SporadicE

Amateur Radio Propagation Studies

SporadicE

Science, research, engineering, operating

SporadicE
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Section 1

Section 2

Section 3

Section 4

Section 5

Section 6

Summary

Thunderstorm effects

Aurora & FAI

Tropospheric ducting

Moonbounce

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Operating

Chronological

Multiple hop on VHF

Incoherent scatter

VHF transatlantic

Meteor scatter

Long-delayed echoes

Thoughts & discussions

This web site's highlights

Sporadic E

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Radio astronomy

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Multiple-tone effect

"Sporadic E" may be considered the most important ionospheric propagation mode in VHF dxing supporting long distance communication even with low power radio stations. The term "sporadic E" is however a geophysical term denoting localized enhancements of the electron density in the E region of the ionosphere with a duration between seconds and several ten minutes. Those electron density enhancements may be observed quite often in the E region of ionosphere which is however not true for sporadic E forward scatter of VHF radio waves. In fact, the electron density is only one of the many controlling parameters in sporadic E dx openings. The geophysical phenomenon has been exhaustively studied experimentally and theoretically by scientists, open questions however remain and some of them are addressed in this section based on observations made by radio amateurs. The BFLogotiny4-icon indicates articles referring to the BeamFinder analysis software.

Buttonsornaments

Thunderstorm effects on sporadic E propagation

An international team of radio amateurs has studied potential thunderstorm effects on the generation of sporadic E by analysing scientific results and QSO data compiled during the 2004 sporadic E season. In a detailed paper, Sabine (DL1DBC), Allard (PE1NWL), Udo (DK5YA), Gabriel (EA6VQ), Joachim (DL8HCZ) and Volker (DF5AI) discuss a possible model of thunderstorm-triggered sporadic E propagation on very high frequencies. In the 2004 data, a remarkable geographical correlation was found between 144 MHz sporadic E QSOs and sferic events, i.e. short term radio pulses emitted by lightning strikes.

a. Thunderstorm effects on sporadic E propagation in 144 MHz
b. Gewittereinflüsse auf die Sporadisch-E Ausbreitung im 144 MHz Band
Grassmann, V., DF5AI
Cremer, S., DL1DBC
Langenohl, U., DK5YA
Munters, A., PE1NWL
Sampol, G., EA6VQ
Kraft, J., DL8HCZ
Dubus 1, p. 9-44, 2005
SpecialTopics1d (English/German, b/w version, PDF, 1.2 MB)
 
Thunderstorm effects on sporadic E propagation in 144 MHz (version 2)
April 2005
SpecialTopics1d1 (English, PDF, coloured and extended version, 1.3 MB)
 
a. Thunderstorm effects on the F region of the ionosphere
b. Gewittereinflüsse auf die ionosphärische F-Region
Dubus 2, p. 58-61, 2005
SpecialTopics1d1b (English/German, PDF, 232 KB)
 
Thunderstorm effects on the ionosphere,
discussion of results and the readers' feedback
June 2005 (last update)
SpecialTopics1d1a (English, HTML, 45 KB)
 
Geographical distribution of sporadic E and sferics on June 27, 2004
Grassmann, V., DF5AI
Cremer, S., DL1DBC
May 2005
SpecialTopics1d1a2 (English, GIF animation, 304 KB)
 
Thunderstom effects on mid-latitude sporadic E?
First results of a data analysis project in amateur radio
Grassmann, V., DF5AI
Cremer, S., DL1DBC
CAL Mid-term Review and Science Meeting,
Elounda, Crete, Greece, June 20-24, 2005
(I am grateful to Prof. K. Schlegel for presenting this document because business issues have prevented Sabine's and my attendance at the conference, unfortunately)
SpecialTopics1d1a1 (English, PowerPoint, 1.3 MB)
 
a. More hints on thunderstorm effects on sporadic E
b. Neue Hinweise auf Gewittereinflüsse auf die sporadische E-Schicht
Dubus 3, p. 45-48, 2005
SpecialTopics1d1a1a (English/German, PDF, 212 KB)
Sferics27060412a

Sporadic E positions (blue) and sferics positions (circles) on June 27, 2004. The color code denotes the number of lightnings per 30 minutes.
June04Animation

Data animation of the June 27, 2004 event.
CALPaper

Presentation at the CAL conference, 2005.
Buttonsornaments1
May202003
144 MHz dx QSOs from May 20, 2003. The small picture denotes the path centers on the Iberian Peninsula interpreted by the radiowaves' footprints on the Earth surface in double hop sporadic E propagation, click map to view  that positions on a large screen map.
f0Es200503

Variation of the critical frequency foEs at El Arenosillo (south-western Spain, blue) and Roquetes (north-eastern Spain, red).

Very long distance propagation in the 144 MHz band

Part 1: Discussion of the May 20, 2003 dx opening

On May 20, 2003 radio amateurs from the Canary Islands reported many 144 MHz QSOs to central Europe and England corresponding to radio path lengths of 3.000 to more than 3.500 kilometers. At the same time, 144 MHz sporadic E QSOs as well as tropospheric dx propagation was reported. Does this dx event represent double hop sporadic E or did tropospheric dx propagation extend the radius of single hop sporadic E? Udo (DK5YA) and Volker (DF5AI) discuss a variety of possible propagation modes by analysing dx reports from radio amateurs, vertical profiles of meteorological data, ionograms and by using the BeamFinder software. Surprising results are found in this Sherlock Holmes type of investigation including new ideas in double hop sporadic E radio propagation on very high frequencies. Surprisingly, this paper has been discussed even by scientific experts, i.e. by commission G (Ionospheric physics and radio wave propagation) of U.R.S.I. (Union Radio-Scientifique Internationale) at the annual national conference in Miltenberg, Germany, October 2003.

Very long distance propagation in the 144 MHz band
Discussion of the May 20, 2003 dx opening
Grassmann, V., DF5AI
Langenohl, U. DK5YA
July 2003
SpecialTopics1 (BFLogotiny, English, PDF, 2.5 MB)
 
Very long distance propagation in the 144 MHz band
Discussion of the May 20, 2003 dx opening
Readers' comments, feedback, contributions
Grassmann, V., DF5AI
Langenohl, U., DK5YA
August-October, 2003
SpecialTopics1a (English, HTML, 36 KB)

 

Appendix

An attempt was made at identifying the possibility of atmospheric gravity waves in the May 20, 2003 dx event. I am grateful to the Instituto Nacional de Técnica Aeroespacial, El Arenosillo (Spain), the Observatorio del Ebro, Roquetes (Spain), and to the Institut Royal Météorologique, Bruxelles (Belgium) for providing detailed Digisonde material for analysis purposes. Having analysed various ionospheric parameters and its variation, there is indeed evidence for wavelike oscillations in, for example, the critical frequency foEs and the total electron content over Spain on this particular day. However, I am reluctant to interpret those wavelike variations by gravity waves. The assumption of atmospheric tides appears more likely but final results are not yet available.


 

Very long distance propagation in the 144 MHz band

Part 2: Dx opportunities in the European sector

The analysis of the May 20, 2003 dx opening between the Canary Islands and central Europe motivates the assumption of double hop sporadic E propagation supported by surface reflection of radiowaves by inland lakes and major rivers. This assumption results from the geographical position of the corresponding path centers which appear to correlate to the location of inland water areas. Assuming this assumption is justified, the results may be extrapolated to other regions in Europe, e.g. the Lake Balaton in Hungary, the Lake Constance between Germany, Switzerland and Austria or, just another example, to the river Dnieper in the Ukraine which also represents large water expanses. Doing so, surprising results are found, i.e. scenarios which appear to correspond to 'historical' examples of very long distance QSOs in 144 MHz.

Very long distance propagation in the 144 MHz band
Part 2: Dx opportunities in the European sector
October 2003
SpecialTopics1c (BFLogotiny1, English, PDF, 732 KB)
 
a. Dx opportunities in 144 MHz double hop sporadic E - Ground reflection of radiowaves by lakes and rivers
b. Dx-Möglichkeiten bei 144 MHz "Double Hop" Sporadisch-E-Verbindungen - Reflexion von Radiowellen durch Binnenseen und Flüsse
Dubus, 4, p. 66-69, 2003
SpecialTopics1c1a (BFLogotiny2, English/German, PDF, 664 KB)
Plattensee

To view your personal dx opportunities in double hop Es by using the lake Balaton in Hungary, identify your geographical position with respect to the circles and radials. In the next step, find your dx target on the same circle but in opposite direction. The blue line indicates an example of possible dx QSOs between Norway and Crete.

 

Very long distance propagation in the 144 MHz band

Results of the 2004 sporadic E season

[August 2004]. On July 11 this year, EA8BPX and EB8BTV both managed another series of long distance QSOs into Northern Italy, the sout-east of France and into Switzerland too. By refering to Fig. 6.24 in the initial paper (see page 30 in the above document by Grassmann and Langenohl), I realized that this QSOs indeed point in the same direction compared to the findings of last year. The figure displays the corresponding path centers of July 11. Note the circle labed "1" corresponds to seasurface reflection close to the Spanish sea coast, the circles labeled "2" denote path centers corresponding to the river Guadalquivir (see the four circles in the south), to a sidearm of the river Guadiana (see the two circles further north) and the river Guadiana itself (see the circle close to the center), respectively. Well, the two circles labeled "3" correspond to the highest position of the Sierra Morena. On August 06, IW2NOR worked EB8AYA and EA8BPX, the corresponding QSO midpoints are indicated by the green circles ("4") in the above image: another example of path centers located along the river Guadalquivir. Do you think all this is an accidental result?

Results of the 2005 sporadic E season

[September 2005]. Since 2003. we keep an eye on 144 MHz long distance QSOs between the Canary Islands and central Europe (path lengths around 3.500 km). Interpreting those QSOs by double hop sporadic E propagation, some sort of ground reflection must exist along the radiowaves' zigzag path between ground and the E region of the ionosphere. Calculating the geographical center of the QSOs, the reflection points are found on the Iberian peninsula. Referring to the 3/2005 issue of the Dubus magazine (see page 81), this type of QSOs are also reported by EB8BTV in 2005. The red circles display the geographical position of the QSO midpoints which appear to correlate to the position of large rivers, lakes and dams similar to the results we have already found in 2003 and 2004. In the analysis of the May 20, 2005 event, we have therefore speculated about seasurface reflection of the 2 meter radiowaves (we have used the term radioglint in inland water expanses). However, assuming radiowaves reflected at ground level, double hop sporadic E QSOs should be accompanied by single hop sporadic E QSOs originating in the central area of the double hop path (i.e. VHF radio stations located within the red circles from above can work into central Europe and also towards the Canary Islands at the same time). In practice, however, we generally find no such geographical correlation between double and single hop sporadic E QSOs which could have something to do with the geographical distribution of the VHF dx stations, of course. However, we have also presented an alternative interpretation, i.e. radiowaves not reflected at ground level but a few hundred meters above ground at the topside of local inversion layers associated with large rivers, lakes and dams. Anyhow, the results from the 2005 sporadic E season appear fully compatible to the previous results. What is the next step in the analyses of very long distance propagation in 144 MHz? I think there is a need to study the meteorological situations in more detail, e.g. (small-scale) inversion layers on the Iberian peninsula above inland water expanses in the months of May and June - with other words: can we identify any systematical features which could be used for prediction purposes (by using, for example, the vertical soundings distributed by the University of Wyoming)? Are there any meteorologists in the ham community willing to volunteer?

EA8JulAug2004

Midpoints of dx QSOs between the Canary Islands and central Europe in 2004.
Map290505EA8
Map290505EA8

Click image

Map290505EA8
Map290505EA8

Midpoints of dx QSOs between the Canary Islands and central Europe in 2005. Click image to obtain a satellite view .

 

Very long distance propagation in the 144 MHz band

Part 3: Use of satellite and aerial images to analyse double hop sporadic E radio links

In 2006, the number of 144 MHz double hop sporadic E QSOs has increased considerably resulting in 128 dx QSO exceeding the distance of 3.000 kilometers (two QSO even represent distances beyond 4.000 kilometers). The corresponding path centers have been analysed with high geographical resolution by referring to the Google Earth internet service. 25 percent of all QSOs represent seasurface reflection of radiowaves in the ocean, all the remaining QSOs show path centers in close vicinity of major rivers (width of a few hundreds meters) and big lakes (size of 1x1 kilometers at least). The below paper therefore closes the case that was opened with the analysis of 144 MHz very long distance QSOs in 2003 (see above): the hypothsis of rivers and lakes enabling double hop sporadic E QSOs is strongly supported by the analysis, it is actually safe to say the hypothesis is verfied to a high degree of certainty.

Use of satellite and aerial images to analyse double hop sporadic E radio links
Dubus 4, p. 67-88, 2006
SpecialTopics1c1 (English, PDF, 1.6 MB)
 
Please note: Figure 4 in the above paper analyses the dx QSO between EA8AVI and DH4FAJ on July 16, 2006. Mathias (DH4FAJ) send me an email because the paper refers to an incorrect QTH locator, i.e. JN48EX in the paper should read JN49EX. Figure 4 in the above paper is therefore replaced by a corrected version which is available by clicking the map display on the right. Instead of identifying the river Guadiana as the radiowaves' footprint on Earth (see figure 4 in the paper), we may now identify a big lake north of the geometrical path center (see the square, note the scaling at the bottom of the map display). The statistical analysis presented in the paper is not affected by this correction.
VLDPLake

Example of the footprint analysis in 144 MHz double hop sporadic E QSOs. The area displays the center of the propagation path between the Canary Islands and Germany (white line) 200 kilometers southwest of Madrid, Spain.

 

Analysing the number of skips in multiple hop propagation

From November 2001 to January 2002, many radio amateurs enjoyed a series of openings between Europe and North America in the 50 MHz band. On November 17, 2001, 1520-1630 UTC, dx stations lined up in multiples of approximately 2000 kilometers within a very small window of azimuth. This situation appears to represent a brilliant example of multiple hop propagation in 50 MHz but the number of skips along the zigzag path between the ionosphere and ground isn't easy to analyse.

50 MHz opening between Europe and North America
Multiple-hop propagation in the 6m band
February 2002, July 2002 (revision)
SpecialTopics1b (BFLogotiny3, English, HTML, 128 KB)
NAEU171101
50 MHz opening, November 17, 2001
Buttonsornaments2

Unusual dx distributions

Plotting the number of QSOs versus dx distance is a simple method of studying the characteristics of dx openings. Analysing sporadic E and Aurora QSO data, I often found unusual dx maxima around 1.500 km. For example: the upper panel on the right displays approx. 1.000 sporadic E stations spotted in the 50 MHz band from three independent locations in recent years. Unusual dx maxima are also found in Aurora dx communication, see, for example, the analysis of the geomagnetic storm from March 31, 2001 (see the lower diagram and the arrows therein). Joe, NA3T, found something similiar when analysing the Aurora QSO data from July 15, 2000. British radio amateurs analysing dx distances in Auroral backscatter also found a dx maximum between 1.400 and 1.500 km (info by Juho, OH8HFY). What's the meaning of this maxima? We don't know yet. In my very first internet publication (1999), I have speculated about an unknown mode of sporadic E which very soon became a matter of dispute, of course. The reader is therefore advised to visit "Six News Magazine" section on the UKSMG webpage which provides a critique on the below article.

Hidden Mode of Sporadic-E?
More magic with the magic band
Webpage of the UK Six Meter Group, 1999
SpecialTopics1b1 (English, HTML, 520 KB)
 
Hidden Mode of Sporadic-E?
More magic with the magic band
Part 2: Sea-/Land distribution in Europe
February, 2000
SpecialTopics1b1a (English, HTML, 708 KB)
DXDistribution

DX distribution in the 50 MHz band
GCD31032001

DX distribution, March 31, 2001 (Aurora)

 

Model calculations in 144 MHz sporadic E

VHF sporadic E propagation is associated with plasma instabilities which may cause strong scatter of radiowaves. This geophysical phenomena are not considered by the theory of electromagnetic wave propagation in an ionized media (i.e. in the basic versions we generally find in textbooks). However, we actually refer to this theory when analysing VHF sporadic E by extrapolating 'shortwave models' to very high frequencies. Very dense sporadic E layers may exceed critical frequencies of 16 MHz but this models result in critical frequencies around 25 MHz (in 144 MHz sporadic E) or even 35 to 39 MHz (in 222 MHz sporadic E) which evidently no longer reflects the true ionosphere. From this perspective, almost all MUF calculation programs used by VHF radio amateurs must be considered incorrect. However, we currently have no alternative model available which appears applicable in VHF dxing. Thus, it is very important to keep in mind that our current approach is nothing else than an imperfect approximation. In 1988, I have contributed to this approach and even the current version of the BeamFinder software provides its 'sporadic E analyser' module by refering to this paper. I am close to ban this module from future BeamFinder releases because this method is no longer acceptable in my view.

Ein einfaches Modell zur Identifizierung von Sporadisch-E
Dubus, 2, p. 128-132, 1988
SpecialTopics1b1b (German, PDF, 360 KB)
MUFCalc

MUF calculations
Strahlengang

Ionospheric ray paths

 

Unless otherwise stated, all material is copyright of Volker Grassmann. All rights reserved. The material, or parts thereof, may not be reproduced in any form without prior written permission of the author.

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