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Dive into the research topics where Timothy S. Olson is active.

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Featured researches published by Timothy S. Olson.


Journal of Geophysical Research | 2013

MAHLI at the Rocknest sand shadow: Science and science-enabling activities

M. E. Minitti; L. C. Kah; R. A. Yingst; Kenneth S. Edgett; Robert C. Anderson; L. W. Beegle; Joseph Carsten; Robert G. Deen; W. Goetz; Craig Hardgrove; D. E. Harker; K. E. Herkenhoff; Joel A. Hurowitz; L. Jandura; Megan R. Kennedy; Gary Kocurek; Gillian M. Krezoski; S. R. Kuhn; D. Limonadi; Leslie J. Lipkaman; M. B. Madsen; Timothy S. Olson; Matthew Robinson; Scott K. Rowland; David M. Rubin; C. Seybold; Juergen Schieber; Mariek E. Schmidt; Dawn Y. Sumner; V. V. Tompkins

[1]xa0During Martian solar days 57–100, the Mars Science Laboratory Curiosity rover acquired and processed a solid (sediment) sample and analyzed its mineralogy and geochemistry with the Chemistry and Mineralogy and Sample Analysis at Mars instruments. An aeolian deposit—herein referred to as the Rocknest sand shadow—was inferred to represent a global average soil composition and selected for study to facilitate integration of analytical results with observations from earlier missions. During first-time activities, the Mars Hand Lens Imager (MAHLI) was used to support both science and engineering activities related to sample assessment, collection, and delivery. Here we report on MAHLI activities that directly supported sample analysis and provide MAHLI observations regarding the grain-scale characteristics of the Rocknest sand shadow. MAHLI imaging confirms that the Rocknest sand shadow is one of a family of bimodal aeolian accumulations on Mars—similar to the coarse-grained ripples interrogated by the Mars Exploration Rovers Spirit and Opportunity—in which a surface veneer of coarse-grained sediment stabilizes predominantly fine-grained sediment of the deposit interior. The similarity in grain size distribution of these geographically disparate deposits support the widespread occurrence of bimodal aeolian transport on Mars. We suggest that preservation of bimodal aeolian deposits may be characteristic of regions of active deflation, where winnowing of the fine-sediment fraction results in a relatively low sediment load and a preferential increase in the coarse-grained fraction of the sediment load. The compositional similarity of Martian aeolian deposits supports the potential for global redistribution of fine-grained components, combined with potential local contributions.


Earth and Space Science | 2017

The Mars Science Laboratory (MSL) Mast cameras and Descent imager: Investigation and instrument descriptions

Michael C. Malin; Michael A. Ravine; Michael A. Caplinger; F. Tony Ghaemi; J. A. Schaffner; J. N. Maki; James F. Bell; James F. Cameron; William E. Dietrich; Kenneth S. Edgett; Laurence J. Edwards; James B. Garvin; Bernard Hallet; Kenneth E. Herkenhoff; Ezat Heydari; Linda C. Kah; Mark T. Lemmon; M. E. Minitti; Timothy S. Olson; Timothy J. Parker; Scott K. Rowland; Juergen Schieber; Ron Sletten; Robert J. Sullivan; Dawn Y. Sumner; R. Aileen Yingst; Brian M. Duston; Sean McNair; Elsa Jensen

Abstract The Mars Science Laboratory Mast camera and Descent Imager investigations were designed, built, and operated by Malin Space Science Systems of San Diego, CA. They share common electronics and focal plane designs but have different optics. There are two Mastcams of dissimilar focal length. The Mastcam‐34 has an f/8, 34 mm focal length lens, and the M‐100 an f/10, 100 mm focal length lens. The M‐34 field of view is about 20° × 15° with an instantaneous field of view (IFOV) of 218 μrad; the M‐100 field of view (FOV) is 6.8° × 5.1° with an IFOV of 74 μrad. The M‐34 can focus from 0.5 m to infinity, and the M‐100 from ~1.6 m to infinity. All three cameras can acquire color images through a Bayer color filter array, and the Mastcams can also acquire images through seven science filters. Images are ≤1600 pixels wide by 1200 pixels tall. The Mastcams, mounted on the ~2 m tall Remote Sensing Mast, have a 360° azimuth and ~180° elevation field of regard. Mars Descent Imager is fixed‐mounted to the bottom left front side of the rover at ~66 cm above the surface. Its fixed focus lens is in focus from ~2 m to infinity, but out of focus at 66 cm. The f/3 lens has a FOV of ~70° by 52° across and along the direction of motion, with an IFOV of 0.76 mrad. All cameras can acquire video at 4 frames/second for full frames or 720p HD at 6 fps. Images can be processed using lossy Joint Photographic Experts Group and predictive lossless compression.


Physical Review C | 2000

Maximally incompressible neutron star matter

Timothy S. Olson

Relativistic kinetic theory, based on the Grad method of moments as developed by Israel and Stewart, is used to model viscous and thermal dissipation in neutron star matter and determine an upper limit on the maximum mass of neutron stars. In the context of kinetic theory, the equation of state must satisfy a set of constraints in order for the equilibrium states of the fluid to be thermodynamically stable and for perturbations from equilibrium to propagate causally via hyperbolic equations. Application of these constraints to neutron star matter restricts the stiffness of the most incompressible equation of state compatible with causality to be softer than the maximally incompressible equation of state that results from requiring the adiabatic sound speed to not exceed the speed of light. Using three equations of state based on experimental nucleon-nucleon scattering data and properties of light nuclei up to twice normal nuclear energy density, and the kinetic theory maximally incompressible equation of state at higher density, an upper limit on the maximum mass of neutron stars averaging 2.64 solar masses is derived.


Space Science Reviews | 2012

Curiosity's Mars Hand Lens Imager (MAHLI) investigation

Kenneth S. Edgett; R. Aileen Yingst; Michael A. Ravine; Michael A. Caplinger; J. N. Maki; F. Tony Ghaemi; J. A. Schaffner; James F. Bell; Laurence J. Edwards; Kenneth E. Herkenhoff; Ezat Heydari; Linda C. Kah; Mark T. Lemmon; M. E. Minitti; Timothy S. Olson; Timothy J. Parker; Scott K. Rowland; Juergen Schieber; Robert J. Sullivan; Dawn Y. Sumner; Peter C. Thomas; Elsa Jensen; John J. Simmonds; Aaron J. Sengstacken; Reg G. Willson; W. Goetz


Archive | 2010

The Mars Science Laboratory (MSL) Mast-mounted Cameras (Mastcams) Flight Instruments

Michael C. Malin; Michael A. Caplinger; Kenneth S. Edgett; F. T. Ghaemi; Michael A. Ravine; J. A. Schaffner; Jennifer Baker; Jason Dante Bardis; Dan Dibiase; J. N. Maki; Reg G. Willson; James F. Bell; William E. Dietrich; Laurence J. Edwards; Bernard Hallet; Kenneth E. Herkenhoff; Ezat Heydari; Linda C. Kah; Mark T. Lemmon; M. E. Minitti; Timothy S. Olson; Timothy J. Parker; Scott K. Rowland; Juergen Schieber; R. Sullivan; Dawn Y. Sumner; Peter C. Thomas; Robin Aileen Yingst


Archive | 2009

The Mars Science Laboratory (MSL) Mars Hand Lens Imager (MAHLI) Flight Instrument

Kenneth S. Edgett; Michael A. Ravine; Michael A. Caplinger; F. T. Ghaemi; J. A. Schaffner; Michael C. Malin; Jennifer Baker; Dan Dibiase; J. Laramee; J. N. Maki; Reg G. Willson; James F. Bell; James F. Cameron; William E. Dietrich; Laurence J. Edwards; Bernard Hallet; Kenneth E. Herkenhoff; Ezat Heydari; Linda C. Kah; Mark T. Lemmon; M. E. Minitti; Timothy S. Olson; Timothy Jay Parker; Scott K. Rowland; Juergen Schieber; R. Sullivan; Dawn Y. Sumner; Peter C. Thomas; Robin Aileen Yingst


Physical Review C | 1989

Relativistic dissipative hydrodynamics and the nuclear equation of state

Timothy S. Olson; William A. Hiscock


Archive | 2009

The Mars Science Laboratory (MSL) Mars Descent Imager (MARDI) Flight Instrument

Michael C. Malin; Michael A. Caplinger; Kenneth S. Edgett; F. T. Ghaemi; Michael A. Ravine; J. A. Schaffner; J. N. Maki; Reg G. Willson; James F. Bell; James F. Cameron; William E. Dietrich; Laurence J. Edwards; Bernard Hallet; Kenneth E. Herkenhoff; Ezat Heydari; Linda C. Kah; Mark T. Lemmon; M. E. Minitti; Timothy S. Olson; Timothy Jay Parker; Scott K. Rowland; Juergen Schieber; R. Sullivan; Dawn Y. Sumner; Peter C. Thomas; Robin Aileen Yingst


Advances in Space Research | 2016

Transient atmospheric effects of the landing of the Mars Science Laboratory rover: The emission and dissipation of dust and carbazic acid

John E. Moores; Juergen Schieber; Alexandre M. Kling; Robert M. Haberle; Casey A. Moore; Mark S. Anderson; Ira Katz; Andre Yavrouian; Michael C. Malin; Timothy S. Olson; Scot C. Randell Rafkin; Mark T. Lemmon; Robert J. Sullivan; Keith Comeaux; Ashwin R. Vasavada


Journal of Geophysical Research | 2013

MAHLI at the Rocknest sand shadow: Science and science-enabling activities: MAHLI AT ROCKNEST

M. E. Minitti; L. C. Kah; R. A. Yingst; Kenneth S. Edgett; Robert C. Anderson; Luther W. Beegle; Joseph Carsten; Robert G. Deen; W. Goetz; Craig Hardgrove; David Emerson Harker; K. E. Herkenhoff; Joel A. Hurowitz; L. Jandura; Megan R. Kennedy; Gary Kocurek; Gillian M. Krezoski; S. R. Kuhn; D. Limonadi; Leslie J. Lipkaman; M. B. Madsen; Timothy S. Olson; Matthew Robinson; Scott K. Rowland; David M. Rubin; C. Seybold; Juergen Schieber; Mariek E. Schmidt; Dawn Y. Sumner; V. V. Tompkins

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Juergen Schieber

Indiana University Bloomington

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Dawn Y. Sumner

University of California

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M. E. Minitti

Planetary Science Institute

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Ezat Heydari

Jackson State University

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J. N. Maki

Jet Propulsion Laboratory

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James F. Bell

Arizona State University

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Kenneth E. Herkenhoff

United States Geological Survey

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