Prof. Peter Read: Publications

A climate database for Mars

JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS 104:E10 (1999) 24177-24194

Authors:

SR Lewis, M Collins, PL Read, F Forget, F Hourdin, R Fournier, C Hourdin, O Talagrand, JP Huot

Experiments on a barotropic rotating shear layer.: Part 1.: Instability and steady vortices

JOURNAL OF FLUID MECHANICS 383 (1999) 143-173

Authors:

WG Früh, PL Read

Flow-field and point velocity measurements in a barotropically unstable shear layer

PHYSICS AND CHEMISTRY OF THE EARTH PART B-HYDROLOGY OCEANS AND ATMOSPHERE 24:5 (1999) 461-466

Authors:

WG Früh, PL Read

Generation of inertia-gravity waves by a time-dependent baroclinic wave in the laboratory

PHYSICS AND CHEMISTRY OF THE EARTH PART B-HYDROLOGY OCEANS AND ATMOSPHERE 24:5 (1999) 455-460

Authors:

AF Lovegrove, PL Read, CJ Richards

Improved general circulation models of the Martian atmosphere from the surface to above 80 km

JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS 104:E10 (1999) 24155-24175

Authors:

F Forget, F Hourdin, R Fournier, C Hourdin, O Talagrand, M Collins, SR Lewis, PL Read, JP Huot

91̽��

Prof. Peter Read

Research theme

Sub department

A climate database for Mars

Authors:

Experiments on a barotropic rotating shear layer.: Part 1.: Instability and steady vortices

Authors:

Flow-field and point velocity measurements in a barotropically unstable shear layer

Authors:

Generation of inertia-gravity waves by a time-dependent baroclinic wave in the laboratory

Authors:

Improved general circulation models of the Martian atmosphere from the surface to above 80 km

Authors:

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91̽��

Prof. Peter Read

Research theme

Sub department

Research groups

A climate database for Mars

Authors:

Experiments on a barotropic rotating shear layer.: Part 1.: Instability and steady vortices

Authors:

Flow-field and point velocity measurements in a barotropically unstable shear layer

Authors:

Generation of inertia-gravity waves by a time-dependent baroclinic wave in the laboratory

Authors:

Improved general circulation models of the Martian atmosphere from the surface to above 80 km

Authors: