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Stefano Debei

Researcher at University of Padua

Publications -  290
Citations -  10185

Stefano Debei is an academic researcher from University of Padua. The author has contributed to research in topics: Comet & Field of view. The author has an hindex of 47, co-authored 286 publications receiving 8851 citations. Previous affiliations of Stefano Debei include University of Trento.

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In situ measurements of the physical characteristics of Titan's environment

TL;DR: The temperature and density profiles, as determined by the Huygens Atmospheric Structure Instrument (HASI), from an altitude of 1,400 km down to the surface were higher than expected and the extent of atmospheric electricity was also hitherto unknown.
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On the nucleus structure and activity of comet 67P/Churyumov-Gerasimenko

Holger Sierks, +70 more
- 23 Jan 2015 - 
TL;DR: Images from the OSIRIS scientific imaging system onboard Rosetta show that the nucleus of 67P/Churyumov-Gerasimenko consists of two lobes connected by a short neck, which raises the question of whether the two Lobes represent a contact binary formed 4.5 billion years ago, or a single body where a gap has evolved via mass loss.
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Dust measurements in the coma of comet 67P/Churyumov-Gerasimenko inbound to the Sun

Alessandra Rotundi, +90 more
- 23 Jan 2015 - 
TL;DR: In this article, the GIADA (Grain Impact Analyser and Dust Accumulator) experiment on the European Space Agency's Rosetta spacecraft orbiting comet 67P/Churyumov-Gerasimenko was used to detect 35 outflowing grains of mass 10−10 to 10−7 kilograms.
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OSIRIS – The Scientific Camera System Onboard Rosetta

TL;DR: The Optical, Spectroscopic, and Infrared Remote Imaging System (OSIRIS) as discussed by the authors is the scientific camera system onboard the Rosetta spacecraft, which consists of a high resolution Narrow Angle Camera (NAC) and a wide angle Camera (WAC) units accompanied by three electronics boxes.
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The morphological diversity of comet 67P/Churyumov-Gerasimenko

TL;DR: Images of comet 67P/Churyumov-Gerasimenko acquired by the OSIRIS imaging system onboard the European Space Agency’s Rosetta spacecraft offer some support for subsurface fluidization models and mass loss through the ejection of large chunks of material.