Solar system

Research group

Research theme

Sub department

About

Related research groups

Exploring the Saturn System in the Thermal Infrared: The Composite Infrared Spectrometer

Chapter in The Cassini-Huygens Mission, Springer Nature (2004) 169-297

Authors:

FM Flasar, VG Kunde, MM Abbas, RK Achterberg, P Ade, A Barucci, B Bézard, GL Bjoraker, JC Brasunas, S Calcutt, R Carlson, CJ Césarsky, BJ Conrath, A Coradini, R Courtin, A Coustenis, S Edberg, S Edgington, C Ferrari, T Fouchet, D Gautier, PJ Gierasch, K Grossman, P Irwin, DE Jennings, E Lellouch, AA Mamoutkine, A Marten, JP Meyer, CA Nixon, GS Orton, TC Owen, JC Pearl, R Prangé, F Raulin, PL Read, PN Romani, RE Samuelson, ME Segura, MR Showalter, AA Simon-Miller, MD Smith, JR Spencer, LJ Spilker, FW Taylor
More details from the publisher

Hydrothermal plume dynamics on Europa: Implications for chaos formation

Journal of Geophysical Research American Geophysical Union (AGU) 109:E3 (2004)

Authors:

Jason C Goodman, Geoffrey C Collins, John Marshall, Raymond T Pierrehumbert
More details from the publisher

Retrievals of jovian tropospheric phosphine from Cassini/CIRS

ICARUS 172:1 (2004) 37-49

Authors:

PGJ Irwin, P Parrish, T Fouchet, SB Calcutt, FW Taylor, AA Simon-Miller, CA Nixon
More details from the publisher

Glacial flow of floating marine ice in “Snowball Earth”

Journal of Geophysical Research: Oceans American Geophysical Union (AGU) 108:C10 (2003) 2002JC001471

Authors:

Jason C Goodman, Raymond T Pierrehumbert

Abstract:

Simulations of frigid Neoproterozoic climates have not considered the tendency of thick layers of floating marine ice to deform and spread laterally. We have constructed a simple model of the production and flow of marine ice on a planetary scale, and determined ice thickness and flow in two situations: when the ocean is globally ice‐covered (“hard snowball”) and when the tropical waters remain open (“soft snowball”). In both cases, ice flow strongly affects the distribution of marine ice. Flowing ice probably carries enough latent heat and freshwater to significantly affect the transition into a Snowball Earth climate. We speculate that flowing marine ice, rather than continental ice sheets, may be the erosive agent that created some Neoproterozoic glacial deposits.
More details from the publisher
More details

Erratum: Decay of passive scalars under the action of single scale smooth velocity fields in bounded two-dimensional domains - From non-self-similar probability distribution functions to self-similar eigenmodes (Physical Review E (2002) 66 (056302))

Physical Review E - Statistical, Nonlinear, and Soft Matter Physics 68:1 2 (2003) 199031

Authors:

J Sukhatme, RT Pierrehumbert