Rebaviour of tbe electric conductivity of tbe precipitations
Main Article Content
Abstract
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.
)[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.
Article Details
How to Cite
MURRI, A. (1970) “Rebaviour of tbe electric conductivity of tbe precipitations”, Annals of Geophysics, 23(4), pp. 363–384. doi: 10.4401/ag-5147.
Issue
Section
OLD
Open-Access License
No Permission Required
Istituto Nazionale di Geofisica e Vulcanologia applies the Creative Commons Attribution License (CCAL) to all works we publish.
Under the CCAL, authors retain ownership of the copyright for their article, but authors allow anyone to download, reuse, reprint, modify, distribute, so long as the original authors and source are cited. No permission is required from the authors or the publishers.
In most cases, appropriate attribution can be provided by simply citing the original article.
If the item you plan to reuse is not part of a published article (e.g., a featured issue image), then please indicate the originator of the work, and the volume, issue, and date of the journal in which the item appeared. For any reuse or redistribution of a work, you must also make clear the license terms under which the work was published.
This broad license was developed to facilitate open access to, and free use of, original works of all types. Applying this standard license to your own work will ensure your right to make your work freely and openly available. For queries about the license, please contact ann.geophys@ingv.it.