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Juno Jupiter image

Simon Calcutt

Emeritus

Sub department

  • Atmospheric, Oceanic and Planetary Physics

Research groups

  • Planetary atmosphere observation analysis
  • Solar system
  • Space instrumentation
  • Planetary surfaces
simon.calcutt@physics.ox.ac.uk
Telephone: 01865 (2)72916
Atmospheric Physics Clarendon Laboratory, room 308
  • About
  • Publications

The origin of belt/zone contrasts in the atmosphere of Jupiter and their correlation with 5-micron opacity

Icarus 149 (2001) 397-415

Authors:

PG Irwin, A.L. Weir, F.W. Taylor, S.B. Calcutt
More details from the publisher

MUSE: Looking for life on Earth

ESA SP PUBL 496 (2001) 389-391

Authors:

AJ Penny, GR Davis, SB Calcutt, JR Drummond, DA Naylor, S Seager

Abstract:

Future missions to measure the mid-infrared spectra of extrasolar planets will obtain spectra spatially integrated over the visible hemisphere of the planet. Interpretation of these spectra will be difficult because they will depend on several imponderable factors; the axial inclination of the planet to the line of sight, the illumination of the planet by its parent star, and the planets' season and climatic state. The spectra will also contain variable components due to changing clouds, planetary rotation and the presence of large satellites. In order to interpret better such spectra, and to constrain the design of missions to measure them, a study is underway of a dedicated mission to take spectra of the spatially-unresolved Earth and to quantify the dependence of the spectrum on these variables.
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The origin of belt/zone contrasts in the atmosphere of Jupiter and their correlation with 5-μm opacity

ICARUS 149:2 (2001) 397-415

Authors:

PGJ Irwin, AL Weir, FW Taylor, SB Calcutt, RW Carlson
More details from the publisher

The NetLander atmospheric instrument system (ATMIS): Description and performance assessment

Planetary and Space Science 48:12-14 (2000) 1407-1420

Authors:

J Polkko, AM Harri, T Siili, F Angrilli, S Calcutt, D Crisp, S Larsen, JP Pommereau, P Stoppato, A Lehto, C Malique, JE Tillman

Abstract:

The pointwise meteorological observations of the Viking Lander and Mars Pathfinder as well as the orbital mapping and sounding performed by, e.g., Mariner 9, Viking Orbiters and the Mars Global Surveyor have given a good understanding of the basic behaviour of the Martian atmosphere. However, the more detailed characterisation of the Martian circulation patterns, boundary layer phenomena and climatological cycles requires deployment of meteorological surface networks. The European NetLander concept comprising four well-instrumented landers is being studied for launch in 2005 and operations spanning at least a Martian year in 2006-2008. The landers are to be deployed to areas in both Martian hemispheres from equatorial regions to low mid-latitudes. The NetLander atmospheric instrument system (ATMIS) on board each of the landers is designed to measure atmospheric vertical profiles of density, pressure and temperature during the descent onto the surface, as well as pressure, atmospheric and ground temperatures, wind, atmospheric optical thickness and humidity through a full Martian year, possibly beyond. The main operational objective of this meteorological experiment is to provide a regular time series of the meteorological parameters as well as accelerated measurement campaigns. Such a data set would substantially improve our understanding of the atmospheric structure, dynamics, climatological cycles, and the atmosphere-surface interactions. The ATMIS sensor systems and measurement approaches described here are based on solutions and technologies tested for similar observations on Mars-96, Mars Pathfinder, Huygens, and Mars Polar Lander. Although the number of observation sites only permits characterisation of some components of the general circulation, the NetLander ATMIS will more than double the number of in situ vertical profiles (only three profiles - two from Viking Landers and one from Mars Pathfinder - are currently available and as envisioned at the time of writing, none of the 2001 and 2003 landers' payloads include entry phase measurements of pressure or temperature), perform the first in situ meteorological observations in the southern low- and mid-latitudes and provide the first simultaneous in situ multi-site observations of the local and general circulation patterns, in a variety of locations and terrains. As such, NetLander ATMIS will be the precursor of more comprehensive meteorological surface networks for future Mars exploration. © 2000 Elsevier Science Ltd. All rights reserved.
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The atmosphere of Mars

JBIS - Journal of the British Interplanetary Society 52:5-6 (1999) 209-216

Authors:

PGJ Irwin, SB Calcutt, FW Taylor, DJ McCleese

Abstract:

Mars, one of the most Earth-like of the planets, is today a cold, dry and barren world. However, there is good evidence that it may have been much warmer and wetter in the past and perhaps even supported life. The public interest aroused by these findings and by recent studies of 'SNC' meteorites, believed to have come from Mars, with their claims of the evidence of ancient Martian life, has focused attention on the ambitious programme of Mars Exploration currently being undertaken by NASA and ESA and has provided additional impetus. Improved measurements of the conditions on Mars' surface and in its atmosphere are central to both agencies' plans, and current atmospheric missions are reviewed in this paper together with possible future designs.

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