Browning, K. A. and Field, M. (2004) Evidence from Meteosat imagery of the interaction of sting jets with the boundary layer. Meteorological Applications, 11 (4). pp. 277-289. ISSN 1469-8080 doi: 10.1017/S1350482704001379
Abstract/Summary
Meteosat infra-red imagery for the Great Storm of October 1987 is analysed to show a series of very shallow arc-shaped and smaller chevron-shaped cloud features that were associated with damaging surface winds in the dry-slot region of this extra-tropical cyclone. Hypotheses are presented that attribute these low-level cloud features to boundary-layer convergence lines ahead of wind maxima associated with the downward transport of high momentum from overrunning, so-called sting-jet, flows originating in the storm's main cloud head. Copyright © 2004 Royal Meteorological Society.
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Item Type | Article |
URI | https://reading-clone.eprints-hosting.org/id/eprint/35115 |
Item Type | Article |
Refereed | Yes |
Divisions | Science > School of Mathematical, Physical and Computational Sciences > Department of Meteorology |
Publisher | Royal Meteorological Society |
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