Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Tephra hazard assessment at Mt. Etna (Italy)

View through CrossRef
Abstract. In this paper we present a probabilistic hazard assessment for tephra fallout at Mt. Etna (Italy) associated with both short- and long-lived eruptions. We analyzed wind data from the atmospheric soundings of the Italian Air Force at Trapani Birgi (western Sicily), and use the TEPHRA advection-diffusion-sedimentation model to capture the variation of wind speed and direction with time. Two different typologies of eruptions were considered in our analysis: eruptions forming strong short-lived plumes (SSL eruptions) and eruptions forming weak long-lived plumes (WLL eruptions). One Eruption Scenario (OES) for both typologies and the Eruption Range Scenario (ERS) for WLL eruptions were identified based on well documented past activity of Etna since the '90. First, model calibration was carried out for two well-known Etna explosive eruptions: the 22 July 1998 and July 2001 Etna eruptions. Second, probabilistic maps were compiled. Results clearly show that the eastern flanks are significantly affected by tephra deposition and that the WLL eruptions and the Plinian eruption of 122 BC represent the largest threat for both infrastructures and agriculture.
Title: Tephra hazard assessment at Mt. Etna (Italy)
Description:
Abstract.
In this paper we present a probabilistic hazard assessment for tephra fallout at Mt.
Etna (Italy) associated with both short- and long-lived eruptions.
We analyzed wind data from the atmospheric soundings of the Italian Air Force at Trapani Birgi (western Sicily), and use the TEPHRA advection-diffusion-sedimentation model to capture the variation of wind speed and direction with time.
Two different typologies of eruptions were considered in our analysis: eruptions forming strong short-lived plumes (SSL eruptions) and eruptions forming weak long-lived plumes (WLL eruptions).
One Eruption Scenario (OES) for both typologies and the Eruption Range Scenario (ERS) for WLL eruptions were identified based on well documented past activity of Etna since the '90.
First, model calibration was carried out for two well-known Etna explosive eruptions: the 22 July 1998 and July 2001 Etna eruptions.
Second, probabilistic maps were compiled.
Results clearly show that the eastern flanks are significantly affected by tephra deposition and that the WLL eruptions and the Plinian eruption of 122 BC represent the largest threat for both infrastructures and agriculture.

Related Results

Tephra layers in Perunika Glacier, Livingston Island, Antarctica
Tephra layers in Perunika Glacier, Livingston Island, Antarctica
<p>Perunika Glacier is an 8 km long and 3 km wide roughly crescent-shaped glacier in Livingston Island, South Shetland Islands, Antarctica. The glacier is heavily cre...
Electron Microprobe Analysis of Glass Shards from Tephra Assigned to Set W, Mount St. Helens, Washington
Electron Microprobe Analysis of Glass Shards from Tephra Assigned to Set W, Mount St. Helens, Washington
We have extended the fallout areas for each of two members of tephra-set W, erupted from Mount St. Helens about 1500 ad , by several hundred kilometers beyond the limits mapped in ...
Tephra deposits associated with silicic domes and lava flows
Tephra deposits associated with silicic domes and lava flows
Most phases of silicic lava dome growth have some associated explosive activity. Tephra produced during this activity have depositional characteristics, grain sizes, and grain shap...
Etna volcano monitoring by remote sensing systems
Etna volcano monitoring by remote sensing systems
The Istituto Nazionale di Geofisica e Vulcanologia - Osservatorio Etneo (INGV-OE) is in charge to monitor Mt. Etna (Catania, Italy), one of the most active volcanoes in Europe. Its...
Multi-Hazard Entanglement
Multi-Hazard Entanglement
Globally, natural hazards such as tropical cyclones cause billions of dollars in damages. These hazards rarely occur in isolation. Frequently, one hazard triggers another, such as ...
Phreatomagmatic maar-diatreme volcanoes and their incremental growth: a model
Phreatomagmatic maar-diatreme volcanoes and their incremental growth: a model
Abstract We report here a growth model for phreatomagmatic maar-diatreme volcanoes with respect to the number of eruptions documented in the tephra beds of maar tephra ri...
The Effects of the Quasi-Biannual Oscillation on Tephra Distribution from a Plinian Eruption
The Effects of the Quasi-Biannual Oscillation on Tephra Distribution from a Plinian Eruption
<p>The quasi-biannual oscillation (QBO) dominates the equatorial zonal wind in the tropical stratosphere. Alternating easterly and westerly wind regimes form in the u...
Electron Microprobe Data for Tephra Attributed to Glacier Peak, Washington
Electron Microprobe Data for Tephra Attributed to Glacier Peak, Washington
Reference samples of three prominent pumice units of Glacier Peak tephra collected east of the volcano within a distance of 100 km are similar petrographically to units described b...

Back to Top