Abstract. Fumarolic fields, especially those with near-surface soil
temperature <100 ∘C, are very common features of active
or quiescent volcanoes, with both open or closed conduits. Their spatial
extent, as well as the time variability of their temperature, are
conditioned by three main factors: (1) Local hydro-meteorological conditions;
(2) Vapor flow from the underlying volcanic-hydrothermal system; (3) Permeability variation induced by stress field changes and/or deposition
dissolution cycles of hydrothermal alteration minerals. Once depurated from
the exogenous noise, time variations of the thermal signal, in term of both
short-lasting transients and medium/long term trends, reflect changes in the
activity state of the related volcanic system, and/or of seismic activity,
also of tectonic origin, affecting volcanoes. Theoretical models of heat
transfer processes are discussed, highlighting how it is very difficult
distinguish between conductive and convective mechanisms or calculating heat
fluxes: as a consequence, thermal data from low temperature fumaroles should
be used as qualitative proxies of volcano-tectonic phenomena acting on the
monitored volcanoes. Following the description of the measuring systems and of the criteria for
designing a performing network for thermal monitoring of fumaroles, some
case histories from Italian volcanoes (Vulcano, Stromboli, Mt. Etna, Mt. Vesuvius) are presented, illustrating how in the last years the monitoring
of low temperature fumaroles have given useful insights on the evolution of
the activity state of these volcanoes.