Propgtn HF/LF propagation question

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radar_hunter

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So we know the two general rules for propagation:

a) High solar activity is generally beneficial for MF/HF propagation because it increases F and E layer ionization which makes reflections from these layers stronger. Upper HF propagation only occurs when solar activity is high.

b) Solar flares and CMEs can degrade MF and lower HF propagation because they increase ionization in the D layer which absorbs lower frequencies. This may happen even during the night when D layer is normally absent.


But some things are still unclear to me:

1) Are there any other ways how solar storms cause propagation conditions to degrade? It seems to me that propagation may get worse even well above 10 MHz which should be less affected by the D layer. One site mentioned ionospheric instability but it wasn't a very scientific source.

2) How do solar conditions affect longwave (LF) and VLF propagation? I have vaguely noticed that longwave stations may be stronger under conditions that result in poor HF propagation. I'm not very sure. There's some information on HFunderground propagation page, it states that longwave propagation may increase at the onset of a solar storm but then it would degrade too.
 

13dka

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OK, I'm definitely not an expert on ionosphere physics but since nobody bites... :)

a) High solar activity is generally beneficial for MF/HF propagation because it increases F and E layer ionization which makes reflections from these layers stronger.

So far correct but to apply this broadly to MF and HF isn't really helpful: What the higher ionization does is increasing the MUF (Maximum Useable Frequency). MF is always far below both the MUF and the critical frequency (at which vertical incidence signals still get reflected), even in the worst case - winter in a solar minimum.

Upper HF propagation only occurs when solar activity is high.

No. Well, depends on what you call "upper HF". :) Upper HF propagation occurs as long as the the MUF is just high enough to allow refraction of waves hitting the F-layer at a very low angle of incidence for a given frequency (the MUF is decreasing when the angle of incidence increases until it is = critical frequency). Surprisingly, this is almost always the case even with the lowest solar minimum flux indices (SFI <70) for frequencies up to 20 MHz and that can sometimes reach 28MHz when the flux increases just a little (e.g. SFI >70)...as long as the ionosphere is undisturbed and the geomagnetic indices stay low.

However, since both the signal strengths and the incidence angles are low in these very baseline propagation conditions, this can be observed only in optimal reception conditions (zero local noise, low receiver noise, high antenna gain/directivity/flat takeoff angle). If any of these conditions are not met (which is the case for most of us at home), the band will appear "closed".

Here's a video shot under this kind of minimum (zero sunspots) conditions (SFI=70, A=3, K=1, nothing to phone home about!) on September 20th, 2020, mostly in the dark:


Here's 28 and 24MHz on June 5th a year later, with SFI=74-77, A=4, K=1, literally in the middle of the night (1:24am local time):


b) Solar flares and CMEs can degrade MF and lower HF propagation because they increase ionization in the D layer which absorbs lower frequencies.

I think it's important to distinguish between flares, CMEs and solar storms in this context. Flares affect mostly the day side of the planet, so MF is for the most part not much affected due to the D-layer preventing skywave propagation anyway. Flares can be responsible for rather short-term upper HF enhancements or the opposite - radio blackouts (depending on the flare severity) while CMEs cause slower, generally detrimental and more long-term interactions with the ionosphere and magnetosphere, up to solar storms. Unfortunately, my understanding of these interactions re HF and MF propagation is bad to non-existent.

This may happen even during the night when D layer is normally absent.

Not sure about what exactly happens at night. As experiments in solar eclipses have shown, the D-layer ionization drops significantly even within the few minutes of a total eclipse, where the moon shadow hits the ground. However, the ionosphere seems to respond with some sluggishness to X-rays, EUV and whatnot dramatically increasing the electron density in its layers, so it may extend into the night.

Related to that and probably with more impact, the season and propagation path must be considered in this regard - for example, in summer on the northern hemisphere, when the northpole is continuously facing the solar wind, over-the-pole paths and generally high latitude stations are permanently affected by anything coming from the sun, which can be felt even in the short nights. When there's much activity, the polar cap can absorb MF and HF.

I'm at 54°N in Europe (Germany) and during disturbed conditions I often observe a complete absence of shortwave signals from the US except maybe FL (most paths to the Northeast, Midwest or West Coast are over or too close to the pole and therefore dead) but the Carribean and South America keep booming in. This is also one of the reasons why summer is generally bad for transatlantic MW DX, particularly in a solar maximum. :)

1) Are there any other ways how solar storms cause propagation conditions to degrade? It seems to me that propagation may get worse even well above 10 MHz which should be less affected by the D layer.

If a solar flare (or more general SID) is strong enough to saturate the D-layer we get the famous radio blackouts, which AFAIK do not affect higher frequencies less or more than lower frequencies. However, on higher frequencies they cause noise on top of the absorption and DX stations on higher frequencies are typically more in multi-hop distance than those on lower frequencies, so these bands may appear more affected.

Solar storms on the other hand are causing geomagnetic storms, which in turn cause ionospheric storms if I understood that right. They cause both degradation and enhancement or additional propagation modes like sporadic E or aurora reflection on VHF. The degradation consists of increased absorption and MUF decrease, that's why ionospheric storms affect the higher HF regions more (in their bad phases).


Screenshot 2023-10-22 at 09.47.44.jpg

2) How do solar conditions affect longwave (LF) and VLF propagation? I have vaguely noticed that longwave stations may be stronger under conditions that result in poor HF propagation

The D-layer can refract frequencies below 250kHz, so any event causing more electrons in that layer could enhance LF? Other than that, I believe the geomagnetic field has a word in this too but like I said, I don't really understand the interaction.

Some not completely unreadable gobbledygook on the topic:

 

radar_hunter

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Hm, thanks for your answer.

So to question 1), in addition to D layer absorption, there's increased noise due to as well as decrease of MUF due to ionospheric effects which were not explained in detail in the linked paper.

So far correct but to apply this broadly to MF and HF isn't really helpful: What the higher ionization does is increasing the MUF (Maximum Useable Frequency). MF is always far below both the MUF and the critical frequency (at which vertical incidence signals still get reflected), even in the worst case - winter in a solar minimum.

But does ionization level also affect the strength of reflections? For example, I don't usually receive many NDBs (at least with my current equipment) but I have observed that sometimes when the conditions are good I can receive numerous NDBs. This doesn't happen very often but I encountered it in a couple of evenings and nights during the last winter.

I think this happened with NDBs both on the "traditional" band between LW and MW broadcast bands as well as with Russian NDBs that transmit in the MW broadcast band.


To question 2), this is from HFunderground propagation page and it's the only explanation for LF propagation conditions I've seen so far:

Longwave
The Dst (disturbance storm time) index provides a measure of the Earth's geomagnetic activity. It can be used to quantify the severity of magnetic storms. Dst, expressed in nanoteslas, is based on the average value of the horizontal component of the Earth's magnetic field measured hourly at four near-equatorial geomagnetic observatories.
During a magnetic storm, the Dst shows a sudden rise, corresponding to the storm sudden commencement, and then decreases sharply as the ring current intensifies. Once the IMF turns northward again and the ring current begins to recover, the Dst begins a slow rise back to its quiet time level.
(Source: Hamilton, D. C., et al., Ring current development during the great geomagnetic storm of February 1986, J. Geophys. Res., 93, 14343, 1988.)
For longwave DXers, positive values, or at least those close to zero, are considered best.

As for D layer effects on longwave, if strong D layer could improve propagation, then longwave stations should be stronger during the day? And this does not seem to happen, I think...
I have noticed improved longwave conditions mostly when it's dark, but that may be because I'm most commonly active with radio in the evening.
 

13dka

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But does ionization level also affect the strength of reflections?

Again, I don't really know what I'm talking about, what I do know is that the interaction mechanisms are much more complicated than "higher ionization = stronger reflections". You have to differentiate between the types of radiation and amount of particles coming from the sun doing different things, and there's always a combination of enhancement and diminution going on. In other simple words, "ionization is only good until it's bad again".

Also, not sure no idea how exactly that matters in this context but there are no "reflections", which would be "bouncing off a surface" by definition. The ionosphere is not solid matter or a mirror though, it's a gaseous medium of charged particles and EM waves get refracted (=bent) while passing through it. The ionization level determines how much the waves can be bent (the "refractive index"), hence the dependence from the angle of incidence. But the waves are also subject to absorption and different refractive indices in the lower, denser layers on their way to the F-layer, that's why strong and deeply penetrating ionization through flares, radiation and solar storms is messing up things more than the baseline ionizing particle flux, giving us a nicely active F-layer without the lower layers spoiling the fun. Or the interplay between all these many factors and forces are causing oddities like "ionospheric ducts" (waves being "caught" in a kind of waveguide between ionospheric layers) or "spread-F" that are not so much related to "higher ionization", yet they enhance signals on particular paths and (that always plays a role, too) particular bands.

For example, I don't usually receive many NDBs (at least with my current equipment) but I have observed that sometimes when the conditions are good I can receive numerous NDBs.

The question is - what's the baseline? Is it enhanced conditions when reception is better or is it just less disturbed conditions? My understanding is that the enhancement we occasionally experience on shortwave (less absorption, higher frequencies being refracted) does not play a role (or not a big one) on MF. What we feel on MF might be more the downsides of these events, when propagation is disturbed? What I (personally and therefore very subjectively) observe on MF in transatlantic DX is that signal strength variations are very much seasonal and hence more related to paths than to "enhanced" or "unsettled" conditions. YMMV, depending on where you live though.

As for D layer effects on longwave, if strong D layer could improve propagation, then longwave stations should be stronger during the day? And this does not seem to happen, I think...

Yes and no, see above, it's complicated... :) The ionosphere does not necessarily have an effect on signal strength there - my understanding is that the groundwave follows the earth curvature (for reasons I don't understand yet either) much more on LF, and the broadcasters switching from "a lot" of power to "a f...ing lot" during the day keep the bigger range and the signals pretty constant - and we all observe only marginal day-to day signal strenght variations. I suspect that ionospheric effects on such a longer-range (~1,000km) groundwave broadcast signal play a lesser role, or their contribution to the signal is just harder to observe. Particularly now due to the extinction of stations below 250 kHz, with diminishing chances to observe stations far enough away (2,000km or more) to make a ionospheric component more obvious (like on MF).

However, when I "studied" the Luxemburg effect (which happens in the ionosphere) in November last year I could directly observe perfectly isolated ionospheric day/night condition differences on LF:

Observing the effect for the past weeks I noticed the relation between solar activity and the severity of the effect: In quiet periods with low A- and K-indices the effect cannot be observed during the day in my northerly position, in the aftermath of flares causing geomagnetic storms and radio blackouts I heard it even at noon.

So "disturbed" conditions due to more intense bombardment from the sun intensified the Luxemburg effect, which may or may not confirm the "D-layer refraction below 250kHz" theory (which isn't mine, it's something I read somewhere as a scientific fact). In other words, the D-layer can behave similar to the F-layer below 250kHz. In fact, I also noticed something that indicates that "refraction" and therefore "inclination angles" were affected:

Interestingly, this seems to have influence on the range in which the effect could be observed more than the signal strength of the 2 stations: The Twente SDR in Enschede (NL) is much closer to Luxemburg and has modulation on 162kHz all day, even in quiet space weather!

This was all just raising more questions though - why was the Luxemburg effect stronger at night, when Radio Luxemburg had less power and the D-layer is supposed to "cool off"? Why is the closer (=higher angle of incidence) receiver hearing this when I can't? I also never found a source that explains in which ionosphere layer the Luxemburg effect takes place, according to my observations (very variable and distance-dependent during the day, less variable and less distance-dependent during the night) the altitude in which that happens may have varied from the D-Layer (day) to the lower E-layer (night).

This document generally explains ELF/LF propagation, even though I understand less than half of it. But even if the understanding isn't quite what it should be, what's still fun and exiting about all this is that we - as radio enthusiasts - are sitting right in the lab and have the instruments to observe it all live! :)
 

WA8ZTZ

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Regarding longwave propagation, my experience has been that the best time to listen is several hours before sunrise during the Winter.
AFAIK the reason why is twofold... the D layer has had more time to dissipate and there are fewer thunderstorms. Sounds simple and there is probably more to it than that. However, my observation has shown no correlation between the Dst thing and LW band conditions.
K index is probably a more reliable indicator. Just my unscientific .02.
 
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