Conference PaperPDF Available

Sound producing mechanism in the temperature inversion layer and its sensitivity to geomagnetic activity

Authors:
  • Aalto University, School of EE, Espoo Finland

Abstract

Sounds associated with aurora borealis, so called Auroral Sounds (AS), are explained by electrical discharges occurring in the Temperature Inversion Layer (TIL) approximately 75 meters above the ground [1]. It is assumed that under favourable weather conditions the number of AS events depends on the activity of the geomagnetic (GM) storm. Historical testimonies of AS indicate that the GM storm should be strong enough to rise bright and lively auroras to the zenith before these sounds can be observed. The goal of this study is to test the relevancy of this claim by studying the sensitivity of the AS producing mechanism under moderate GM activity. A four-hour sound measurement was performed around the local magnetic midnight on Jan 25–26, 2022 at Fiskars village in southern Finland. Sixty AS event candidates were manually selected and their temporal distributions and period histograms constructed for statistical comparisons with the GM data measured simultaneously by the Finnish Meteorological Institute (FMI) at Nurmijärvi Geophysical Observatory (NGO). The data was also used for regression models to study possible causal relationship between the GM activity and the AS events. A strong causality was found. The temporal distribution of the sounds was predicted by the GM activity with 90% accuracy after a delay of 21 min. The results show that in good weather conditions the AS events are much more common than previously thought.
1
Sound producing mechanism in temperature inversion layer and
its sensitivity to geomagnetic activity
Unto K. Laine1,*
1Department of Signal Processing and Acoustics, Aalto University, Espoo, Finland.
* unto.k.laine@aalto.fi
Abstract
Sounds associated with aurora borealis, so called Auroral Sounds (AS), are explained by electrical
discharges occurring in Temperature Inversion Layer (TIL) approximately 75 meters above the ground [1]. It
is assumed that under favorable weather conditions the number of AS events depends on the activity of the
geomagnetic (GM) storm. The historical testimonies of AS indicate that the GM storm should be strong
enough to rise the bright and lively auroras to the zenith before these sounds can be observed. The goal of
this study is to test the relevancy of this claim by studying the sensitivity of the AS producing mechanism
under a moderate GM activity. A four-hour long period of the sound measurements done around the local
magnetic midnight Jan 2526, 2022 at Fiskars village, Finland, is analyzed. Sixty AS event candidates were
manually selected and their temporal distribution and period histogram constructed for statistical
comparisons with the GM data measured simultaneously by the Finnish Meteorological Institute (FMI) at
Nurmijärvi Geophysical Observatory (NGO). The data was also used for regression models to study possible
causal relationship between the GM activity and the AS events. A strong causality between the GM activity
and the AS events was found. The sounds were predicted by the GM activity with 90% accuracy after a
delay of 21 min. The results show that the AS events are much more common than previously thought.
Keywords: aurora borealis, solar wind, magnetosphere, auroral sounds, geomagnetism, temperature
inversion layer, regression models, period histogram.
1 Introduction
Based on the present knowledge, Auroral Sounds (AS) have physically existed around auroral zones as long
as the Earth has had an atmosphere and magnetosphere similar to the present ones. Thus, the problem of AS
is not just a millennial problem, as often referred to, but has probably surprised many species before the
humans. The question of the first descriptions of aurora borealis and also of the sounds associated, have been
discussed a long time. Based on earlier studies [2,3], it is probable that one of the first documented
observations was made by prophet Ezekiel around 593 BCE. For some reason the earlier studies of this event
are limited entirely to the visual part of Ezekiel’s observations falling silent in front of his sound perceptions.
Ezekiel not only described the visual art of auroras, which he called angels, but continued with the sounds.
He tells, that he heard “the roar of rushing waters”.
When the Auroral Acoustics project [1] started and the author made one of his first AS observations, a TV-
reporter asked for a description of the sounds. The answer was: “they sounded like Niagara Falls from a
distance of one kilometre”. Afterwards, when the author became familiar with the text of Ezekiel, the
similarity of the descriptions surprised. The recent AS observations include descriptions, where a strange
sound from the sky woke up the attention and after looking to the direction of the sound source an aurora
was observed. The sound focused the mind to search its reason from the direction it was perceived, on the
open sky. In Same culture we find opinions that an aurora without a sound is not a real aurora. A ‘real
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aurora’ should be bright, colourful, lively with changing structures. Exactly these features are often
mentioned as conditions for auroral audibility.
Until around 1930’s some authors still believed that under special conditions auroras may come down below
the altitude of the clouds and therefore they could be audible [4]. Even after the hundreds of altitude
measurements made by Norwegian Carl Størmer [5], who first time showed that only in extremely rare cases
the lowest edge of the auroral curtain may be a little below 80 kilometres, some authors kept asking, could
they still sometimes come much closer to the ground and be therefore audible. Because the acoustics is not in
the focus of geophysics, the location of the sound source was never studied or revealed.
At the end of the 18th century, the question of whether electricity could explain the auroras garnered
increasing attention. The earliest texts proposing that the AS events are caused by electric discharges are
probably from the years 1831 and 1834 [6,7]. Sometimes AS were even used as a proof for the electric
nature of the aurora. In the 1920’s C. A. Chant, editor of The Journal (JRASC) interested about this problem
and asked the readers to send their sound observations to the editorial [8,9]. Professor William C. Baker,
from Queen’s University, Kingston, sent a letter to Chant where he described an AS event which occurred in
mid-winter in 1884 or 1885. Baker’s story was exact and rich in ideas. He described the sounds as “the
crumpling of stiff paper”. He assumed that the sounds are produced by the same electro-magnetic (EM)
source that also controls the visible aurora and describes the sound; “It reminds of the noise heard when
discharging the glass jar”, referring to a capacitor known as Layden jar. Baker summarizes that because the
delay between the auroral movements and the sounds was small (12 s), the sound source must be closer to
the observer than the light source. It is obvious that Chant learned much of these accurate observations and
embraced Baker’s brilliant ideas. However, the problem of where such capacitor is and how it is charged,
remained unresolved almost one hundred years during which, with a few exceptions [10], more speculation
was produced than genuine research to solve this problem.
However, the electric fields caused by the GM activity are never large enough to produce directly discharges
and sounds in the lower atmosphere. Tree tops are quiet. The present Inversion Layer Hypothesis (ILH)
provides a physical explanation for the sound production [1]. It assumes that after a calm and sunny day the
warm air at the ground rises carrying negative ions up forming a Temperature Inversion Layer (TIL) about
70-100 metres from the ground. Above this layer positive ions are ‘raining’ down from the upper atmosphere
accumulating in the layer above the warm air. Because vertical movement of the air is minimal at the
inversion, these two layers continue to accumulate charges forming finally a structure like a large plate
capacitor. The activation of a GM storm generates the needed additional potential between the layers and
triggers the discharges. It should be noted that the energy for the sounds is loaded to the capacitor during the
evening and night, meanwhile the GM activity works just as an activator for the discharges.
The main goal of this paper is to study the sensitivity of the sound production mechanism of the inversion
layer under moderate GM activity. The statistical connections between the magnetic field measurements
made by the FMI and the recorded AS events are studied. Four different methods to reveal these connections
are introduced. They all provide similar results showing a causal relationship between the magnetic field
fluctuations and the sounds. Surprisingly many periodic events known in the field of geomagnetism have left
their fingerprints to the sound sequence. The new findings support the presented ILH.
Next chapter starts with a description of the measuring system, the weather, and the GM conditions during
the night of measurements. Then the selection of sixty AS events is described with examples of their
temporal and spectral properties. Chapter 3 describes the four approaches to show the causal and statistical
connections between the magnetic field measurements made by FMI and the recorded AS events. The paper
ends with a conclusion that summarises not only the new results, but the whole Auroral Acoustics project.
3
2 Sounds and magnetic field measurements Jan 2526, 2022
The same measuring system as described in [1] was used in this recording, too. Its ‘soul’ is the highquality
measuring microphone of Brüel & Kjær (4179 with preamp 2660) that was mounted at the focus of a
parabolic dish antenna directed vertically to the sky. The internal noise of this microphone is around -3 dBA
and it is carefully shielded against all EM-interferences. Additionally, two other microphones and a VLF
loop antenna were connected to a fourchannel digital recorder thus allowing the sound source localization.
2.1 The weather and geomagnetic conditions
A moderate GM activation occurred on Jan 2526, 2022. The Kyoto Dst index [11], shown in Figure 1,
stayed at -35 during the hours 1920 LT. The intensity of the GM activation degreased during the period of
data collection. The local magnetic field activity, measured at NGO (60° 30.5’ N, 2 39.3’ E), was
moderate, too. The FMI has estimated that the GM activity meter should rise over 0.3 nT/s before the
probability of auroras in the southern Finland is high. The highest measured activity was only 0.14 (see
Figure 5 chart in blue) indicating that during the night in question aurora was probably not visible in the
southmost Finland.
Figure 1. Kyoto Dst in the night Jan 2526 2022. The arrow shows the time window of
The data collection for this work (21:2001:20 LT).
The quasi-K-index calculated for the three last hours before the local midnight gives K=4 and for the next
three hours after the midnight K=3 (in decimals: 4.6 and 3.7). The probabilities of these occurrences at
Nurmijärvi are correspondingly: 8.1% and 19.3% [12]. However, still the developed automatic analysis of
the recorded audio material was able to find around two hundred AS candidates and a careful manual selec-
tion (carried out before the automatic analysis) sixty cases in the 4 h time window. This means that the sound
production in the TIL is much more common than ever imagined. Under favourable weather conditions, TIL
is sensitive to even relatively small geomagnetic disturbances as will be seen. The probability for similar
geomagnetic activities is over 25% in south Finland, however, the buildup of a strong TIL is not equally
common and both of them are needed for the sound production.
Figure 2. Wind and temperature conditions at Jokioinen Jan 2526, 2022. Blue boxes indicate the time
window of the measurements used in this study. Data from the FMI.
17 18 19 20 21 22 23 0 1
Measurements
-35
-30
-25
-20
-15
-10
-5
0
Kyoto Dst Jan 25–26, 2022
Dst
4
The closest fully armed FMI weather station to the Fiskars village locates at Jokioinen, about 90 km to the
North. According to the data of that station, the air pressure degreased from 1020 to 1017.6 hPa during the
measurements, and the sky was clear. The clear night produced about 9 °C temperature drop at the ground
from the highest midday reedings indicating that an inversion layer was formed. The wind speed was around
2 m/s at the beginning of the data collection and increased later close to 3 m/s (see Figure 2).
2.2 Sixty AS event
Sixty AS event were manually collected from the 4 h long recording of the B&K microphone signal based on
their auditive, temporal and spectral properties. Twenty examples of them are shown in the Figure 3. The AS
events have large temporal variability. Some of them are like impulses, very compact in time, meanwhile
some others are like clap or pop sounds with noisy echoes. In the left frame a sequency of cracks is shown
(the fourth signal from the top). Due to the amplitude (peak) normalization, it looks like the background
noise is varying. In reality it varied quite little. The night was calm and quiet.
Figure 3. Twenty randomly selected AS events from the set of sixty cases.
Figure 4. Mean of ten randomly selected AS event spectrum.
 |   | 
 |   | 
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Figure 4 shows the mean of spectra of ten AS events that occurred in a row. The signal of the B&K
measuring microphone is high-pass filtered before the recording. The filter with -6 dB/oct rolloff and 500
Hz cutoff is used to hinder strong infra sounds to clip the signal by driving it out of its dynamic range.
The spectral peaks below the 300 Hz occur often at the Schumann resonances. They are sometimes clearly
intensified around the AS events. These components from a constant background hum on which the AS
events are superimposed. A strong 50 Hz component is seen. It cannot be caused by any direct electric or
magnetic field leakage from the mains to the microphone which is carefully shielded and has a low output
impedance. The present supposition is that also this acoustic hum is created at the inversion layer. The
observation that this peak often varies between 4752 Hz supports this idea. The electric network in Finland
is based on 50 Hz AC and this frequency can’t vary so much out of its standard. However, these details in the
low-frequency range need still more work. The main spectral peak of the AS events is located around 700
2500 Hz. Sometimes spectral peaks may appear even around 79 kHz.
In the following the time instances of the AS events are studied in comparison to the GM activity and in
more detail to the magnetic field measurements made by FMI at NGO.
3 Causality between GM activity and AS events
During the first phase of the Auroral Acoustics project one attempt was made to build a bridge between AS
events and geomagnetic measurements made by the FMI. This was published in the Master’s Thesis of Janne
Hautsalo [13]. Without extracting the individual AS events from the audio signals the whole material was
analysed by a 1/3octave filter bank and the RMS values of the outputs correlated with those of the GM field
at different delays. Statistically significant correlations were found at many frequency bands and at many
delays. Since that analysis it was clear that the variations in the geomagnetic fields are the cause for the
sounds, even though that time the localizations of the sound sources were not solved, neither the physical
mechanism of the sound production. The experience of the past years provides methods to extract the AS
events from the noisy background both manually and algorithmically. An automatic method is under
development, but it is not yet working sufficiently well to serve the research like this.
After the extraction of the individual AS events their temporal histogram in 10 min windows is constructed
(the right histogram in red in Figure 5). The data starts at 21:20 and continues to 01:10 local time. The data
for the histogram in blue is taken from the webpage of the FMI [14]. Both histograms have a clear peak of
maximal activity. The GM activity seems to precede and predict the AS events.
Figure 5. Comparison of the number of AS events and the GM activity at NGO in 10 min windows.
The unit of the GM data is 10 pT/s. The time scale in the middle is the local time.
GM Activity Nr of AS Events
0510 0 5 10
21:30
22:00
22:30
24:00
23:30
00:00
00:30
01:00
GM Activity and AS Events in 10 min Windows
6
The direct correlation between the GM activity and the number of AS events gives r = 0.44 with a large
p = 0.38. When the GM activity is delayed by 10 and 20 minutes, these numbers are: r = 0.69, p = 0.4 and
r = 0.47, p = 0.09. This indicates that a statistically significant fit should occur at a delay around 20 minutes.
A closer picture of the connections between the magnetic field fluctuations and the AS events can be created
by applying the regression analysis.
3.1 Regression Model
A standard method to reveal possible causality between a set of independent variables and a dependent
variable, or a response of a system to variations in the independent variables, is the regression analysis.
Now, the GM data provided by the FMI containing three magnetic field components (Bx, By, Bz) and
sampled with ten second periods is used for a regression model to predict the number of the AS events
counted in overlapping 12–34 minute windows moved in oneminute steps. The mean of the magnetic field
components are removed and the sequences partitioned to tenminute segments consisting of 60 samples
each. The RMS values of each segment of each component is computed. The obtained RMS sequences form
the independent variables for the regression model.
First, eleven time-sifted variants of the AS event sequence are produced moving the window’s centre starting
from 1 to 12 min after the first AS event in steps of one minute. Additionally, there was a constant delay of
10 min between the magnetic field data and the first AS event. Now, each timesifted variant represents the
AS event sequence with a delay varying from 11 to 22 minutes providing the solving of the optimal lag for
the regression model. The optimal regression model was found with a lag of 21 minutes. It predicts the AS
events with 90% accuracy (R2 = 0.895). The correlation between the best regression model and the optimal
AS event shiftvariant is r = 0.95 with p < 0.0001 when the 32 min window size is used.
The regression coefficients for the {Bx, By, Bz} sequences are {0.91, 0.22, -0.12}. When the mean RMS
values of these sequences are multiplied with their coefficients, we get: {6.58, 3.15, -2.49}. This indicates
that the Bx has more active role in the sound production than the By and the effect of Bz is negative. This
leads to a conclusion that the variation in the horizontal magnetic field component H={Bx, By} has an
important role in the sound generation in the temperature inversion layer. This outcome provides a deeper
insight to the Inversion Layer Hypothesis: Variations in the Hcomponent induces vertical potentials
(electromotive forges) which may increase the ionization in and between the charged layers thus increasing
the probability of a discharge between the layers in the form of an avalanche of electrons [15].
Figure 7. Smoothed temporal distribution of the sixty AS events (in blue, delayed 21 min) predicted by a
magneticfieldbased regression model (in red). R2 values as a function of the window size (on the right).
7
3.2 Period histogram of the AS event sequence
A novel, not earlier discussed aspect related to AS is their period histogram. Knowing the time instances of
the sixty AS events, a histogram of all time periods between the events is easily constructed by subtracting
every time instant from all the later ones. The number of periods in a gliding fourminute window is
calculated at oneminute intervals to construct the histogram shown in Figure 8 in blue. Also, period
histograms of one hundred randomized cases with the same number of events were constructed. Their mean
and deviations from the mean by one standard deviation are correspondingly illustrated in gray, red, and
green. The AS events are clearly not located randomly in the fourhour window, but certain periods are
occurring more often than the others. Especially periods of 10, 17, 26, 37, and 53 minutes arise strongly
above the random statistics. These peaks deviate from the random mean 15.2, 9.4, 10.8, and 12.0 times the
random STD. Their largest pvalue is smaller than 0.007 indicating the statistical significancy of these
peaks. The histogram shows also how the number of the shortest periods is high. These cases include clap
pairs, known as “klipklap”events. These cases together with the crackling sounds have been analysed
earlier and their statistical connections to Schumann resonances shown [16].
Figure 8. Period histogram of the AS events shows peaks at durations of 10, 17, 26, 37, and 53 minutes.
Statistics of one hundred random cases are presented as a reference (see text).
The found peaks at durations of 10, 17, 26, 37, and 53 min happen to be almost identical to those found in a
study of the magnetosphere and the solar wind by Huang &al. [17]. They summarize: ‘It is known that the
solar wind has significant effect on the magnetospheric convection and that magnetospheric electric fields
can penetrate into the midlatitude and low-latitude ionosphere. We suggest that the midlatitude ionospheric
electron density perturbations were caused by the penetration of magnetospheric electric fields which were
controlled or modulated by the oscillations in the IMF (Interplanetary Magnetic Field) or solar wind
pressure.In that study the loss time of the oxygen ions due to recombination at the F region altitudes were
estimated to be 12, 18, 26, 37, and 52 min at the altitudes of 220, 230, 240, 250, and 260 km. Now a question
arises as to whether these processes, occurring at 220260 km above the ground, could cause the same
pattern in geomagnetic field on the ground and further in AS event period histogram or, is this just a
coincidence? This cannot be answered in this short study. However, next the period histograms of the
magnetic field measurements at NGO are analyzed and compared to the AS event period histogram.
3.3 Period histograms of the magnetic field sequences Bx, By, and Bz
Period histograms were constructed for the same magnetic field data that was used for the regression model
in section 3.1 by using practically the same algorithm as in the construction of the period histogram for the
AS events. In this case the amplitude peaks of the magnetic field components must first be solved. The cross-
correlation between the obtained period histograms of the components (Bx, By, Bz) and the period histogram


5 10 15 20 25 30 35 40 45 50 55 60
0
20
40
60
80
100
120
5 10 15 20 25 30 35 40 45 50 55 60
Period Length in Minutes
Number of Cases
Histogram of AS event periods
Nr of AS Event periods Random Mean+STD
Random Mean-STD Random Mean
8
of the AS events are: r={0.58, 0.60, 0.58} with the largest p< 0.0001. The period histogram of By and that of
AS events are shown in Figure 9. The period histogram of the By component has the three first peaks
approximately at the same period length as the AS event histogram, whereas the fourth peak of the AS event
histogram doesn’t have any clear counterpart in the By histogram. The same is true with the Bx and Bz
period histograms.
Figure 9. Period histograms of AS events and simultaneous magnetic field By-component at NGO.
Figure 10. Period histogram of AS events and AR model (see text).
The statistical connections between the period histograms can be illuminated further by constructing a
regression model from the magnetic field component histograms to model the AS event histogram. The
obtained regression model is depicted in red in Figure 10.
The cross-correlation between the AR model and the period histogram of the AS events is r=0.64 with
p<<0.0001. Thus, the magnetic field components explain 41% of the AS events period histogram. However,
when the cross-correlation is calculated in a smaller window having period lengths between 530 min, the
correlation improves to r=0.72 (p<<0.0001) and R2=0.52. The three first peaks of the AS events period
histogram are explained by the regression model that is based on the period histograms of the magnetic field
components by 52%.
3.4 H-component of the magnetic field
The role of the horizontal (H) component activity in the AS event production was discussed above. The
magnetic field components Bx and By were interpolated for solving the ∆H vectors at 130050 seconds


5 10 15 20 25 30 35 40 45 50 55 60
0
20
40
60
80
100
120
5 10 15 20 25 30 35 40 45 50 55 60
Period Length in Minutes
Number of Cases
Period Histograms of AS events and By
Nr of Event periods Nr of By periods


5 10 15 20 25 30 35 40 45 50 55 60
0
20
40
60
80
100
120
5 10 15 20 25 30 35 40 45 50 55 60
Period Length in Minutes
Number of Cases
Period Histogram of AS events and its AR model
Nr of Event periods AR model
9
before the sound events in steps of 50 s. The obtained results are clustered to five classes by using Gaussian
mixture method (see Figure 11). The ∆H values of the first and largest cluster with 22 cases are amplified by
ten for a better visualization. This cluster has a sharp variation in the Bx-component before the sound events.
The analysis shows that about 2/3 of the cases (#48) have a slow and large variation of 2040 nT and 1/3
(cluster 1) a smaller but fast variation before the AS event.
Figure 11. Five cluster means of the ∆H = {∆Bx, ∆By} before the AS events (at origin).
4 Conclusions
The Auroral Acoustics project started over twenty years ago [18]. That time there was not much hope that
this millennial problemcould ever be solved. Many geophysicists around the globe had fixed their
opinions: Auroral sounds are illusionsand They are physically impossible”. However, a new, previously
unknown sound producing mechanism in the temperature inversion layer was discovered [1]. The present
study connects the sound production to the independent magnetic field measurements. The results show that
the sound producing mechanism is far more sensitive to the magnetic field variations and the auroral sounds
are much more common than has ever been understood. The key issue is the formation of a strong
temperature inversion layer. This occurs only during an excellentfox weather” conditions meaning; calm,
serene sky, temperature drop around 8°C, and at least a moderate geomagnetic activity.
AS events have a complex relationship to the different types of geomagnetic activities. It was discovered
earlier that the patterns of the crackling sounds are connected to the Schumann resonances [16]. The present
work shows new connections through period histograms between the magnetism and the sounds. The
discovered important periods are on the band 1040 min belonging to the Ps 6 type magnetic variations that
are especially connected to By–component during the recovery phase of magnetic substorms [19]. The
discovered 21 min delay between the magnetic fluctuations and the sounds has not yet explanation.
Auroral sounds are produced with a separate process from the auroral light production. However, both have
the same geomagnetic background causing synchronism between these phenomena. The creation of auroral
sounds may occur and be audible even without any visual aurora, which is one of the revolutionising
conclusions of this long project. Still, due to the historical and perceptual (cognitive) reasons, we may still
use the term auroral sounds, even though the sounds are not ‘auroral’, but electric discharge sounds created
at 70100 m above the ground.
Acknowledgements
The author is grateful to the FMI for providing the geomagnetic data of NGO and Okko Räsänen as well as
an anonymous reviewer for the constructive comments on the manuscript.


-10 10 20 30
nT
-40
-20
20
40
60
nT
H values 1300–50 seconds before the AS events
1(#22)2(#9)3(#2)4(#16)5(#11)
10
References
[1] Unto K. Laine, Auroral Acoustics project a progress report with a new hypothesis, Baltic-Nordic
Acoustic Meeting, BNAM 2016, Stockholm, Sweden, June 2016.
[2] George L. Siscoe, S. M. Silverman, and K. D. Siebert, Ezekiel and the Northern Lights: Biblical
Aurora Seems Plausible, Eos, Transaction, American Geophysical Union, Vol. 83, No. 16, 16 April
2002, pp 173179.
[3] Oleg M. Raspopov, Ezekiel’s Vision: Visual Evidence of SternoEtrussia Geomagnetic Excursion?
Eos, Transaction, American Geophysical Union, Vol. 84, No. 9, 4 March 2003, pp. 7788.
[4] Sydney Chapman, The Audibility and Lowermost Altitude of the Aurora Borealis, Nature Vol. 127 No.
3201, March 7 1931, pp. 341-342.
[5] Carl Størmer, Altitudes of Aurorae, Nature, Vol. 97, No. 2418, March 2 1916, p. 5.
[6] W. Dunbar, Notice of the Aurora Borealis of Last Winter. Edinburgh Journal of Natural and
Geographical Sciences (New Series), Vol III, ART. V., April 1831, pp. 225-226.
[7] Anonymous, Aurora Borealis, The Knickerbocker 1834 New-York Monthly Magazine Vol. IV.
August, 1834, pp. 98-107.
[8] William C. Baker, a letter to the editor of Journal of the Royal Astronomical Society of Canada,
JRASC, Vol XVII, No. 7, September 1923, p. 279.
[9] Fiona Amery, The disputed sound of the aurora borealis: Sensing liminal noise during the first and
second international polar years, 18823 and 19323.
https://royalsocietypublishing.org/doi/10.1098/rsnr.2021.0031
[10] S. M. Silverman, T. F. Tuan, Auroral audibility, Adv. Geophysics, Vol 16, pp. 155266, 1973.
[11] http://wdc.kugi.kyoto-u.ac.jp/dst_realtime/index.html
[12] https://space.fmi.fi/image/realtime/K/quasi_K_NUR.html
[13] Janne Hautsalo, Master’s Thesis, Study of Aurora Related Sound and Electric Field Effects, Helsinki
University of Technology, 2005. http://lib.tkk.fi/Dipl/2005/urn007898.pdf
[14] https://www.ilmatieteenlaitos.fi/revontulet-ja-avaruussaa
[15] Rudolf A. Treumann, Zbigniew Klos, Michel Parrot, Physics of electric discharges in atmospheric
gases: an informal introduction, arXiv:0711.1672v2, 10 Apr 2008.
[16] Unto K. Laine, Auroral crackling sounds and Schumann resonances, 26th International Congress on
Sound and Vibration, Montreal, Canada, 7-11 July 2019.
[17] Chao-Song Huang, J.C. Foster, P.J. Erickson, Effects of solar wind variations on the midlatitude
ionosphere, Journal of the Geophysical Research Space Physics, 16 August 2002.
https://doi.org/10.1029/2001JA009025.
[18] Unto K. Laine, Twenty Years Hunting for Auroral Sounds, Project document, 2021.
https://www.researchgate.net/project/Auroral-Acoustics
[19] Robert L. McPherron, Magnetic pulsations: Their sources and relation to solar wind and geo-
magnetic activity, Surveys in Geophysics (2005) 26:545592, 2005.
ResearchGate has not been able to resolve any citations for this publication.
Conference Paper
Full-text available
Observations of unusual sounds like claps, snaps, and cracklings from a serene sky under actively moving, bright aurora borealis have been reported during a long history. Since year 2000 the auroral sounds have been studied in Finland. In 2011 a sound source associated with the aurora was localized for the first time in the sky approximately 70 meters from the ground. To accommodate for the surprisingly low altitude of the source, a hypothesis that the sounds are produced by corona discharges in a temperature inversion layer at the observed altitude was pub-lished in 2016. The focus of the present paper is in the acoustic analysis of the crackling sounds that are sequences with complex temporal structures. It is shown that the sounds share similar rhythmical patterns, which are connected to the electromagnetic resonances in the atmosphere, also known as the Schumann resonances.
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Eerie sounds associated with bright and lively moving aurora borealis have surprised and even frightened observers for thousands of years. Since the 17th century their existence and cause have been at the centre of many speculations and hypotheses. These have ranged from a totally skeptical view of their existence to some possible physical or physiological explanation. No widely accepted physical model or reason for these sounds exists. There was at least one attempt to measure these sounds, performed at the Geophysical Institute in Alaska, during 1962-64. However, this did not yield a single recorded example or scientific publication. In February 2000 two researchers from the Sodankylä Geophysical Observatory (SGO) and the author agreed to start an informal co-operation on this research topic. The project was called Auroral Acoustics. It began by publishing some webpages to provide general information on the topic and to collect testimonies of auroral sound observations in Finland. These were also collected by SGO via telephone interviews. To date this dataset contains more than 300 observations. The design of the scientific setup for sound and EM-field measurements started in spring 2000. So far the Auroral Acoustics project has had two active phases; the first phase of the project occurred during solar cycle #23 (2000-05) and the second phase during cycle #24 (2011-ongoing). The project was basically inactive during the five years around the solar minimum between the activity peaks. This paper describes the two phases of the project and presents the main results of the sound and EM-field measurements recorded during more than one hundred auroral nights. The estimation of the locations of the sound sources has led to a new hypothesis for a possible physical mechanism to explain these sounds. The new hypothesis is based on the temperature inversion layer found in the lower atmosphere.
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