D. T. Young
Current Organizations / Institutes
The organizations/institutes from the scholar's latest article
Previous Organizations / Institutes
The organizations / institutes from the scholar's other articles in the past ten years
Research Subjects
D. T. Young has a total of 131 co-authors. Here are the top co-authors by number of shared publications:
- David John McComas
Princeton University
5 shared publications J. E. Nordholt
Los Alamos National Laboratory, Los Alamos, NM
5 shared publicationsR. Goldstein
Jet Propulsion Laboratory, Pasadena, CA
4 shared publications- Andrew J. Coates
University College London
3 shared publications D. Reisenfeld
Department of Physics and Astronomy; University of Montana; Missoula Montana USA
3 shared publications- Herbert O. Funsten
Los Alamos National Laboratory
3 shared publications
Latest Publications
- Top Cited PapersOpen Access
- 24 December 2014
- Published by Springer Nature in Space Science Reviews
- Vol. 199 (1-4) , 407-470
Hot Plasma Composition Analyzer for the Magnetospheric Multiscale Mission
- 24 December 2014
- Published by Springer Nature in Space Science Reviews
- Vol. 199 (1-4) , 407-470
Top Cited PapersOpen AccessHot Plasma Composition Analyzer for the Magnetospheric Multiscale Mission
- 19 March 2013
- Published by Wiley
- p. 393-396
The Comet/Solar Wind Transition Region at Giacobini-Zinner
- 18 March 2013
- Published by Wiley in Geophysical Monograph Series
- Vol. 54, 171-176
A 360° Field-of-View Toroidal Ion Composition Analyzer Using Time-of-Flight
- 18 March 2013
- Published by Wiley in Geophysical Monograph Series
- Vol. 54, 171-176
A 360° Field-of-View Toroidal Ion Composition Analyzer Using Time-of-Flight
- 18 March 2013
- Published by Wiley in Geophysical Monograph Series
- Vol. 54, 143-157
Space Plasma Mass Spectroscopy Below 60 Kev
- 18 March 2013
- Published by Wiley in Geophysical Monograph Series
- Vol. 54, 143-157
Space Plasma Mass Spectroscopy Below 60 Kev
- Open Access
- 18 March 2013
- Published by Wiley
- p. 209-214
The Cassini Ion Mass Spectrometer: Performance Metrics and Techniques
- 18 March 2013
- Published by Wiley
- p. 209-214
Open AccessThe Cassini Ion Mass Spectrometer: Performance Metrics and Techniques
- Open Access
- 23 July 2011
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 116 (A7)
Cassini Plasma Spectrometer and hybrid model study on Titan's interaction: Effect of oxygen ions
- 23 July 2011
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 116 (A7)
Open AccessCassini Plasma Spectrometer and hybrid model study on Titan's interaction: Effect of oxygen ions
- 1 April 2007
- Published by Springer Nature in Space Science Reviews
- Vol. 129 (4) , 327-357
Plasma Experiment for Planetary Exploration (PEPE)
- 1 April 2007
- Published by Springer Nature in Space Science Reviews
- Vol. 129 (4) , 327-357
Plasma Experiment for Planetary Exploration (PEPE)
- 25 February 2005
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 307 (5713) , 1262-1266
Composition and Dynamics of Plasma in Saturn's Magnetosphere
During Cassini's initial orbit, we observed a dynamic magnetosphere composed primarily of a complex mixture of water-derived atomic and molecular ions. We have identified four distinct regions characterized by differences in both bulk plasma properties and ion composition. Protons are the dominant species outside about 9 R S (where R S is the radial distance from the center of Saturn), whereas inside, the plasma consists primarily of a corotating comet-like mix of water-derived ions with ∼3% N + . Over the A and B rings, we found an ionosphere in which O 2 + and O + are dominant, which suggests the possible existence of a layer of O 2 gas similar to the atmospheres of Europa and Ganymede.
- 25 February 2005
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 307 (5713) , 1262-1266
Composition and Dynamics of Plasma in Saturn's Magnetosphere
During Cassini's initial orbit, we observed a dynamic magnetosphere composed primarily of a complex mixture of water-derived atomic and molecular ions. We have identified four distinct regions characterized by differences in both bulk plasma properties and ion composition. Protons are the dominant species outside about 9 R S (where R S is the radial distance from the center of Saturn), whereas inside, the plasma consists primarily of a corotating comet-like mix of water-derived ions with ∼3% N + . Over the A and B rings, we found an ionosphere in which O 2 + and O + are dominant, which suggests the possible existence of a layer of O 2 gas similar to the atmospheres of Europa and Ganymede.