Volcanic ash layer depth: Processes and mechanisms. Issue 2 (26th January 2015)

• Record Type: Journal Article
• Authors: Dacre, H. F.; Grant, A. L. M.; Harvey, N. J.; Thomson, D. J.; Webster, H. N.; Marenco, F.
• Is Part Of: Geophysical research letters. Volume 42:Issue 2(2015:Jan.)
• Page Start: 637
• Page End: 645
• Publication Date: 2015-01-26
• Subjects: vertical wind shear -- ash size distribution -- turbulent mixing -- ash sedimentation; Geophysics -- Periodicals; Planets -- Periodicals; Lunar geology -- Periodicals; 550
• DOI: 10.1002/2014GL062454
• Languages: English
• ISSNs: 0094-8276

Abstract

Abstract: The long duration of the 2010 Eyjafjallajökull eruption provided a unique opportunity to measure a widely dispersed volcanic ash cloud. Layers of volcanic ash were observed by the European Aerosol Research Lidar Network with a mean depth of 1.2 km and standard deviation of 0.9 km. In this paper we evaluate the ability of the Met Office's Numerical Atmospheric‐dispersion Modelling Environment (NAME) to simulate the observed ash layers and examine the processes controlling their depth. NAME simulates distal ash layer depths exceptionally well with a mean depth of 1.2 km and standard deviation of 0.7 km. The dominant process determining the depth of ash layers over Europe is the balance between the vertical wind shear (which acts to reduce the depth of the ash layers) and vertical turbulent mixing (which acts to deepen the layers). Interestingly, differential sedimentation of ash particles and the volcano vertical emission profile play relatively minor roles. Key Points: NAME distal ash layer depths compare exceptionally well with observations Ash layer depth is determined by vertical wind shear and turbulent mixing The volcano characteristics have a minor effect on distal ash layer depths