Evaluating the structure and magnitude of the ash plume during the initial phase of the 2010 Eyjafjallajökull eruption using lidar observations and NAME simulations

Author:

Dacre H. F.,Grant A. L. M.,Hogan R. J.,Belcher S. E.,Thomson D. J.,Devenish B. J.,Marenco F.,Hort M. C.,Haywood J. M.,Ansmann A.,Mattis I.,Clarisse L.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference27 articles.

1. The 16 April 2010 major volcanic ash plume over central Europe: EARLINET lidar and AERONET photometer observations at Leipzig an Munich, Germany;Ansmann;Geophys. Res. Lett.,2010

2. Observations of the altitude of the volcanic plume during the eruption of Eyjafjallajökull, April–May 2010;Arason;Earth Syst. Sci. Data Discuss.,2011

3. Total grain-size distribution and volume of tephra-fall deposits;Bonadonna;Bull. Volcanol.,2005

4. Numerical modelling of tephra fallout associated with dome collapses and Vulcanian explosions: Application to hazard assessment on Montserrat;Bonadonna,2002

5. The 1989–1990 eruption of Redoubt volcano, Alaska: Impacts on aircraft operations;Casadevall;J. Volcanol. Geotherm. Res.,1994

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