Global gyrokinetic ITG turbulence simulations of MAST plasmas

37th EPS Conference on Plasma Physics 2010, EPS 2010 1 (2010) 521-524

Authors:

S Saarelma, A Bottino, J Candy, G Colyer, A Field, W Gutenfelder, P Hill, A Peeters, CM Roach

Evidence for Climate Change on Mars

Chapter in Solar System Update, Springer (2010) 135

Authors:

SR Lewis, PL Read

Abstract:

This book, the first in a series of forthcoming volumes, consists of topical and timely reviews of a number of carefully selected topics in solar systemn science.

Synchronization in a pair of thermally coupled rotating baroclinic annuli: understanding atmospheric teleconnections in the laboratory.

Phys Rev Lett 104:20 (2010) 204501

Authors:

AA Castrejón-Pita, PL Read

Abstract:

Synchronization phenomena in a fluid dynamical analogue of atmospheric circulation is studied experimentally by investigating the dynamics of a pair of thermally coupled, rotating baroclinic annulus systems. The coupling between the systems is in the well-known master-slave configuration in both periodic and chaotic regimes. Synchronization tools such as phase dynamics analysis are used to study the dynamics of the coupled system and demonstrate phase synchronization and imperfect phase synchronization, depending upon the coupling strength and parameter mismatch.

On the dynamics of multiple systems of hot super-Earths and Neptunes: Tidal circularization, resonance and the HD 40307 system

(2010)

Authors:

John CB Papaloizou, Caroline Terquem

Assessing eddy parameterization schemes in a differentially heated rotating annulus experiment

Ocean Modelling 32:3-4 (2010) 118-131

Authors:

E Pérez-Pérez, PL Read, IM Moroz

Abstract:

We investigate three of the most common hypotheses underpinning parameterizations of baroclinic eddy fluxes in the context of the differentially heated rotating annulus experiment. The investigation is carried out over a region of parameter space which embraces the onset of baroclinic instability, the regular wave regime and the onset of irregular flows, the latter of which is arguably most relevant to oceanic conditions. Through diagnostics from a 2D axisymmetric and a 3D eddy-resolving numerical model, it was found that the transport of heat by baroclinic eddies is not strictly an adiabatic process but that diffusive 'ventilation' of the flow in the thermal boundary layers is significant during the nonlinear development of the flow. Total heat transport, however, is conserved overall. Depending on the stages of flow evolution and on the region in parameter space under consideration, either heat, quasi-geostrophic potential vorticity (QGPV) or relative vorticity (QGRV) may become a suitable variable on which to parameterize baroclinic eddy fluxes in a down-gradient manner. These results raise issues for eddy parameterization schemes that rely on these assumptions in ocean and atmosphere models. © 2009 Elsevier Ltd.