Since the beginning of radio astronomy several surveys of the galactic background have been made at various frequencies, but most of them covered only the limited region near the galactic plane (see e.g., Salter & Brown 1988).
It is presently known that the background continuum radiation is a mixture
of thermal free-free emission from ionized hydrogen and non-thermal synchrotron
emission resulting from the interaction of cosmic ray electrons with the galactic
magnetic field. At frequencies higher than about 1 GHz, the diffuse thermal component
becomes important in the galactic plane; for example, at 1420 MHz it may
reach 30% to 50% (Reich 1986). The non-thermal component is important at low
frequencies and increases with decreasing frequency until
the free-free absorption due to ionized hydrogen sets in at around a few tens of MHz.
Continuum surveys in this range (say 20 MHz
100 MHz) are therefore most
important to investigate the structure of the magnetic field in our Galaxy,
the spatial and energy distributions of cosmic ray electrons as well as those of the
synchrotron radio emission. However, only a few surveys, discussed in Sect. 5,
have been made in this frequency range because of inherent difficulties. For
example, to achieve a good angular resolution at low frequencies it is necessary
to build a large array; terrestrial interference (man-made and natural) generally
becomes serious with decreasing frequency; the ionospheric opacity increases as
the frequency decreases, and changes in opacity result in spurious
intensity variations of the incoming background radiation. Furthermore, solar
radio bursts fatally disturb the observation of the background radiation during
high solar activity periods.
In this paper we present the results of a northern survey at 45 MHz. The observations were made with the MU (Middle and Upper atmosphere) radar located at Shigaraki, Japan. The data processing was performed at the Maipu Radio Observatory, Chile, and the final maps were obtained at the Max-Planck-Institut für Radioastronomie, Germany, making use of the NOD2 program package (Haslam 1974).
Copyright The European Southern Observatory (ESO)