Following large explosive volcanic eruptions precipitation decreases over much of the globe1-6, particularly in climatologically wet regions4,5. Stratospheric volcanic aerosols reflect sunlight, which reduces evaporation, whilst surface cooling stabilises the atmosphere and reduces its water-holding capacity7. Circulation changes modulate this global precipitation reduction on regional scales1,...

In this paper we present a model for the growth of a maar-diatreme complex in a shallow marine environment. The Miocene-age Costa Giardini diatreme near Sortino, in the region of the Iblei Mountains of southern Sicily, has an outer tuff ring formed by the accumulation of debris flows and surge deposits during hydromagmatic eruptions. Vesicular lava clasts, accretionary lapilli and bombs in the ...

Recent observations have shown that explosive volcanic eruptions can generate low frequency surface pressure signals that are observable with microbarographs, and can be interpreted as atmospheric internal waves (Baines & Sacks 2013). Some examples from the Caribbean island of Montserrat are shown in Figure 1. Suitably interpreted, it is possible that these observations may give information abo...

Volcan Santiaguito (Guatemala) “breathes” with extraordinary regularity as the edifice’s conduit system accumulates free gas, which periodically vents to the atmosphere. Periodic pressurization controls explosion timing, which nearly always occurs at peak inflation, as detected with tiltmeters. Tilt cycles in January 2012 reveal regular 26 ± 6min inflation/deflation cycles corresponding to at l...

[1] Explosive eruptions can inject large amounts of volcanic gases into the stratosphere. These gases may be scavenged by hydrometeors within the eruption column, and high uncertainties remain regarding the proportion of volcanic gases, which eventually reach the stratosphere. These are caused by the difficulties of directly sampling explosive volcanic eruption columns and by the lack of labora...

Abstract One of the biggest challenges in volcanology is assessing role magma properties (volatile budgets, storage depths, and ascent rates) controlling eruption explosivity. We use a new approach based on apatite to estimate volatile contents rates from sequence sub-Plinian, effusive, Vulcanian deposits at Rabaul caldera (Papua New Guinea) emplaced 2006 CE probe mechanisms responsible for sud...

Explosive eruptions are the surface manifestation of dynamics that involve transfer magma from underground regions accumulation. Evidence involvement compositionally different magmas reservoirs is continuously increasing to countless cases. Yet, models eruption consider only uppermost portion plumbing system, neglecting connections deeper storage. Here we show extent and efficiency interconnect...