/research/radio-school/2017/lectures/west-single-dish-astronomy-2017.pdf

 

https://science.nrao.edu/facilities/gbt/single-dish-school-lectures/sds-2015/combining-single-dish-zero-spacing-data-with-interferometric-maps/view

 

 

VLBI

 

https://science.nrao.edu/science/meetings/2018/16th-synthesis-imaging-workshop/talks/Deller_VLBI.pdf

 

http://www.astron.nl/eris2017/Documents/ERIS2017_L12_Campbell_no-anim.pdf

version with animations:

http://www.astron.nl/eris2017/Documents/ERIS2017_L12_Campbell_with_anim.pdf

 

 

Wide-field imaging:

 

https://science.nrao.edu/science/meetings/2018/16th-synthesis-imaging-workshop/talks/Rao_Wide_1.pdf

 

https://science.nrao.edu/science/meetings/2018/16th-synthesis-imaging-workshop/talks/Rao_Wide_2.pdf

 

http://www.astron.nl/eris2017/Documents/ERIS2017_T9A.pdf

 

 

Astrometry

 

Update on the ICRF3 and link with Gaia

 

“The third realisation of the international celestial reference frame  by very long baseline interferometry” has been published  by  Charlot  et al https://arxiv.org/abs/2010.13625.  It contains positions for 4588  compact radio sources.   A subset of 303 sources, uniformly distributed on the sky, are identified as "defining sources" and as such serve to define the axes of the frame. A subset of 500 sources is found to have extremely accurate positions at 8.4 GHz, in the range of 0.03 to 0.06 mas. Comparing ICRF3 with the Gaia Celestial Reference Frame 2 in the optical domain, there is no evidence for deformations larger than 0.03 mas between the two frames. 

 

 

New astrometric applications in the Solar System

 


 

An exciting new application of VLBI astronomy is in the Solar System.  Here VLBI observations provide not only celestial 2D coordinates but can take advantage of ultra-precise radial Doppler measurements of spacecraft, down to the residual noise of ~0.015 mm/s. The technique is called PRIDE - Planetary Radio Interferometry and Doppler Experiment. The tracking of the Huygens lander (part of the Cassini mission) onto Titan on 14 January 2005 was the first demonstration of PRIDE. The picture shows an artist’s impression of the Huygens probe arriving at Titan together with the reconstructed descent trajectory of the probe. The latter is based on various in-situ measurements with the on-board instruments (cameras, altimeters, accelerometers) and VLBI tracking of the probe at 2040 MHz with a network of 17 radio telescopes distributed globally (Asia, Australia, Europe and USA). VLBI tracking provided the highest lateral (astrometric) precision of 1 km (1-sigma) in the ICRF frame. Currently the working goal of PRIDE is a 1-sigma lateral precision of  ~50 m at the 5 A.U. distance of the Jovian system using observations at X-band (8.4 GHz).   (Credits:  Artist’s impression – ESA and D.Ducros; Descent trajectory – Huygens DTWG and JIVE (Leonid Gurvits)).

 

As well as ultra-precise astrometry of spacecraft and natural celestial bodies in Solar System future applications of PRIDE include: improvements of planetary ephemerides, detection of Solar Coronal Mass Ejections, measurements of planetary atmospheres (e.g. Venus, Mars) by means of radio occultations, verification of the Einstein Equivalence Principle.  Recent references to the astrometric technique are:

D. A. Duev et al  2012, “Spacecraft VLBI and Doppler tracking: algorithms and implementation” A&A, 541, A43

D. A. Duev et al  2016, “Planetary Radio Interferometry and Doppler Experiment (PRIDE) technique: A test case of the Mars Express Phobos fly-by”, A&A 593, A34.

 

 

 

Geodesy

 

An Introduction/Overview

 

VLBI has made major contributions to the study of plate tectonics. A useful introduction can be found at

 https://www.haystack.mit.edu/edu/pcr/Data/pdf/Introduction%20to%20plate%20tectonics,%20geodesy%20and%20VLBI-final.pdf   

A publicly available 50+ page tutorial document on geodetic and astrometric VLBI (Elements of Geodetic and Astrometric Very Long Baseline Interferometry)

written by Axel Nothnagel can be found at  https://www.vlbi.at/index.php/rushmore_teams/axel-nothnagel/.  He states that this document is an open tutorial for educational purposes, in particular for newcomers to geodetic and astrometric VLBI but also for the specialists wanting to expand their knowledge about topics, which are not in their main focus.

 

Increasing separation  of a transatlantic baseline

 


A baseline between Europe and the USA is lengthening at 17.28 ± 0.16 mm per year.  The plot above shows the change in baseline length measured between radio telescopes at Westford (MA, USA) and Wettzell (Germany). Each dot represents the 24h-average length of the baseline determined with a single VLBI session. The observations are X- / S-band group delays taken from the IVS (International VLBI Service for Geodesy and Astrometry) archive; the errors are obtained by propagation of the formal errors of the geocentric coordinates. The long-term change is caused by a superposition of plate tectonic and inter-glacial isostatic adjustment processes, which are different at the two sites. In addition to the long-term change, the original data show a faint quasi-sinusoidal variation. This signal originates from displacements of the crust due to geophysical surface loading - mainly of hydrological, atmospheric and oceanic origin - that are currently not considered as conventional analysis models (IERS Conventions). The deviations are more pronounced prior to about 1994 when the networks of IVS observing stations customarily contained small numbers of antennas (> 5) and the observation quality was not as good as it is today  (image courtesy Robert Heinkelmann and Susanne Lunz GFZ Potsdam - see

https://www.gfz-potsdam.de/en/section/space-geodetic-techniques/topics/geodetic-and-astrometric-vlbi/)

 

Update on the World-wide geodetic array: VLBI2010

 

Plate motions are now studied predominantly with GPS and so the main scientific thrust  of VLBI geodesy is the study of the Earth’s rotation which requires comparison with the fixed quasar reference frame ICRF2 and ICRF3.  GPS from orbiting satellites is not suited to Earth Rotation studies.

 

The international IVS service is engaged in a major upgrade to the world-wide geodetic array. This includes new 14m telescopes with fast slew speeds and instantaneous broad band receiving systems (2-14 GHz) see https://www.mpifr-bonn.mpg.de/1263600/Hase_110329VLBI2010.pdf

 

 

 

The SMOS Earth Resources Satellite

 

 


 

The European Space Agency’s SMOS satellite (see https://earth.esa.int/web/guest/missions/esa-operational-eo-missions/smos/multimedia-book) is a radio telescope in space pointing downwards; it operates on the same interferometric principles as, for example, the JVLA with which it shares the Y-shaped antenna array configuration. SMOS operates at L-band where the atmosphere  highly transparent  and by detecting small changes in surface brightness temperature measures soil moisture, sea surface salinity, sea ice thickness and others geophysical variables (image credit European Space Agency).

 

Note that the NASA/JPL/GSFC  single dish radiometer missions Aquarius and SMAP share the same observational goals (see Supp. Mat Chapter 8) as SMOS.  All these missions demand highly accurate (0.1K) calibration of surface brightness.

 

 


 

 

Pros and cons of single dishes vs. phased arrays vs. aperture synthesis arrays:

Single dishes:

 

Scientific Advantages: where the angular resolution of the dish does not matter

       Searching for pulsars and timing them (Sections 15.13 & 15.16) – with the aid of focal plane arrays or PAFs

       Searching for Fast Radio Bursts (new Supp.Mat. section “The Time Variable Radio Sky”)

       Involvement in VLBI Networks – resolution then set by antenna separations (Section 11.4)

Scientific Advantages: where the filled aperture of the dish matters

       Large-area spectral line and continuum surveys - no low brightness emission is missed

(Chapter 14) also low angular resolution means sky can be mapped in a practical period of time.

Technical advantages

        Receiver systems: are usually one-off designs and hence relatively easy to change/upgrade

        Standard methods for observations/analysis developed over decades.

General disadvantages

        Size and collecting area limited:

-   sensitivity limited  

-   angular resolution limited: hence cannot localize FRBs and  also source confusion limits deep surveys (Section 8.9)

-   accurate power calibration difficult (Section 6.5 and Supp. Mat. Chapter 6)

        Greater susceptibility to unwanted signals (RFI, see Section 1.5 ).

 

See also the presentation:  https://www.mpifr-bonn.mpg.de/948285/Possenti_Why_Single_Dish.pdf

 

Adding interferometers (beam-forming arrays; phased arrays; aperture arrays):

 

General points

o  Adding responses produces “direct” imaging - form an instantaneous power beam like single dish (Section 8.2; section 11.6; Supp Mat Chapter 8).

o  Flexible digital beam forming enabled by the on-going revolution in digital signal processing

o  Higher sidelobes in “tied array beams” (Section 8.2; Supp Mat Chapter 8) arise from an unfilled aperture; but reducing the maximum baseline to get better instantaneous filling limits the resolution.

o  The number of elements required to cover a given area increases as (wavelength)-2  thus costs currently set the upper frequency limit (for large areas) at about 350 MHz with dipole-like elements (section 8.1; section 11.6); technology improvements required for dense aperture arrays at higher frequencies.

 

Advantages

·     Well-suited for real-time “non-imaging” applications e.g.  pulsars and transients too small to resolve and for which precise amplitude calibration is less important than for synthesis imaging

·     With independent delay systems can populate the primary beam of individual elements or patches with many higher resolution “tied array beams” (Section 8.2) thus particularly good for surveys for transient sources.

 

Disadvantages

o  Subject to receiver gain variations,  just as single dishes

o  To cover the antenna primary beam with “tied array” beams likely to require a major investment in electronics

o  Pose a calibration challenge for wide-fields and long integrations: (Section 11.6)

§  Difficulty in characterizing the element primary beam, on all baselines

§  At long wavelengths and long baselines: suffer the effects of the turbulent ionosphere (section 4.4; section 9.7; section 11.6)

 

 

Multiplying or correlation interferometers (aperture synthesis arrays):

 

General points

·        “Indirect imaging: spatial coherence (section 9.6) i.e. visibility data are in the Fourier domain – image reconstruction is a secondary step. Compare with

i)                    X-ray crystallography: which only measures the intensity of the scattered waves and does not have direct access to the Fourier phase as in radio interferometry; also uses “tricks” to obtain phase information.

ii)                    Holography: where phase information is partially captured via intensity fringes in the hologram formed by adding the scattered wave with a reference wave.

·       Can assemble large collecting areas from many smaller elements (Chapter 10) with resolution set by the antenna separation not the size of the antennas.

·       In contrast to adding arrays correlation arrays see the entire field-of-view, set by the primary antenna beam, at once.

 

Advantages

·       Correlating the complex electric fields gives access to relative phase information

o   provides positional accuracy well within the conventional synthesised beam for astrometry and geodynamics (Section 9.3; Section 11.4)

·       Confusion limit much lower than for single dishes: higher resolution means less blending of the responses to the population of discrete sources (Section 10.12).

·       Resistant to uncorrelated signals

o   Gain variations in independent receivers

o   Atmospheric emission above independent antennas

o   Less sensitive to man-made RFI than dishes

 

Disadvantages

·       Only N(N-1)/2 baselines thus the Fourier transfer function has gaps

o   Deconvolution techniques usually required to “fill in the gaps” but with no formal guarantee of the fidelity of the reconstructed image (section 10.15)

o   No “zero-baseline” information (section 11.5) and finite filling factor gives reduced brightness temperature sensitivity (section 10.12) hence not well suited to imaging smooth low brightness emission

o   In worst case (typically wide fields and low frequencies) visibility information collected may be insufficient to capture the complexity of the field being imaged.

 

 

 

 

Routes to survey speed improvements

 

Survey Speed ~ [Aeff/Tsys]2 x BW x FoV

 

·       Effective area: Aeff

o   Invariably at a cutting edge since natural radio sources are very weak

o   For dishes the size is fixed at build time but the feed illumination pattern (Section 8.3) can be optimised with phased array feeds (Section 8.7) à limited improvement possible

o   For arrays can always add more elements

·       System temperature: Tsys

o   Receiver performance is already close to realistic limits – particularly from ground-based sites à only limited improvement possible in Tsys (Section 6.4)

·       Receiver frequency bandwidth: BW

o   Can use broad-band single pixel feeds (Section 8.1) for dishes and arrays but the practical frequency range is limited by need to maintain polarization purity across the band (section 7.6) and RFI.

·       Field-of-View: FoV

o   Sky coverage of single dishes increased with focal plane horn arrays and phased array feeds (PAFs) à major improvement possible in FoV (Section 8.7); the cutting edge is now the development of cryogenic PAFs.

o   Arrays can take advantage of PAFs – current examples are ASKAP and WSRT/APERTIF (Section 8.7; Section 10.1 and Supp. Mat Chapter 8).

o   Low frequency arrays with small basic elements are already sensitive to huge areas of sky (Section 11.6).

 

 

The Square Kilometre Array

The SKA public web site

The SKA public web site https://www.skatelescope.org/  provides comprehensive overview of all aspects of the project to build the world’s largest radio telescope, at sites in Africa (South Africa initially) and Australia. The Global Headquarters of the SKA Organisation is at the Jodrell Bank Observatory UK which is the scientific home of two of the authors (FGS and PNW). 

The first four sections:

·       About the SKA

·       Design

·       Technology

·       Science Goals

contain most of the material which directly complements our text although the other sections are also full of interesting information, in particular more detailed technical information and memoranda. The reader should browse them at leisure. As regards the sections listed above we draw particular attention to following sub-sections

·       About the SKA

o   The SKA Project

§  The layout

o   The specific sites in Africa and Australia

·       Design

o   The work of the nine international consortia which came together to design the first phase SKA1 which will be built

o   The advanced instrumentation programme  looking ahead to technology enhancements in particular

§  Wide Band Single Pixel Feeds;

§  A mid-frequency aperture array;

§  Phased array feeds.

·       Technology

o   Aperture arrays (SKA1-LOW in the first instance)

o   SKA dishes

o   Software and computing

o   Signal processing

o   Precursors and Pathfinders (ASKAP; MeerKAT; MWA; HERA)

·       Science Goals

o   Concise descriptions of the SKA’s Key Science Programmes

o   The 2015 version science case: 135 chapters, 1200 contributions and 2000 pages (2 volumes) – papers available on the SKA site. https://www.skatelescope.org/news/ska-science-book/

 

 

 

 

The SKA science web site

The SKA site aimed at astronomers  https://astronomers.skatelescope.org/  provides more in-depth information on a range of topics including

·       The telescopes: LOW- and MID- including

o   Frequency bands

o   Plots of anticipated sensitivity performance

·       The Timeline

o   The build up to operations of Phase 1 in Australia and South Africa

·       The science community

o   Information of the many Science Working Groups  and Focus Groups and how to join them

·       Documentation

o   The repository of documents on, among other topics: design, performance, configuration, Key Science.