Australian Cosmic Ray Modulation Research
M. L. Duldig
, PASA, 18 (1), in press.
Next Section: Recent Instrumentation
Title/Abstract Page: Australian Cosmic Ray Modulation
Previous Section: The Early Years
Contents Page: Volume 18, Number 1
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Subsections
Establishing the Australian Network of Observatories
Surface Muon Telescopes
In parallel with the development of the East-West
experiment in Hobart the Physics Department at Melbourne
University also began research in cosmic rays. The research team
included several notable names including David Caro, Fred Jacka,
John Prescott and Phil Law. A Geiger Müller four tray
telescope and an ionization chamber were developed. This
equipment made observations from Melbourne. Three further sets of
equipment were constructed for deployment when the newly formed
Australian National Antarctic Research Expeditions (ANARE) bases
were opened. In the summer of 1947-48 one set of equipment was
sent to each of Heard and Macquarie Islands and the final set was
operated from the HMAS ``Wyatt Earp''. The testing and operation
of the equipment and the ``Wyatt Earp'' voyage is described in Law
(2000). The results from the voyage were published the same year
as the expedition (Caro et al. 1948). In 1949 the equipment was
returned from the islands for overhaul and maintenance but in 1950
the Melbourne group decided to discontinue cosmic ray research,
putting its efforts into nuclear physics instead. Phil Law
invited the Physics Department at the University of Tasmania to
take over the ANARE work and Geoff Fenton was put in charge.
Early in 1949 the Hobart group was already building an East-West
telescope similar to the one above for deployment to Macquarie
Island. This experiment was established on the island in 1950 and
operated alongside the Melbourne University experiment. A
replacement telescope for the Melbourne University instrument was
constructed at Hobart during 1951 and deployed the following
summer. It continued operating until 30 March 1959 when fire
destroyed the cosmic ray laboratory at Macquarie Island. Perhaps
the most significant result from the instrument was the recording
of the giant flare-induced Ground Level Enhancement (GLE) observed
worldwide in February 1956 (Fenton et al. 1956). The East-West
telescope had been returned to Hobart at the end of 1951. A
description of the Macquarie Island experiments and operations can
be found in K.B. Fenton (2000).
N.R. (Nod) Parsons was appointed as the Australian Antarctic
Division's officer in Hobart for the cosmic ray program following
the changeover in responsibility for the research from Melbourne
University to the University of Tasmania. Nod had been involved
with the programs at both universities and had ``wintered'' at
Macquarie Island with K.B. (Peter) Fenton in 1950. The Mawson
station was established in 1954 on the Antarctic Continent and a
cosmic ray laboratory was added the following year. This housed a
vertical telescope and an inclined telescope that could be set to
any desired zenith angle and automatically rotated each hour to
the next azimuth of a preset series. Nod Parsons was responsible
for the installation and commissioning of the equipment and handed
over a fine facility to R.M. (Bob) Jacklyn at the end of the year
for the International Geophysical Year. Bob would later take over
as head of the Australian Antarctic Division research program.
These telescopes and various upgraded replacements continued
operating at Mawson until 1972 when a new laboratory was
constructed at the station that incorporated underground
observations.
During August 1953 a vertical telescope was installed at the
University campus in Hobart. A new cosmic ray observatory was
constructed on the campus in 1975 and a new vertical telescope was
run in parallel with the old one for some time. Continuous
recording has continued to the present giving almost 50 years of
data.
Ken McCracken installed a small 60 cm square muon telescope at Lae
at the same time as the neutron monitor was installed (see Section
3.3 below).
In 1968 a new telescope system was added to the Mawson cosmic ray
observatory. This consisted of two units viewing north and south
at a zenith angle of 76o giving an effective atmospheric
absorber depth of 40 metres water equivalent (mwe). This
experiment would complement observations from the Cambridge
underground telescopes (see Section 3.2 below) and
results from the observations supported the case for an
underground observatory at Mawson. A small vertical telescope was
also operated at Macquarie Island in 1969.
The new observatory at Mawson was constructed during 1971 and
early 1972 as described below. The surface telescopes comprised
three north and south high zenith angle crossed systems using
coincidences between vertical walls of Geiger Müller counters
to view at the same zenith angle as the inclined system in the old
observatory. The south pointing telescope viewed across the
geographic pole into the opposite temporal hemisphere as well as
perpendicular to the local geomagnetic field. The result of such
a view was to spread the rigidity dependent responses in time due
to geomagnetic deflection (see Section 6.1.1 below) of
the incoming particles. The northern view reached equatorial
latitudes which, in partnership with the underground system, gave
complete southern hemisphere coverage from a single observing site
(Jacklyn et al. 1975). These surface counters were replaced by
larger area multi-zenith angle proportional counter systems during
1986 and 1987 (Jacklyn & Duldig 1987; Duldig 1990).
Underground Muon Telescopes
One of the most important early developments was
the decision by Geoff Fenton to operate underground telescopes in
a disused railway tunnel at Cambridge near Hobart. The depth was
shallow enough that the counting rate was still sufficiently high
for useful studies and, perhaps more fortuitously, not so shallow
that changes in atmospheric structure would have complicating
effects on the telescope response. This latter feature was not
known at the time. At the selected depth studies of both solar
and sidereal variations and their energy dependencies could be
investigated. The instruments, based on those already put into
operation at Mawson by Nod Parsons, commenced observations on 19
July 1957 (Fenton et al. 1961).
Planning for further underground telescopes was well underway in
the early 1970's. A deep underground system was installed in the
Poatina power station in central Tasmania late in 1971. The depth
of 357 mwe meant that the observations should be at energies
beyond the influence of solar modulation but the count rate was
also low and several years of observation would be required to
obtain significant results for the sidereal anisotropy (Fenton &
Fenton 1972, 1975; Humble et al. 1985; Jacklyn 1986).
Also during 1971 construction of the new Mawson
surface/underground observatory was commenced (Jacklyn 2000). Bob
Jacklyn, who had assumed leadership of the Australian Antarctic
Division cosmic ray program, optimized the available telescope
viewing directions to take advantage of both the geographic polar
location and the position of the Mawson station relative to the
magnetic pole. Telescopes were designed and constructed by Attila
Vrana to put these plans into place. An 11 m vertical shaft was
blasted into the granitic rock and two chambers were excavated at
the bottom of the shaft. A surface laboratory was then
constructed over the shaft. One underground chamber housed five
cosmic ray telescopes. The remaining chamber was used for seismic
observations. Three telescopes viewed north at a zenith angle of
24o. This is aligned to the local magnetic field and the
response is thus unaffected by any geomagnetic deflection of the
arriving cosmic ray particles. Two smaller telescopes viewed
south-west at 40o zenith angle. After accounting for
geomagnetic bending (see Section 6.1.1 below) the view
of these telescopes is effectively along the Earth's rotation
axis. They are therefore insensitive to the daily rotation of the
Earth, viewing a fixed region over the south pole. Changes in
their response do not arise from scanning an anisotropy but rather
from isotropic variations in the cosmic ray density (i.e. changes
in the total number of cosmic rays) near the Earth. Both the north
and south-west telescope systems were subsequently upgraded to
proportional counter systems in the early 1980's (Jacklyn &
Duldig 1983).
The Neutron Monitor Network
During 1955 Ken McCracken began construction of
Hobart's first neutron monitor as part of his PhD studies
(McCracken 2000). This monitor followed the Chicago design
developed by John Simpson (Simpson et al. 1953) that was later
adopted as the standard neutron monitor for the International
Geophysical Year (IGY). The counters thus became known as IGY
counters and installations of this type are described by the
number of counters followed by the mnemonic (eg 12 IGY). Because
the count rate of neutron monitors increases rapidly with altitude
the new instrument was sited at ``The Springs'' on Mt Wellington,
700 m above sea level. At the time this was the highest point on
the mountain with good road access and electrical power. The
counters employed BF3 gas enriched in B10. Cosmic ray
neutrons interact with lead surrounding the counters producing
additional neutrons. These neutrons were further thermalized when
passing through an inner paraffin moderator so that the cross
section for neutron capture by the Boron was optimal. Paraffin
also surrounded the lead to act as a partial ``reflector''
redirecting some of the scattered neutrons back toward the
counters. The neutron capture by Boron produced an
-particle and a Lithium ion which were then detected by
the proportional counter as a pulse, amplified and counted.
For an extensive review of neutron monitor design see Hatton
(1971).
The monitor was installed at ``The Springs'' in July 1956,
unfortunately after the giant GLE of February. As part of the IGY
several other monitors were also being constructed at this time.
One was sent to Mawson and installed in early 1957 and another was
installed at Lae, New Guinea in April of the same year (McCracken
2000). IGY counters were added to the network at Brisbane, Casey,
Darwin, Wilkes and on the University campus in Hobart (Table
1). The Wilkes monitor was moved to Casey station with the
rest of the Australian Antarctic operations in that region in
1969. The Mt Wellington monitor was destroyed by the major
bushfires of 1967 around Hobart. An improved monitor design
(Carmichael 1964), known as NM-64 or IQSY (International Year of
the Quiet Sun) monitors, led to the eventual replacement of most
IGY monitors worldwide. Installations of this type are also
described by the number of counters followed by the mnemonic (eg
18 NM-64). The Darwin monitor was constructed using the new design
in 1967 and the Mt Wellington monitor was similarly rebuilt in
1970. Subsequently, Brisbane, Hobart and Mawson all upgraded to
IQSY monitors. For a complete worldwide history of neutron
monitor development, installation and use readers should refer to
the special issue of Space Science Reviews published recently
(Bieber et al. 2000).
Table 1:
Australian Neutron Monitor Network
| | Location |
Type |
Lat |
Lon |
Alt |
Cutoff |
From |
To |
| | |
|
|
|
|
|
|
|
| | |
|
|
|
|
|
|
|
| | |
12 IGY |
-27.50 |
152.92 |
s.l. |
7.2 GV |
30 Nov 1960 |
31 Dec 1973 |
| | Brisbane |
9 NM-64 |
-27.42 |
153.08 |
s.l. |
7.2 GV |
1 Jan 1977 |
Jun 1993 |
| | |
9 NM-64 |
-27.42 |
153.12 |
s.l. |
7.2 GV |
1 Jul 1993 |
30 Jan 2000 |
| | |
|
|
|
|
|
|
|
| | |
|
|
|
|
|
|
|
| | Casey |
12 IGY |
-66.28 |
110.53 |
s.l. |
0.01 GV |
12 Apr 1969 |
31 Dec 1970 |
| | |
|
|
|
|
|
|
|
| | |
|
|
|
|
|
|
|
| | Darwin |
9 NM-64 |
-12.42 |
130.87 |
s.l. |
14.0 GV |
1 Sep 1967 |
Oct 2000 |
| | |
|
|
|
|
|
|
|
| | |
|
|
|
|
|
|
|
| | |
12 IGY |
-42.90 |
147.33 |
15 m |
1.88 GV |
1 Mar 1967 |
22 Nov 1977 |
| | Hobart |
12 IGY |
-42.90 |
147.33 |
18 m |
1.88 GV |
1 Nov 1975 |
- |
| | |
9 NM-64 |
-42.90 |
147.33 |
18 m |
1.88 GV |
1 Apr 1978 |
- |
| | |
|
|
|
|
|
|
|
| | |
|
|
|
|
|
|
|
| | Kingston |
9 NM-64 |
-42.99 |
147.29 |
65 m |
1.88 GV |
20 Apr 2000 |
Nov 2000 |
| | |
18 NM-64 |
-42.99 |
147.29 |
65 m |
1.88 GV |
Nov 2000 |
- |
| | |
|
|
|
|
|
|
|
| | |
|
|
|
|
|
|
|
| | Lae |
3 IGY |
-6.73 |
147.00 |
s.l. |
15.5 GV |
1 Jul 1957 |
28 Feb 1966 |
| | |
|
|
|
|
|
|
|
| | |
|
|
|
|
|
|
|
| | |
12 IGY |
-67.60 |
62.88 |
15 m |
0.22 GV |
1 Apr 1957 |
11 Oct 1972 |
| | Mawson |
12 IGY |
-67.60 |
62.88 |
30 m |
0.22 GV |
1 Jan 1974 |
12 Feb 1986 |
| | |
6 NM-64 |
-67.60 |
62.88 |
30 m |
0.22 GV |
13 Feb 1986 |
- |
| | |
|
|
|
|
|
|
|
| | |
|
|
|
|
|
|
|
| | Mt |
12 IGY |
-42.92 |
147.24 |
725 m |
1.89 GV |
Jul 1956 |
31 Jan 1967 |
| | Wellington |
6 NM-64 |
-42.92 |
147.24 |
725 m |
1.89 GV |
5 Jun 1970 |
- |
| | |
|
|
|
|
|
|
|
| | |
|
|
|
|
|
|
|
| | |
|
Tasmania and Delaware Universities and
the Australian Antarctic |
| | Transportable |
3 NM-64 |
Division are presently using this instrument for annual ship-borne |
| | |
|
latitude surveys between Seattle and McMurdo |
| | |
|
|
|
|
|
|
|
| | |
|
|
|
|
|
|
|
| | Wilkes |
12 IGY |
-66.42 |
110.45 |
s.l. |
0.01 GV |
5 Mar 1962 |
9 Apr 1969 |
| | |
|
|
|
|
|
|
|
Liaweenee Air Shower Experiment
In the early 1980's it was becoming clear that the
sidereal daily variation at energies of 1012--1014 eV
had an amplitude of about 0.05% as measured by deep underground
and small air shower experiments in the northern hemisphere. The
only measurements in the southern hemisphere were from the Poatina
power station telescopes at the bottom end of this energy window
(Fenton & Fenton 1975; Humble et al. 1985; Jacklyn 1986). A new
air shower experiment was therefore installed in the central
plateau region of Tasmania at Liawenee (Fenton et al. 1981, 1982;
Murakami et al. 1984). This experiment showed that the southern
hemisphere sidereal response was much smaller than the northern
hemisphere at 0.02% (Fenton et al. 1990) which was to have
important implications for understanding the structure of sidereal
anisotropies (see Section 7 below).
Next Section: Recent Instrumentation
Title/Abstract Page: Australian Cosmic Ray Modulation
Previous Section: The Early Years
Contents Page: Volume 18, Number 1
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© Copyright Astronomical Society of Australia 1997