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Non-hydrostatic effects on mountain wave breaking in directional shear flows

TitleNon-hydrostatic effects on mountain wave breaking in directional shear flows
Publication TypeArticolo su Rivista peer-reviewed
Year of Publication2017
AuthorsGuarino, Maria Vittoria, and Teixeira Miguel A. C.
JournalQuarterly Journal of the Royal Meteorological Society
Volume143
Pagination3291 – 3297
Type of ArticleLetter
ISSN00359009
Abstract

Mountain waves excited by narrow 3D orography are investigated using idealized numerical simulations of atmospheric flows with directional wind shear. The stability of these waves is compared with the stability of hydrostatic mountain waves. The focus is on understanding how wave breaking is modified via gravity wave–critical level interaction, when non-hydrostatic (dispersive) effects arise. The influence of non-hydrostatic effects on wave breaking appears to be a function of the intensity of the background shear, increasing the stability of the flow (inhibiting wave breaking) for weak wind shear, but decreasing it instead (enhancing wave breaking) for stronger wind shear. © 2017 Royal Meteorological Society

Notes

Cited by: 2; All Open Access, Green Open Access

URLhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85031126279&doi=10.1002%2fqj.3157&partnerID=40&md5=82996e3bfaea7a7be05a23d735d7fc1e
DOI10.1002/qj.3157
Citation KeyGuarino20173291