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In August 2001 a new joint collaboration between italian physicists and norwegian engineers was succesfully carried into effect with a new mission to Norway, in order to further investigate a luminous phenomenon which is occurring recurrently in the valley of Hessdalen. The italian research-activity of this year was concentrated in the acquisition of optical data coming from conventional photography, video imaging and video-spectroscopy. Many photographs, videos and some spectra were obtained of the phenomenon. The results coming from the subsequent analysis show that: 1) the luminous phenomenon is a thermal plasma; 2) the light-balls are not single objects but are constituted of many small components which are casually vibrating around a common barycenter; 3) the light-balls are able to eject smaller light-balls; 4) the light-balls change shape all the time; 5) the luminosity increase of the light balls is due to the increase of the radiating area. This mission was able to finally visualize the real structure and nature of the light-phenomenon and its time-behaviour. The cause, and the physical mechanism with which radiation is emitted is currently unknown, and will be investigated in further missions. Some physical hypotheses are amply discussed. http://www.itacomm.net/ph/embla2001/embla2001_e.pdf
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... Photometric analysis of "balls of light" carried out at Hessdalen, the Norwegian site deemed a symbolic place to study these types of physical phenomenon, shows that this luminous phenomenon can produce high levels of energy, which remain confined during the event and are inexplicable in terms of known physics. For example, it has been calculated that this anomalous phenomenon in the atmosphere can reach a remarkable luminous power, up to 100kW (Teodorani, 2008), while, from the Planck curve maximum a temperature of around 6,500°K has been measured, which remained approximately constant for the entire duration of the luminous phenomenon, ranging from a few seconds to 3 minutes, despite drastic variations in luminosity (Teodorani et al., 2001). ...
... To date, thanks to documentation available on the website, we know that ball lightning has been observed in various parts of the globe, over land and sea, and near volcanoes (Bach, 1993). However, in some areas, it manifests more frequently, for example, in the Hessdalen Valley in Norway (Teodorani, 2004, Strand, 1985Teodorani and Strand, 2001), Marfa in Texas (Bunnell, 2009;Stephan et al., 2009;Bunnell et al.,2011;Stephan et al., 2011) and in Italy, especially in the Northern Apennines (Straser, 2007(Straser, , 2009). ...
... The relation between luminous phenomena, tectonic stress built up in rocks and earthquakes has been known and studied for a long time in many parts of the world (Finkelstein and Powell, 1970;Lockner and Johnston, 1983;Derr, 1986;Tsukada, 1997;St-Laurent et al.,2006), whereas in the Taro Valley seismic area, a time correlation between balls of light and earthquakes has been suggested by this author. Besides the Taro Valley, luminous phenomena have been recorded in other parts of the Earth (Bunnell, 2003;Strand, 1996Strand, -2003Straser, 2009;Teodorani and Strand, 2001) and have been accompanied with photographic evidence on many occasions. A link between tectonic stress and luminous phenomena was already conjectured and explained in the second half of the last century through the theory of piezoelectricity (Derr, 1986;Finkelstein et al., 1973), According to this hypothesis, certain silicate minerals, such as quartz, produce charged clouds and electric potentials through air ionization when they are subjected to mechanical deformation caused, for example, by crustal stress. ...
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... Moreover, the problems faced in studying the Hessdalen phenomena are similar to those associated with the study of electric, magnetic and electromagnetic signals observed with earthquakes. They are: the necessity to obtain a continuous recording extended in space, because electromagnetic phenomena are usually well localized and unpredictable [5,6,7,8]; the extraction of the signal from man made and natural noises [9,10,11,12,13,14]; and the search of the source that is closely connected to the hypotheses for a model to understand the observations [6,7,8,9]. ...
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