Greg Neumann / Ralph Lorenz / Atmosphere Science Advisory Group / Huygens Descent Trajectory Working Group / Atmospheric Advisory Group / WT Kasprzak AE / /
Continent
Europe / /
Country
United States / United Kingdom / /
Currency
pence / /
Event
Person Travel / Natural Disaster / Business Partnership / /
Facility
Open University / NASA Goddard Spaceflight Center / University of Arizona / University of Arizona Press / /
IndustryTerm
energy / neutral gas composition / large network / thermodynamic systems / /
Organization
Open University / Pioneer Venus mission / NASA Goddard Spaceflight Center / NASA’s Mars Exploration Rover mission / American Geophysical Union / MER mission / Nuclear Regulatory Commission / Science Team / National Aeronautics and Space Administration / GISS Mission / University of Arizona Press / American Astronomical Society / University of Arizona / Astronomical Society of the Pacific / /
Person
Alvin Seiff / Jay Melosh / Milton Keynes / Mars Odyssey / Niemann / ALLISON - PAGE JPL / Neutral Mass Spectrometer / John Zarnecki / David Atkinson / Chamberlain / Greg Neumann / Ion Mass Spectrometer / Mars Climate Orbiter / Steve Bougher / PAUL WITHERS / Roger Yelle / /
Position
HB / advisor / Graduate Research Assistant / Principal Investigator / Co-Investigator / Participating Scientist / RT / General / Research Assistant / Consultant to John Zarnecki / Global Surveyor / Chair / representative / surveyor / current PhD supervisor / /
Product
Beagle 2 Accelerometer / Titan / /
ProgrammingLanguage
RC / J / /
ProvinceOrState
Maryland / Arizona / /
PublishedMedium
Geophysical Research Letters / the European Mars Express / The Mars Express / Icarus / /
Winds in Planetary Atmospheres Introduction: The basic circulation of an atmosphere is defined by its pressure, temperature, and wind fields [Holton, [removed]Pressure and temperature have a direct effect on the passage of