The mutual relations between solar activity, thunderstorms and Vertical Gradients of Electro Atmospheric Potential

The mutual relations are established between solar
 activity expressed in Wolf numbers, the vertical gradient of electro atmospheric
 potential measured in the Geophysical Observatory of Macerata,
 the geomagnetic field measured in the Observatory of the nearby town of&#1...

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Bibliographic Details
Main Authors: C. SCUTERINI, R. FUSARI, A. MURRI
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 1974-06-01
Series:Annals of Geophysics
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/4912
Description
Summary:The mutual relations are established between solar
 activity expressed in Wolf numbers, the vertical gradient of electro atmospheric
 potential measured in the Geophysical Observatory of Macerata,
 the geomagnetic field measured in the Observatory of the nearby town of
 Aquila, and the thunderstorm activity over the whole of the Italian territory.
 The mutual relationship between the vertical gradient, the geomagnetic
 field and the frequency of thunderstorms and solar activity are clearly
 evident. In particular the antiparallel behavior between solar activity
 and the vertical gradient, as well as thunderstorm frequency lias been made
 clear by observations carried out over a period of 22 years.
 The results obtained from a study of the geomagnetic field and the
 vertical gradients agree with the research on a much shorter period of time
 recently carried out by Rao.
 Observational values have been treated as statistical elements (2) to
 enable smoother readings, without however moving the maximums and
 mínimums of the phenomenon in the given period of time so that parallelisms
 and antiparallelisms resulting from theso observational values are
 kept.
 The average values of the vertical gradients of electro atmospheric
 potential were derived for electrically calm days.
 From these 5 days per month were chosen by probability method;
 the averages were then calculated on these five days chosen stochastically.
 We considered an electrically calm day one in which the sky was absolutely
 clear, with no thunderstorms either in the vicinity or far from the observatory,
 with neither fog or haze present.
ISSN:1593-5213
2037-416X