The propagation of radio signals in the medium frequency band (MF: 300kHz-3MHz), the high frequency band (HF: 3MHz-30MHz) and even the very high frequency band (VHF: 30MHz-300MHz) is largely influenced by the condition of our sun and, through the emissions of our sun, also the earth magnetic field that captures these. Because of its importance for certain radio communications, a number of observatories continuously monitor the condition of the sun and the geomagnetic field. Follow the steps outlined in this section to get an instant view on how propagation conditions are right now. If you are completely new to the topic of shortwave propagation, then have a look at AE4RV's HF Radio Propagation Primer (Flash movie!).

Current Solar-Geophysical Data Dashboard

Sunspots
Click to open!
SIDC Belgium
Solar Flux
X-ray Solar Activity of past 24h
(X-ray, past 24h) N3KL

SF  ·104 jansky @ λ = 10.7cm
D-Region Absorption
Click to enlarge! Next update in minute. SWPC
Coronal Holes
& CMEs

Click to enlarge!
SpaceWeather, SOHO & SXI
Solar Wind
Click to enlarge! Click for an explanation about the dials. Next update in minute(s). SWPC
Aurora
Click to enlarge! Click to enlarge! Next update in minute(s). SWPC
Sunspots &
Coronal Holes

Click to enlarge!
DXLC Norway & SOHO

Geomagnetic Field
Geomagnetic Field Activity
(based on real-time mid-latitude K) ON4AA

A  (mid-latitude daily average)
K  (mid-latitude 3h average)
Next update in minute(s).

An overview of the current solar and geomagnetical conditions is presented below.

The first step towards some serious real-time HF propagation forecasting is collecting the solar-geophysical data of the moment (i.e. solar flux and geomagnetic planetary A- & K-indices) from the Latest Geophysical Alert Message - WWV Broadcast printed in the white frame below.

This information is automatically refreshed every 10 minutes past the hour.
Next update in minute(s).
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Terminology

You are eager to learn more about the terms that are used in solar-geophysical reports?

Visit NOAA's Space Weather Prediction Center!

If you are in a hurry to learn, have a quick look at this Glossary of Solar Terrestrial Terms of NOAA's Space Weather Prediction Center, formerly known as the Space Environment Center (SEC).

For those who have more time to read: David A. Rosenthal compiled a very instructive and more comprehensive primer, published by Radio Netherlands, that helps us to understand solar-geophysical alert broadcasts.

by David A. Rosenthal (Radio Netherlands)

Summary of Solar-Geophysical Effects on HF Propagation

In general, the augmented electromagnetical solar flux originating from sunspots has a positive effect on HF propagation by improving the ionisation of the ionosphere and thereby increasing the maximum useable frequency (MUF) of the ionospheric layers, as well as their respective hop distances.

However, sunspots may exhibit a propensity to produce giant solar flares or prominences, staying for minutes to hours. The X-rays and particles originating from these flares are capable of causing sudden shortwave radio fadeouts on sunlit paths due to increased D-layer absorption starting at the lower bands and moving up with flare intensity. In the case of an , an or a be sure to monitor the absorption curve on SEC's D-region absorption chart. During quiet episodes of solar activity, this graph will remain void.

Structure of the Sun

In an other, slightly more delayed mechanism, particles escaping from the Sun's Coronal Holes (CHs) or freed during Coronal Mass Ejections (CMEs) travel at high speed through space along the Sun's interplanetary magnetic field. This is called the solar wind. CH particles need 5 days to reach Earth, CME particles only 4. When they get trapped by the Earth's geomagnetic field they cause aurora upon entering the Earth's atmosphere at the magnetic poles. The effect is more pronounced when the z-component of the interplanetary magnetic filed Bz is pointing south relative to the Earth's magnetic poles (see leftmost dial). On 160m, signals paths crossing an aurora zone are often completely lost or severly skewed.

Geomagnetic disturbances , reflected in higher A- and K-indices, might bring good DX to the VHF enthusiasts among us, but will have detrimental effects for propagation starting at the lower bands (≤10MHz).

An explanation by the experts: The Earth's magnetic field causes the ionosphere to become anisotropic. Hence, incident plane waves entering the ionosphere will split in an ordinary and an extraordinary wave. Upon exiting the ionosphere, both modes would normally recombine into a single plane wave, if it were not for the polarisation changes caused by the geomagnetic disturbances. This results in signal loss. The effect is called Faraday rotation.