Nonhydrostatic wave generation at strained fronts

Callum J. Shakespeare*

*Corresponding author for this work

Research output: Contribution to journalArticlepeer-review

3 Citations (Scopus)

Abstract

A simple analytical model is developed to describe wave generation during frontogenesis forced by a horizontal strain field. In contrast to previous models, neither geostrophic nor hydrostatic balance is assumed. The generated waves are trapped in the strain field and form steady bands of enhanced vertical flow on either side of the surface front on scales from 1 to 100 km. The predictions of the analytical model are confirmed by comparison with fully nonlinear numerical simulations.

Original languageEnglish
Pages (from-to)2837-2850
Number of pages14
JournalJournal of the Atmospheric Sciences
Volume73
Issue number7
DOIs
Publication statusPublished - 2016
Externally publishedYes

Fingerprint

Dive into the research topics of 'Nonhydrostatic wave generation at strained fronts'. Together they form a unique fingerprint.

Cite this