Rebaviour of tbe electric conductivity of tbe precipitations



Continuing the researl'hes on the preci]litations, at the
)[cteurulogieal Observatory of )[acerata and the l'hysies lllstitute uf the
Ulliversity of Camerillo, ItUrillg the years 1967/08/69/70 measnrenwnts have
beell catTied uut un the conductivity of Jiquid amI solid predpitatiolls with
the aim of determining- the beha viuur at differellt altit1HIes.
lt hM thus bcen found that the conductivity decrca~cs lillearly ill
the eOllr.~e of the raill Cali iC the willd remains cUllstallt ill dirertion, while
the litwar hehaviollr ceases with the changing of diredinn of the witllt.
The behaviour nf the conductivity is analogou~ at the two (juntaH of obHer.
valiun, except the value of the same whirh appears millor at higher quota.
The law of di.~trihution of the (~otllludivity, considerell as reganis the llellsity
of rainfall, may be re]ll'esenteli with a ]Jarticular fllnction whkh has belm
calculated. However the dispersion of tlte values appears considerable, in
re1ation to the llifferent meteurolog-iral situat ions that aceumpanied the Cali
uf the pn'\(~i]litatinns, ohjed of the researclt. There have also been Jixell
the tran~pnrt equations that reglllatll, in turblllent air maHSt's, the lliffllsion
Hf tlw partides tu which the conductivity of the raills is due.

Full Text:



We use cookies to ensure that we give you the best experience on our website. If you continue to use this site we will assume that you are happy with it (Read more).

Published by INGV, Istituto Nazionale di Geofisica e Vulcanologia - ISSN: 2037-416X