My radio telescope has five channels, as follows:
1. Solar Observation Channel, using a large satellite TV antenna, centre frequency 12 GHz - for observation of sunspot activity.
2. Milky Way Observation Channel, using a 1m parabolic mesh antenna, centre frequency 1.42 GHz - for observation of hydrogen clouds in the Milky Way galactic arms.
3. Meteor Detection Channel, using a folded dipole antenna modified with a parasitic back-reflector, centre frequency 50.408 MHz - for observation of meteor activity utilising the British Astronomical Association GB3MBA radio beacon.
4. Sudden Ionospheric Disturbance (SID) Channel, using an L-shaped antenna with an electrical length of 7 ft (horiz) x 14.3 ft (vert).
5. Aurora Detector Channel, employing a remote electric field antenna and local magnetic field antenna to give a combined audio output.
The surface of the Sun that we observe in the visible is called the photosphere. But the lower region of the Sun's atmosphere is called the chromosphere and, together with the corona, is where most of its radio emissions arise.
The thermal component of solar radiation follows the black body law and is predominant at high frequencies (Infrared, f> 300 GHz & also some high-end radio waves, f> 3 GHz), while the non-thermal component (synchrotron radiation) is predominant at lower frequencies (microwave, f <3 GHz).
Note: Infrared spectrum is 300 GHz to 400 THz.
My telescope is picking up mainly synchrotron radiation, produced by charged particles being accelerated by the sun’s magnetic field.
SOLAR REGIONS
An active Sun has much larger flux density than does a quiet Sun in the frequency range between 100 MHz (3-m wavelength) and 30 GHz (1 cm wavelength). So the telescope is ideal for picking up flare activity.
Synchrotron radiation occurs when a moving, charged particle is accelerated by magnetic field lines in a direction perpendicular to its movement, i.e., outwards from the sun.
NOTE: the condition for the production of an EM wave is acceleration of charged particles.
Sub-burst during flare showing strong Type III fine features, which were audible during demodulation as a whistle falling in pitch. These fine features are believed to be caused by outward radiating beams of nonthermal electrons, their frequency falling as the solar medium becomes less dense.
There are three forms of hydrogen that exist in our galaxy:
(1) HI – neutral hydrogen. This naturally radiates electromagnetic radiation at 1.420405752 GHz (21 cm wavelength), due to a phenomenon known as electron spin-flip. The signal is very weak and sits amidst the general 'noise', but my radio telescope is able to detect that peak by employing spectrum averaging software, which elevates the wanted signal sufficiently above the noise floor for detection.
(2) HII - ionised hydrogen. Atoms of this form of hydrogen comprise single protons whose electrons have been removed during high-temperature events in space. When hydrogen is ionised, a soup of free electrons and free protons is created. Hence, as these particles are charged, they generate electromagnetic radiation when they accelerate, collectively producing a strong, smooth continuum of frequencies.
(3) H2 – molecular hydrogen. This is radio-silent but its presence can be inferred by observing the behaviour of the cold HI envelope that always surrounds it.
For more in-depth details of hydrogen detection physics and the techniques I use, please follow this link: DETAILED EXPLANATION
At a basic level, what is interesting is that the peak signal frequency of the HI will vary depending upon whereabouts the telescope is aimed within the galaxy. This is due to the fact that different parts of the galaxy are moving at different relative velocities to us on Earth (due to the galactic rotation and other localised phenomena), and so this causes the radiated frequency to be modified by the Doppler Effect.
This radial velocity (velocity along the line of sight of the telescope) can actually be calculated by noting the observed frequency of the peak measured by the telescope and applying a calculation.
Using this technique, I can plot a radial velocity map of the observed parts of the Milky Way and, from any large velocity changes, distinguish between different galactic arms.
The arms of the Milky Way are shown below:
The diagram above is one of my samples of the galactic hydrogen response. The HI peak is very small and embedded in all the noise that is visible in the top centre display. However, as a result of integration (averaging over a number of seconds) its amplitude adds coherently from the many samples taken during this time period, whereas the noise integrates in a random fashion. This results in the amplitude of the signal rising above that of the noise, and it can be seen as the peak in this spectrum screenshot.
In this sample, the frequency peak is shifted from the natural emission frequency of molecular hydrogen due to a Doppler component caused by the fact that the cloud is approaching us (in relative motion terms) at a radial velocity of approximately 6 km/s.
I detect meteors using a signal from a beacon located near Nottingham, see: Meteor Beacon
This beacon transmits a radio signal at 50.408MHz (CW) vertically upwards into the region where meteors entering the earth's atmosphere burn up and interfere with radio signals, a phenomenon that occurs at an altitude of 80 to 100km in the thermosphere.
This signal can be detected using a suitable antenna and receiver at distances within about 1200km of the beacon.
This channel of the telescope can also be used for the detection of aurora activity and transient phenomena, such as the lower frequencies of radiation associated with gamma ray bursts.
Meteor head echo captured during the Delta Aquarid shower in late July 2025
This channel is sensitive to SIDs, such as those occurring eight minutes after a solar flare burst.
The operational bandwidth of this detector is focused upon the Very Low Frequency (VLF) radio band, which ranges from 3 kHz to 30 kHz. I usually centre its receiver at around 23 kHz.
SIDs are caused by the emission of X-rays and ultraviolet radiation that increase the ionisation of the ionosphere, particularly in the D-layer (50 to 90 km from earth’s surface), an effect that either attenuates or accentuates VLF radio signals.
NOTE: The antenna is non-resonant at VLF, acting as a voltage probe for electric field detection.
This was an M-class flare with eight bursts within it showing Class III fine features. But what I have shown here is two samples of the SID channel noise level.
It is clear that the noise level of BURST 7 sample is lower than that of the out of burst sample, which is consistent with the UV and X-rays in the solar burst causing an increase in ionisation of the D-layer of the ionosphere and increasing its refractive index so that the VLF radio signals are attenuated.
My VLF aurora detector is sensitive between 300 Hz and 10 kHz and comprises two parallel channels:
(1) An electric field detector fitted with a short copper rod antenna.
(2) A magnetic field detector using a wire-wound ferrite rod antenna.
The copper rod antenna is remote from the observatory to minimise the effect of local electrical interference. The magnetic ferrite rod antenna is mounted in the observatory, suitably distanced from mains cables. Both antennae feed amplifier circuits whose outputs are then fed to a final audio stage, which drives two small loudspeakers, allowing me to 'listen' to the earth's atmosphere for auroral activity!
The sun is always emitting solar wind, a stream of charged particles that interact with the earth’s magnetic field, mostly to be deflected into space. However, when there is a strong surge of the charged particles, such as after a solar CME, a significant number of them get funnelled down towards the poles along the flux lines of the magnetic field.
Whenever this happens, a luminous aurora is generated due to the charged particles colliding with nitrogen and oxygen molecules in our atmosphere. But that is not the only effect. As a stream of charged particles is moving through a magnetic field, RF electromagnetic radiation is also produced, with strong components between 1–10 kHz
At VLF, the earth and its ionosphere collectively behave like a giant waveguide of approximately 90 km width, trapping the electromagnetic energy generated between the the conducting Earth below and the ionosphere above. The electric fields generated bounce, duct, and reinforce over enormous distances, which produces surprisingly strong electric fields.
At the ground itself, the tangential electric field must of course be zero, so the electric field lines will be pretty much vertical near the surface. And vertical fields couple extremely well to a short rod antenna, because the rod acts as a vertical capacitor plate. Electrons in it are pulled one way leaving a positive charge (the deficit of electrons) on the opposite side. And as the field alternates, the charge on the rod oscillates making a tiny current flow into and out of the rod.
The antenna is connected directly to a pre-amp, which converts this current into a measurable voltage that drives the audio amplifier and loudspeaker stage.
Meanwhile, the wire-wound ferrite rod antenna of the second, magnetic channel couples with the magnetic element of the generated electromagnetic waves, and similarly drives a pre-amp and outputs to the audio stage. So the result is a combined audible output.
Electric Field Antenna
Magnetic Field Antenna
Audio Output Stage