Publications


Introduction

in , 105 (2011) 113-116

J Brindley, P Read, J Gibbon, A Soward


Infrared Radiation and Planetary Temperature

PHYSICS OF SUSTAINABLE ENERGY II: USING ENERGY EFFICIENTLY AND PRODUCING IT RENEWABLY 1401 (2011)

RT Pierrehumbert


Bifurcations leading to summer Arctic sea ice loss

JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 116 (2011) ARTN D19120

DS Abbot, M Silber, RT Pierrehumbert


Climate Stabilization Targets: Emissions, Concentrations, and Impacts over Decades to Millennia

National Academies Press, 2011

COSTFAGG Concentrations, BOASA Climate, DOEAL Studies, NR Council

The book quantifies the outcomes of different stabilization targets for greenhouse gas concentrations using analyses and information drawn from the scientific literature.


Some fine points on radiative forcing Reply

PHYSICS TODAY 64 (2011) 12-12

RT Pierrehumbert


Saturn: Storm-clouds brooding on towering heights

Nature 475 (2011) 44-45

P Read


Assessing atmospheric predictability on Mars using numerical weather prediction and data assimilation

QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY 136 (2010) 1614-1635

P Rogberg, PL Read, SR Lewis, L Montabone


Synchronization in climate dynamics and other extended systems

Understanding Complex Systems 2010 (2010) 153-176

PL Read, AA Castrejón-Pita

Synchronization is now well established as representing coherent behaviour between two or more otherwise autonomous nonlinear systems subject to some degree of coupling. Such behaviour has mainly been studied to date, however, in relatively low-dimensional discrete systems or networks. But the possibility of similar kinds of behaviour in continuous or extended spatiotemporal systems has many potential practical implications, especially in various areas of geophysics. We review here a range of cyclically varying phenomena within the Earth's climate system for which there may be some evidence or indication of the possibility of synchronized behaviour, albeit perhaps imperfect or highly intermittent. The exploitation of this approach is still at a relatively early stage within climate science and dynamics, in which the climate system is regarded as a hierarchy of many coupled sub-systems with complex nonlinear feedbacks and forcings. The possibility of synchronization between climate oscillations (global or local) and a predictable external forcing raises important questions of how models of such phenomena can be validated and verified, since the resulting response may be relatively insensitive to the details of the model being synchronized. The use of laboratory analogues may therefore have an important role to play in the study of natural systems that can only be observed and for which controlled experiments are impossible. We go on to demonstrate that synchronization can be observed in the laboratory, even in weakly coupled fluid dynamical systems that may serve as direct analogues of the behaviour of major components of the Earth's climate system. The potential implications and observability of these effects in the long-term climate variability of the Earth is further discussed. © 2010 Springer-Verlag Berlin Heidelberg.


Predicting chaotic climates: from Earth to super-Earths?

MATHEMATICS AND ASTRONOMY: A JOINT LONG JOURNEY 1283 (2010) 57-74

PL Read


Mudball: Surface dust and Snowball Earth deglaciation

JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 115 (2010) ARTN D03104

DS Abbot, RT Pierrehumbert


Saturn's emitted power

Journal of Geophysical Research E: Planets 115 (2010)

L Li, BJ Conrath, PJ Gierasch, RK Achterberg, CA Nixon, AA Simon-Miller, FM Flasar, D Banfield, KH Baines, RA West, AP Ingersoll, AR Vasavada, AD Del Genio, CC Porco, AA Mamoutkine, ME Segura, GL Bjoraker, GS Orton, LN Fletcher, PGJ Irwin, PL Read

Long-term (2004-2009) on-orbit observations by Cassini Composite Infrared Spectrometer are analyzed to precisely measure Saturn's emitted power and its meridional distribution. Our evaluations suggest that the average global emitted power is 4.952 ± 0.035 W m-2 during the period of 2004-2009. The corresponding effective temperature is 96.67 ± 0.17 K. The emitted power is 16.6% higher in the Southern Hemisphere than in the Northern Hemisphere. From 2005 to 2009, the global mean emitted power and effective temperature decreased by ∼2% and ∼0.5%, respectively. Our study further reveals the interannual variability of emitted power and effective temperature between the epoch of Voyager (∼1 Saturn year ago) and the current epoch of Cassini, suggesting changes in the cloud opacity from year to year on Saturn. The seasonal and interannual variability of emitted power implies that the energy balance and internal heat are also varying. Copyright © 2010 by the American Geophysical Union.


The Importance of Ice Vertical Resolution for Snowball Climate and Deglaciation

JOURNAL OF CLIMATE 23 (2010) 6100-6109

DS Abbot, I Eisenman, RT Pierrehumbert


Evidence for Climate Change on Mars

in Solar System Update, Springer (2010) 135-

SR Lewis, PL Read

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.


Effectiveness of stirring measures in an axisymmetric rotating annulus flow

PHYSICA D-NONLINEAR PHENOMENA 239 (2010) 675-683

RJ Keane, PL Read, GP King


Structure and dynamics of the Martian lower and middle atmosphere as observed by the Mars Climate Sounder: Seasonal variations in zonal mean temperature, dust, and water ice aerosols

JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS 115 (2010) ARTN E12016

DJ McCleese, NG Heavens, JT Schofield, WA Abdou, JL Bandfield, SB Calcutt, PGJ Irwin, DM Kass, A Kleinbohl, SR Lewis, DA Paige, PL Read, MI Richardson, JH Shirley, FW Taylor, N Teanby, RW Zurek


Global gyrokinetic ITG turbulence simulations of MAST plasmas

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

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


Structure and dynamics of the Martian lower and middle atmosphere as observed by the Mars Climate Sounder: Seasonal variations in zonal mean temperature, dust, and water ice aerosols

Journal of Geophysical Research E: Planets 115 (2010)

DJ McCleese, NG Heavens, JT Schofield, WA Abdou, JL Bandfield, SB Calcutt, PGJ Irwin, DM Kass, A Kleinböhl, SR Lewis, DA Paige, PL Read, MI Richardson, JH Shirley, FW Taylor, N Teanby, RW Zurek

The first Martian year and a half of observations by the Mars Climate Sounder aboard the Mars Reconnaissance Orbiter has revealed new details of the thermal structure and distributions of dust and water ice in the atmosphere. The Martian atmosphere is shown in the observations by the Mars Climate Sounder to vary seasonally between two modes: a symmetrical equinoctial structure with middle atmosphere polar warming and a solstitial structure with an intense middle atmosphere polar warming overlying a deep winter polar vortex. The dust distribution, in particular, is more complex than appreciated before the advent of these high (∼5 km) vertical resolution observations, which extend from near the surface to above 80 km and yield 13 dayside and 13 nightside pole-to-pole cross sections each day. Among the new features noted is a persistent maximum in dust mass mixing ratio at 15-25 km above the surface (at least on the nightside) during northern spring and summer. The water ice distribution is very sensitive to the diurnal and seasonal variation of temperature and is a good tracer of the vertically propagating tide. Copyright 2010 by the American Geophysical Union.


A bulk cloud parameterization in a Venus General Circulation Model

ICARUS 206 (2010) 662-668

C Lee, SR Lewis, PL Read


A laboratory model of Saturn's North Polar Hexagon

Icarus 206 (2010) 755-763

AC Barbosa Aguiar, PL Read, RD Wordsworth, T Salter, Y Hiro Yamazaki

A hexagonal structure has been observed at ∼76°N on Saturn since the 1980s (Godfrey, D.A. [1988]. Icarus 76, 335-356). Recent images by Cassini (Baines, K., Momary, T., Roos-Serote, M., Atreya, S., Brown, R., Buratti, B., Clark, R., Nicholson, P. [2007]. Geophys. Res. Abstr. 9, 02109; Baines, K., Momary, T., Fletcher, L., Kim, J., Showman, A., Atreya, S., Brown, R., Buratti, B., Clark, R., Nicholson, P. [2009]. Geophys. Res. Abstr. 11, 3375) have shown that the feature is still visible and largely unchanged. Its long lifespan and geometry has puzzled the planetary physics community for many years and its origin remains unclear. The measured rotation rate of the hexagon may be very close to that of the interior of the planet (Godfrey, D.A. [1990]. Science 247, 1206-1208; Caldwell, J., Hua, X., Turgeon, B., Westphal, J.A., Barnet, C.D. [1993]. Science 206, 326-329; Sánchez-Lavega, A., Lecacheux, J., Colas, F., Laques, P. [1993]. Science 260, 329-332), leading to earlier interpretations of the pattern as a stationary planetary wave, continuously forced by a nearby vortex (Allison, M., Godfrey, D.A., Beebe, R.F. [1990]. Science 247, 1061-1063). Here we present an alternative explanation, based on an analysis of both spacecraft observations of Saturn and observations from laboratory experiments where the instability of quasi-geostrophic barotropic (vertically uniform) jets and shear layers is studied. We also present results from a barotropic linear instability analysis of the saturnian zonal wind profile, which are consistent with the presence of the hexagon in the North Pole and absence of its counter-part in the South Pole. We propose that Saturn's long-lived polygonal structures correspond to wavemodes caused by the nonlinear equilibration of barotropically unstable zonal jets. © 2009 Elsevier Inc. All rights reserved.


Geophysical flows as dynamical systems: the influence of Hide's experiments

ASTRONOMY & GEOPHYSICS 51 (2010) 28-35

M Ghil, PL Read, LA Smith

Pages