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J. G. Esler

Researcher at University College London

Publications -  38
Citations -  1109

J. G. Esler is an academic researcher from University College London. The author has contributed to research in topics: Vortex & Polar vortex. The author has an hindex of 16, co-authored 37 publications receiving 1013 citations.

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A New Look at Stratospheric Sudden Warmings. Part III: Polar Vortex Evolution and Vertical Structure

TL;DR: In this paper, the evolution of the Arctic polar vortex during observed major midwinter stratospheric sudden warmings (SSWs) is investigated for the period 1957-2002, using 40-yr European Centre for Medium-Range Weather Forecasts (ECMWF) Re-Analysis (ERA-40) Ertel's potential vorticity (PV) and temperature fields.
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Wave patterns generated by an axisymmetric obstacle in a two-layer flow

TL;DR: In this paper, a 3D reconstruction of the interface between the two layers of a two-layer stratified fluid is used to investigate the wave pattern as a function of the Froude number, based on the relative density of the fluid layers.
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Stratospheric Sudden Warmings as Self-Tuning Resonances. Part I: Vortex Splitting Events

TL;DR: In this article, the fundamental dynamics of vortex splitting in stratospheric sudden warmings (SSWs), which are known to be predominantly barotropic in nature, are reexamined using an idealized single-layer f-plane model.
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A Lagrangian perspective of the tropopause and the ventilation of the lowermost stratosphere

TL;DR: In this paper, back trajectories driven by large-scale analyzed wind fields are used to investigate troposphere to stratosphere transport (TST) in the Northern Hemisphere tropopause region, as well as the surface sources for such transport, defined in terms of the locations where each trajectory last left the atmospheric boundary layer ( log pressure height z* < 1 km).
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Dispersive dam-break and lock-exchange flows in a two-layer fluid

TL;DR: Dam break and lock exchange flows are considered in a Boussinesq two-layer fluid system in a uniform two-dimensional channel in this paper, where the focus is on inviscid 'weak' dam breaks or lock exchanges, for which waves generated from the initial conditions do not break, but instead disperse in a so-called undular bore.