The GEM project is an on-going international collaborative effort in
the fields of radio astronomy and cosmology. The project goal is to accurately
determine the spatial distribution and absolute intensity in the radio
and microwave spectrum of the radiation emitted by the Milky Way galaxy
and by the unresolved blend of external galaxies.
Institutions actively participating in the project through
bilateral cooperation agreements are:
The project has been supported in part by the US Department of Energy,
by the US National Science Foundation, by the Progetto Italia
Antartide, by INPE-Brazil, and by Colciencias of Colombia. Some of the
publications to date are on the following
GEM publication list.
Some preliminary
GEM maps
i.e. 408, 1465, and 2300 MHz.
Scientific Motivation
Any instrument trying to measure the intensity or anisotropy of the
Cosmic Microwave Background (CMB) sees the galactic radiation as a
foreground signal, which cannot be avoided by instrumental or
observational techniques, and must be accounted for and subtracted from
the data during the analysis.
The uncertainties in the maps and in the frequency dependence
of the galactic emission at radio and microwave frequencies have become
the limiting factor in the accuracy and interpretation of the low
frequency measurements of the spectrum of the CMB, and of the COBE-DMR
measurements of the angular distribution of the CMB.
The overall sky brightness results from the superposition of
signals generated by the acceleration of relativistic electrons
(synchrotron radiation), by thermal bremsstrahlung inside hydrogen
clouds (HII radiation), and by thermal radiation of dust clouds, plus
smaller signals from external galaxies. The exact mixture of
synchrotron, HII, and dust signals depends on the observing frequency
and the region observed. The dust component is dominant at the high end
of the radio spectrum and in the IR region. Because of its spectral
index, ~1.5, the dust
contribution is negligible for observations below 50 GHz.
At intermediate frequencies the thermal HII emission is
dominant, especially in the plane of the galaxy, where giant gas clouds
provide the material and conditions for large concentrations of ionized
hydrogen. This radiation originates in the interaction of free
electrons with other ions. The HII radiation has a spectral index of
about -2.1, weakly dependent on the observing frequency and on the
(poorly known) temperature of the electrons.
At low frequencies and away from the galactic plane, the
synchrotron radiation is dominant. Synchrotron radiation is generated
by the energy loss of electrons with relativistic velocities, when
their trajectories are deflected around the field lines of the
interstellar magnetic field. The intensity of this radiation depends on
the number density of relativistic electrons along the line of sight,
while the spectral index (typically -2.75 at low frequencies) depends,
and can be determined from the energy spectrum of the electrons, and
the intensity of the magnetic field
The galactic signal has been modeled by adding together the
synchrotron emission measured at low frequency and away from the
galactic plane, with the HII signal deduced from measurements at
intermediate frequencies, and the dust emission measured in the IR.
Each component is then frequency scaled according to a power law. This
approach suffers from:
- uncertainty in the spectral index of synchrotron emission,
because of poorly determined electron spectrum and magnetic field
intensity
- uncertainty in the spectral index of HII emission because
of unknown electron temperature distribution
- uncertainty in the spectral index of dust emission because
of unknown size and chemical composition of the dust grains
- poorly determined zero level of the measurements of sky
emission
- uncertainty in the absolute value of the instrument gain
- uncertainty in the time dependency of the instrument gain
- lack of sky coverage in the existing data-base
Experimental Goals
The final products of the GEM project will be a set of new, self
consistent maps at several frequencies. Features that will link these
maps together, and set them apart from the existing ones are:
- maps of constant angular resolution and beam pattern will
be produced at several frequencies between 408 MHz and 10 GHz.
- absolute calibration of the zero level of the map to
better than (1 K) * (f/408)-2.75, [where f is the observing frequency
in MHz] for f > 1500 MHz, and to better than 0.1 K for f
< 1500 MHz
The GEM project will also overcome the shortcomings of the existing
data-base by providing:
- total sky coverage
- accuracy of the gain level to better than 3%
- sensitivity to the circularly polarized component (total
intensity) of the galactic signal
GEM Instrument Operation
The Berkeley team has developed a compact and portable 5.5-m diameter
radio antenna, which has been used for the first-stage observations.
The first observations were made from near Bishop, California (fall
1993 through fall 1994 with time out for refurbishment), from de Leyva,
Colombia which is close to the equator (first half of 1995),
Teide, Tenerife, Spain (from fall 1995 through fall 1997),
and was moved to Cachoeria Paulista Brazil in 1998 with plans to move
and operate in Rio Grande de Sul, Brazil beginning early 1998.
The project fell far behind schedule (funding and other issues)
and the current plan is to move to Brazilia in 2001.
Receivers currently are operational at 0.408, 1.5, 2.3, and
5.0 GHz. A prototype for 10 GHz has been constructed and upgrades are
planned.
The results of the observations and the equipment operating in
each location
are shown in these
pictures.
- 1991
Construction Bldg 60 LBL
- 1991/1992
South Pole, Antarctica
- 1993-1994
Bishop, California, USA 1995
Education
, Outreach from Bishop effort
- 1995 (1st half)
Villa de Leyva, Colombia
- 1995-1997
Teide, Tenerife, Spain
- 1998-
Cachoeria Paulista, Brazil
- 2001-
Brasilia, Brazil
- 2001- Mounting the Antenna, Brazil
- 2005- 5GHz Receiver installed at Cachoeria Paulista, Brazil
GEM Instrument Description
Berkeley team has developed a compact and portable 5.5-m diameter radio
antenna, which will be used for the first-stage observations. It
consists of a deep parabolic reflector, which can be illuminated either
via a prime-focus mounted feed antenna, or a Cassegrain optics. The
reflecting surface is surrounded by a set of metallic ground screens,
which reduce the beam spillover and the signal from the ground via the
antenna side lobes. The ground screens extend the diameter of the
parabolic antenna to 9.5 meters.
GEM
description material
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