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Luisa Lara

Researcher at Spanish National Research Council

Publications -  125
Citations -  7778

Luisa Lara is an academic researcher from Spanish National Research Council. The author has contributed to research in topics: Comet & Comet dust. The author has an hindex of 45, co-authored 121 publications receiving 6835 citations. Previous affiliations of Luisa Lara include European Space Agency.

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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.
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Vertical distribution of Titan's atmospheric neutral constituents

TL;DR: The vertical distribution of Titan's neutral atmosphere compounds is calculated from a new photochemical model extending from 40 to 1432 km as mentioned in this paper, which makes use of many updated reaction rates, and of the new scheme for methane photolysis proposed by Mordaunt et al.