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Navigation:: Home >> Radio signal propagation >> this page Sudden Ionospheric Disturbance (SID)- overview of the sudden ionospheric disturbance, SID, that affects HF radio signal propagation
Sudden Ionospheric Disturbances or SIDs are often experienced on the HF or short wave bands where they may also be called blackouts, short wave fades (SWF), or they are sometimes referred to as the Dellinger effect, after the person who first noted them. As the name implies they occur suddenly, and they cause a blackout of ionospheric radio propagation for a number of hours. This may cover part, or even all of the HF radio spectrum. Cause The radiation from the Sun caused by the flare is not limited to one form of radiation, but it includes all forms including a high level of X-rays. The X-rays are able to penetrate through to the D layer or D region of the ionosphere and as a result they give rise to a high level of ionisation in the D region. This results in a very significant increase in the level of D region attenuation. Although the increase in the level of radiation is rapid, it takes time for the level of ionisation to rise. As a result the lower frequencies are affected first, and as the degree of ionisation increases, so the higher frequencies are affected. During a normal day the D region normally affects frequencies up to two or three MHz, but the increase in radiation from a flare can cause much higher frequencies to be affected. Often it can result in a complete black out of the HF bands. At other times a SID may only affect the lower frequencies. Other effects
Summary of the effects of solar disturbances
SID duration It is also worth noting that it is only the sunlit side of the earth that is affected. Any areas that were in darkness when the flare occurred escape the effects. A further effect of a flare is that at the same time as the X-ray radiation reaches the Earth giving rise to a blackout, it is found that noise bursts from the increased levels of radio frequency radiation may be monitored at VHF.
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