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EuroPlanet, Sept. 22, 2006Stas Barabash, Page 1 ENA diagnostics of the solar wind interaction with planetary bodies Stas Barabash Swedish Institute of
EuroPlanet, Sept. 22, 2006Stas Barabash, Page 1 ENA diagnostics of the solar wind interaction with planetary bodies Stas Barabash Swedish Institute of
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Plasma layers in the terrestrial, martian and venusian ionospheres: Their origins and physical characteristics Martin Patzold (University of Cologne) and
Plasma layers in the terrestrial, martian and venusian ionospheres: Their origins and physical characteristics Martin Patzold (University of Cologne) and
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Simon Van Gorp 1/x Thesis defense 28 th of February, 2011 Search for physics beyond the standard electroweak model with the WITCH experiment Simon Van
Simon Van Gorp 1/x Thesis defense 28 th of February, 2011 Search for physics beyond the standard electroweak model with the WITCH experiment Simon Van
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Roberta Sparvoli, Sif 2001 - Milano La missione NINA: misure di raggi cosmici di bassa energia in orbita terrestre Roberta Sparvoli per la Collaborazione
Roberta Sparvoli, Sif 2001 - Milano La missione NINA: misure di raggi cosmici di bassa energia in orbita terrestre Roberta Sparvoli per la Collaborazione
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Langmuir’s Paradox: Can Ion instability at sheath-edge thermalize the ions too? Chi-Shung Yip Noah Hershkowitz University of Wisconsin – Madison Greg Severn
Langmuir’s Paradox: Can Ion instability at sheath-edge thermalize the ions too? Chi-Shung Yip Noah Hershkowitz University of Wisconsin – Madison Greg Severn
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The Ionization of the Local Interstellar Cloud Jonathan Slavin Harvard-Smithsonian Center for Astrophysics
The Ionization of the Local Interstellar Cloud Jonathan Slavin Harvard-Smithsonian Center for Astrophysics
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Observational Constraints on the Interplanetary Hydrogen (IPH) Flow and the Hydrogen Wall John T. Clarke Boston University Boston University NESSC meeting
Observational Constraints on the Interplanetary Hydrogen (IPH) Flow and the Hydrogen Wall John T. Clarke Boston University Boston University NESSC meeting
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1 ESS200C Planetary Ionospheres Lecture 16. 2 Interactions with the Moon The Moon has no significant atmosphere and no ionosphere. The lunar crust is
1 ESS200C Planetary Ionospheres Lecture 16. 2 Interactions with the Moon The Moon has no significant atmosphere and no ionosphere. The lunar crust is
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Frictional Cooling MC Collaboration Meeting June 11-12/2003 Raphael Galea
Frictional Cooling MC Collaboration Meeting June 11-12/2003 Raphael Galea
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Frictional Cooling NUFACT03 5-11 June, 2003 Studies at Columbia University/Nevis Labs Raphael Galea, Allen Caldwell + Stefan Schlenstedt (DESY/Zeuthen)
Frictional Cooling NUFACT03 5-11 June, 2003 Studies at Columbia University/Nevis Labs Raphael Galea, Allen Caldwell + Stefan Schlenstedt (DESY/Zeuthen)
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Fenn 1998 (Science) Electropspray
Fenn 1998 (Science) Electropspray
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ESS 200C Lecture 18. An isolated substorm is caused by a brief (30-60 min) pulse of southward IMF. Magnetospheric storms are large, prolonged disturbances
ESS 200C Lecture 18. An isolated substorm is caused by a brief (30-60 min) pulse of southward IMF. Magnetospheric storms are large, prolonged disturbances
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