Rebaviour of tbe electric conductivity of tbe precipitations

Continuing the researl'hes on the preci]litations, at the<br />)[cteurulogieal Observatory of )[acerata and the l'hysies lllstitute uf the<br />Ulliversity of Camerillo, ItUrillg the years 1967/08/69/70 measnrenwnts have<br />beell catTied uut un t...

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Main Author: A. MURRI
Format: Article
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia (INGV) 1970-06-01
Series:Annals of Geophysics
Online Access:http://www.annalsofgeophysics.eu/index.php/annals/article/view/5147
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spelling doaj-9486a6ca378844f089982bb56bf7f01c2020-11-24T22:56:09ZengIstituto Nazionale di Geofisica e Vulcanologia (INGV)Annals of Geophysics1593-52132037-416X1970-06-0123436338410.4401/ag-5147Rebaviour of tbe electric conductivity of tbe precipitationsA. MURRIContinuing the researl'hes on the preci]litations, at the<br />)[cteurulogieal Observatory of )[acerata and the l'hysies lllstitute uf the<br />Ulliversity of Camerillo, ItUrillg the years 1967/08/69/70 measnrenwnts have<br />beell catTied uut un the conductivity of Jiquid amI solid predpitatiolls with<br />the aim of determining- the beha viuur at differellt altit1HIes.<br />lt hM thus bcen found that the conductivity decrca~cs lillearly ill<br />the eOllr.~e of the raill Cali iC the willd remains cUllstallt ill dirertion, while<br />the litwar hehaviollr ceases with the changing of diredinn of the witllt.<br />The behaviour nf the conductivity is analogou~ at the two (juntaH of obHer.<br />valiun, except the value of the same whirh appears millor at higher quota.<br />The law of di.~trihution of the (~otllludivity, considerell as reganis the llellsity<br />of rainfall, may be re]ll'esenteli with a ]Jarticular fllnction whkh has belm<br />calculated. However the dispersion of tlte values appears considerable, in<br />re1ation to the llifferent meteurolog-iral situat ions that aceumpanied the Cali<br />uf the pn'(~i]litatinns, ohjed of the researclt. There have also been Jixell<br />the tran~pnrt equations that reglllatll, in turblllent air maHSt's, the lliffllsion<br />Hf tlw partides tu which the conductivity of the raills is due.http://www.annalsofgeophysics.eu/index.php/annals/article/view/5147
collection DOAJ
language English
format Article
sources DOAJ
author A. MURRI
spellingShingle A. MURRI
Rebaviour of tbe electric conductivity of tbe precipitations
Annals of Geophysics
author_facet A. MURRI
author_sort A. MURRI
title Rebaviour of tbe electric conductivity of tbe precipitations
title_short Rebaviour of tbe electric conductivity of tbe precipitations
title_full Rebaviour of tbe electric conductivity of tbe precipitations
title_fullStr Rebaviour of tbe electric conductivity of tbe precipitations
title_full_unstemmed Rebaviour of tbe electric conductivity of tbe precipitations
title_sort rebaviour of tbe electric conductivity of tbe precipitations
publisher Istituto Nazionale di Geofisica e Vulcanologia (INGV)
series Annals of Geophysics
issn 1593-5213
2037-416X
publishDate 1970-06-01
description Continuing the researl'hes on the preci]litations, at the<br />)[cteurulogieal Observatory of )[acerata and the l'hysies lllstitute uf the<br />Ulliversity of Camerillo, ItUrillg the years 1967/08/69/70 measnrenwnts have<br />beell catTied uut un the conductivity of Jiquid amI solid predpitatiolls with<br />the aim of determining- the beha viuur at differellt altit1HIes.<br />lt hM thus bcen found that the conductivity decrca~cs lillearly ill<br />the eOllr.~e of the raill Cali iC the willd remains cUllstallt ill dirertion, while<br />the litwar hehaviollr ceases with the changing of diredinn of the witllt.<br />The behaviour nf the conductivity is analogou~ at the two (juntaH of obHer.<br />valiun, except the value of the same whirh appears millor at higher quota.<br />The law of di.~trihution of the (~otllludivity, considerell as reganis the llellsity<br />of rainfall, may be re]ll'esenteli with a ]Jarticular fllnction whkh has belm<br />calculated. However the dispersion of tlte values appears considerable, in<br />re1ation to the llifferent meteurolog-iral situat ions that aceumpanied the Cali<br />uf the pn'(~i]litatinns, ohjed of the researclt. There have also been Jixell<br />the tran~pnrt equations that reglllatll, in turblllent air maHSt's, the lliffllsion<br />Hf tlw partides tu which the conductivity of the raills is due.
url http://www.annalsofgeophysics.eu/index.php/annals/article/view/5147
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