Summary of JCMT Instrumentation for Semester 95A
Introduction Semester 95B (1 August 1995 - 31 January 1996) JCMT instrument
availability and sensitivities are summarized below. Additional details can be found in 'The James
Clerk Maxwell Telescope: A Guide for the Prospective User', which is available over the e-mail
fileserver or through the JCMT Section of the Royal Observatory Edinburgh, by contacting the JCMT
Group at the Herzberg Institute of Astrophysics in Canada or the NFRA at Dwingeloo, The
Netherlands, or from the Joint Astronomy Centre in Hawaii. The current version is dated January
25, 1995. The e-mail fileserver system exists to provide instrumental data, both archival and
current, and other information. To get acquainted with the latter send the one-line message "help" to
the Internet address: JCMT_INFO@JACH.HAWAII.EDU The User Guide also may be
browsed on the Internet hypertext-based World-Wide Web, at URL
/JCMT/home.html which carries a variety of other information too.
Spectral Line Observations Three SIS mixer receivers form the core of the heterodyne
program, A2, B3i and C2. One other SIS receiver (G) has been available on occasion via
collaboration with the MPE, Garching group. A summary of the properties of this instrumentation is
given below, followed by a few additional details.
Table 1. Summary of spectral line observational data.
Freq. IF B/W Trx Efficiency Tel. HPBW
(GHz) (GHz) (MHz) (K) Ap. Beam fss losses (")
A2 205-285 1.50 600 95 0.57 0.69 0.80 0.91 19.7
B3i 300-380 1.50 700 180 0.49 0.58 0.70 0.91 14.3
C2 450-505 3.94 1000 250 0.31 0.52 0.70 0.83 10.8
G 660-692 1.50 800 800 (0.20) 0.25 (0.60) 0.65 7.0
The IF and IF instantaneous
bandwidth (B/W) are given. DSB receiver temperature values (Trx) are typical (average) numbers
for each receiver; there are significant changes as a function of frequency. The efficiencies (where
measured) are accurate to at least 10%. Quoted beam efficiencies are derived from measurements
towards Jupiter. The beam can be slightly elliptical and may depend somewhat on frequency. Beam
maps are available via anonymous FTP (ask for fileserver item 'receivers.beam_maps' for details) and
the WWW. A new SIS version of Receiver G first saw service in March 1994 and the data given
above are based on information from that time. Users should note that because receiver C2 uses
an EIP counter to phaselock the Gunn local oscillator, the resolution achievable is limited by the
Gunn's intrinsic phase stability, with the consequence that lines observed with C2 are likely to be
broadened instrumentally by an additional 0.5 km/sec, and thus C2 may NOT be suitable for the
observation of sources requiring velocity resolution better than a few tenths of a km/sec. Note that
the line frequency itself is not affected by the phase 'jitter'. Until late 1994 A2 had a similar EIP
system; this has since been replaced with a true phaselock system adapted from the old receiver B2.
In the case of B3i a much more agile phaselock system is used that can suppress the Gunn oscillator's
inherent phase noise. Thus for B3i the resolution is limited only by the spectrometer. (a)
Receiver A2 A2 is a single-channel receiver which was commissioned in March 1992. Its
excellent low-noise performance results in a total SSB system temperature (Tsys) of better than 400 K
at the zenith across most of the band under normal conditions. (b) Receiver B3i
B3i (also a single-channel device) is one of the best receivers available in this band in the world. The
DSB receiver temperature response is not constant with frequency, and ranges from a best value of
near 160 K at 355 GHz (even better values have been recorded below 310 GHz), up to about 265 K at
330 GHz. On the sky, SSB system temperatures below 600 K have been obtained under good
conditions. (c) Receiver C2 C2 is a single-channel receiver which covers
frequencies from about 450 to 505 GHz. In May 1993 it successfully completed commissioning at
the JCMT, and has been used for PATT observations since that time, when atmospheric conditions
have permitted. Generally this is when the opacity of the atmosphere measured at 225 GHz is less
than 0.1 at 461 GHz, and less than 0.06 at 492 GHz. Two Gunn oscillators (overlapping at 475
GHz) are used to cover the complete frequency band; changing Gunns during an observing night is
not encouraged. DSB receiver temperatures of 190 and 220 K are typical for C2 near 460 and 490
GHz respectively. Under excellent conditions total SSB system temperatures can be less than 1000
and 2000 K respectively at these frequencies. Typical system temperatures are usually 2000 and
3000 K respectively, or better, under good observing conditions. (d) Receiver 'G'
The new SIS version of receiver G was first used at the JCMT in March 1994. Excellent results were
obtained. A Gunn oscillator gives continuous coverage across the 650-692 GHz band, which includes
both the CO (6-5) and 13CO (6-5) transitions. Observations with G are possible if the zenith opacity
at 225 GHz is less than about 0.08. Receiver 'G' has been available via a collaborative agreement
between the MPE group in Garching and the JAC, and observers interested in using it should first
contact Dr. L. Tacconi (e-mail LINDA at MPE- GARCHING.MPG.EDU for further information).
Because of the collaborative nature of the use of the receiver, it is usually offered for a limited time
period only. If the usual pattern of availability is followed it seems unlikely that receiver G will be
offered in semester 95B however, and it is likely to be replaced subsequently by the upper band of
receiver W (see below). (e) Forthcoming spectral line receivers. B3i will
ultimately be replaced by a dual-channel receiver (B3) to be delivered in summer 1995 for
commissioning in July. It should be available for use in semester 95B. The performance of B3's
mixers should be better than that of B3i, with a DSB receiver temperature of typically 100 K from
325 - 360 GHz. The instantaneous bandwidth should be greater, also, but the tuning range is likely
to be somewhat less than that of B3i. Early in semester 95B, a dual-mixer dual-waveband SIS
system (Receiver W; 'W' is for 'wide-band optics') for the C- and D-band windows should be
commissioned (current estimates place its delivery to Hilo at late summer 1995). Receiver W will
likely replace both C2 and G. The goals are for W to cover the ranges 430 - 510 GHz and 625 - 710
GHz. The sensitivity of W should easily exceed that of C2; no estimates can be given yet for the D-
band window. (f) Spectrometer Backends The Digital Autocorrelation
Spectrometer (DAS) has 2048 delay channels having a total maximum bandwidth of 920 MHz in
each of two inputs. It is capable of a wide range of configurations, with spectral resolutions of
between 0.14 and 1.5 MHz. The widest bandwidth modes are useful only for receivers (such as C2)
with sufficient IF bandwidth. 750- and 760-MHz configurations are available to make use of the full
IF bandwidths of receivers A2 and B3i. In some cases it is possible to observe several lines
simultaneously with good resolution. The AOSC is an acousto-optical spectrometer which offers
a resolution of about 330 kHz and a total bandwidth of 500 MHz for a single IF channel. The AOSC
serves as a backup for the DAS. Receiver G has its own dedicated AOS. Further details
regarding both spectrometers are given in the User's Guide. (g) Approximate rms
sensitivities after 30 minutes' integration Below is a table of the calculated rms noise in
Kelvin after a total observation time of 30 minutes (this assumes 15 minutes on source, 15 minutes
on a reference position) at selected line frequencies, for three different atmospheric transmissions. In
the first case, a 'typical good' value is used for the system temperature, based on the observed
distribution of values over the last six months. In parentheses, the expected values of the rms noise
are given for 'exceptional' (corresponding to a water vapour pressure of 0.5 mm in all cases), and
'marginal' weather conditions. In the latter case the highest value of water vapour pressure (given in
terms of zenith optical depth at 225 GHz; 'tmax' below) at which we recommend observations for the
given frequency is used. The behaviour of atmospheric transmission with water vapour pressure
impacts strongly on the system temperatures of receivers B3, C2 and G, and conditions worse than
'marginal' render observations unrewarding.
Table 2. Summary of spectral line sensitivities.
Freq. Rec. Trx Tsys dv tmax Rms noise (K)
(GHz) (K) (K) (MHz) Typical (good, poor)
230 A2 95 400 0.38 0.20 0.035 (0.026, 0.059)
266 140 600 0.38 0.20 0.052 (0.036, 0.093)
331 B3i 265 1500 0.38 0.10 0.130 (0.087, 0.250)
345 180 800 0.38 0.15 0.070 (0.057, 0.220)
461 C2 190 3000 0.38 0.08 0.260 (0.150, 0.860)
492 220 3800 0.38 0.06 0.330 (0.240, 1.020)
661 G 1100 17000 1.00 0.08 0.820 (0.430, 3.400)
692 800 18000 1.00 0.08 0.840 (0.400, 4.500)
In this table, the calculations have been made assuming an observing elevation of 60 degrees, and
(except for receiver G) use of the DAS in its 500-MHz standard configuration. The transmission in
the 'exceptional' and 'marginal' cases has been derived from IRAM's ATM routine (authored by
Stephane Guilloteau). Estimates for G are based on March 1994 performance. Most spectral-
line observations are carried out either in position-switched or beam-switched mode. In the first case,
the reference position is given relative to the source position. In the second instance, the secondary
mirror position is 'chopped' at a rate of 1 Hz, with a throw of typically 1 to 3 arcmin. For
relatively narrow line sources frequency switching is an attractive option. The chief advantage of this
technique over either position- or beam-switching is that the telescope never leaves the source
position. Thus its use reduces the rms noise by a factor of 1.4 over those values given in the above
table for the same total integration time. Frequency switching is implemented in hardware for B3i
(and presumably also B3), and via software ('slow frequency switching') for A2 and C2.
Spectral line mapping is usually done in a position- or frequency-switched mode, on a grid of
positions. When the lines are strong (say, more than 2 K), it will be possible to use the on-the-fly
mode of observing, in which the telescope is scanned at a rate corresponding to an integration time of
not less than 5 seconds per point. This method is being developed, and is not offered for regular use
at present. Continuum Observations (a) UKT14 Until displaced by
SCUBA (see below) the UKT14 bolometer system will be available for observations with filters at 2,
1.3, 1.1, 0.85, 0.8, 0.75, 0.6, 0.45 and 0.35 mm. The aperture of the bolometer can be adjusted
between 21 and 65 mm. Sensitivities range from typically 0.3 Jy/sqrt(Hz) through to 10 Jy/sqrt(Hz)
under good photometric conditions. The properties of UKT14 using the various available filters
and apertures are given in the following table. The wavelength corresponds to the effective value for
a precipitable water vapour of 1 mm, and a thermal blackbody (e.g. a planet). The value of
the NEFD given is that which should be obtained under 'good' conditions for a 65 mm aperture; users
should use this value to estimate time requirements. In parentheses, values for the 'best' and 'poor'
atmospheric conditions are given to indicate typical ranges obtained. The aperture which gives a
diffraction-limited beam is given in the table; photometry will normally be carried out with full
aperture (65 mm). Beam maps are available via anonymous FTP, as noted above. Photometry is
carried out by chopping the secondary mirror at several Hz, with a throw of 1-2 arcmin in azimuth
usually. Most mapping with UKT14 is done in a continuous scanning ('on-the-fly') mode.
(b) UKT14 polarimeter So long as UKT14 is available, the Aberdeen/QMW
polarimeter also will be offered as an optional accessory for it. The effective NEFD of the
polarimeter/UKT14 combination is slightly worse than NEFD(p) = 2xNEFD/P, where P is the degree
of polarisation of the source and NEFD is that for the filter/waveplate in question for UKT14 alone.
Observations are possible at 1100, 800, and 450 microns. Additional information appears in the
User's Guide. (c) SCUBA The submillimetre bolometer camera SCUBA is not
expected to arrive in Hilo before late summer 1995. After undergoing tests in Hilo it will displace
UKT14 on the left-hand Nasmyth platform, in order to undergo mechanical, electrical and cryogenic
fitting. It will not be available for astronomical observations until some time later following a
lengthy commissioning period.
Henry Matthews / JAC
Table 3. Properties of the UKT14 bolometer system.
Filter Wavelength Centre Band- Aperture Beam- NEFD Notes
Freq. width width (65 mm aperture)
(mm) (mm) (GHz) (GHz) (mm) (") Jy.sqrt(sec)
2.0 1920 150 40 65 27 0.8 (0.7, 1.2) 1
1.3 1260 233 64 65 19 0.5 (0.4, 1.0)
1.1 1090 264 74 65 19 0.4 (0.3, 1.0)
0.85 850 354 30 47 13 0.8 (0.7, 5.0)
0.8 790 384 103 47 13 0.5 (0.4, 5.0)
0.75 750 411 28 42 13 0.9 (0.7, 5.0)
0.6 625 480 119 36 11 5.0 (3.0, * ) 2
0.45 444 682 84 27 8 5.0 (3.0, * ) 3
0.35 351 864 113 21 6 10.0 (6.0, * ) 3
Notes: (1) At 2 mm UKT14 is poorly matched to the telescope. (2) This
filter is best avoided. It is difficult to obtain consistent calibrations, due to deep atmospheric
absorption lines in the window. (3) Observations are not possible under 'poor'
conditions at these wavelengths.
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