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

Frank S. Marzano | Zendy; Luigi Mereu | Zendy; Mario Montopoli | Zendy; Domenico Cimini | Zendy; Giovanni Martucci | Zendy

Open Access

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

Author(s) -

Frank S. Marzano,

Luigi Mereu,

Mario Montopoli,

Domenico Cimini,

Giovanni Martucci

Publication year - 2015

Publication title -

annals of geophysics

Language(s) - English

Resource type - Journals

SCImago Journal Rank - 0.394

H-Index - 60

eISSN - 2037-416X

pISSN - 1593-5213

DOI - 10.4401/ag-6762

Subject(s) - volcanic ash , volcano , geology , lidar , tephra , radar , ceilometer , volcanic arc , meteorology , remote sensing , seismology , subduction , geography , telecommunications , computer science , tectonics

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. [...]

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