Annex to: Volcanic Ash Cloud Observation using Ground-based Ka-band Radar and Near-Infrared Lidar Ceilometer during the Eyjafjallajökull eruption

Volcanic ash plumes are formed during explosive volcanic eruptions. After advection over several thousands of kilometers, volcanic ash particles are highly fragmented, dispersed and aged with micron- sized sorting. This Annex describes the ash microphysical modeling and the simulated radar and lidar...

Full description

Bibliographic Details
Published in:Annals of Geophysics
Main Authors: Marzano, Frank S., Mereu, Luigi, Montopoli, Mario, Cimini, Domenico, Martucci, Giovanni
Format: Article in Journal/Newspaper
Language:English
Published: Istituto Nazionale di Geofisica e Vulcanologia, INGV 2015
Subjects:
Eyjafjallajökull
Online Access:https://www.annalsofgeophysics.eu/index.php/annals/article/view/6762
https://doi.org/10.4401/ag-6762
Description
Summary:Volcanic ash plumes are formed during explosive volcanic eruptions. After advection over several thousands of kilometers, volcanic ash particles are highly fragmented, dispersed and aged with micron- sized sorting. This Annex describes the ash microphysical modeling and the simulated radar and lidar signatures. [.]

Similar Items