Differenze pluviometriche tra i versanti tirrenico ed adriatico lungo l’allineamento Livorno-Monte Cimone-Modena

Differences in rainfall between the Tyrrhenian and the Adriatic side of the Northern Apennines range along Livorno – M. Cimone – Modena traverse

Authors

  • Franco Rapetti Centro di Studio per la Geologia Struttuale e Dinamica dell’Appennino, C.N.R., Pisa, Italy Author
  • Sebastiano Vittorini Centro di Studio per la Geologia Struttuale e Dinamica dell’Appennino, C.N.R., Pisa, Italy Author

Keywords:

Rainfall amount, Rainfall intensity, Rainfall rate, Rainfall altimetric gradient, Tuscan-Aemilian Apennines

Abstract

Amount, intensity and rate of precipitations recorded in sixteen stations along a line crossing the Tuscan-Aemilian section of the Northern Apennines have been considered. It has then been possible to compare the patterns of this climatic element on both sides of the mountain range. A marked difference between the two sides has been pointed out: the Tyrrhenian side results definitely more rainy than the Adriatic one. The altimetric gradient has also been calculated. It results non- uniform along the whole slope, on which it is possible to distinguish two sections, each of them showing a linear increase of rainfall: the foothill section and the mountain section. Even in this respect marked differences between the two sides of the Apennines have been observed.

Published

2024-07-11

Issue

Section

Research and review papers

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