Published July 28, 2011 | Version v1
Publication

The Canada-France Ecliptic Plane Survey - Full Data Release: The Orbital Structure of the Kuiper Belt

Others:
Univers, Transport, Interfaces, Nanostructures, Atmosphère et environnement, Molécules (UMR 6213) (UTINAM) ; Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC) ; Université Bourgogne Franche-Comté [COMUE] (UBFC)-Université Bourgogne Franche-Comté [COMUE] (UBFC)
Department of Physics and Astronomy [Vancouver] ; University of British Columbia (UBC)
NRC Herzberg Institute of Astrophysics ; National Research Council of Canada (NRC)
SwRI Planetary Science Directorate [Boulder] ; Southwest Research Institute [Boulder] (SwRI)
Department of Planetary Sciences [Tucson] ; University of Arizona
Cornell University [New York]
Laboratoire de Cosmologie, Astrophysique Stellaire & Solaire, de Planétologie et de Mécanique des Fluides (CASSIOPEE) ; Université Nice Sophia Antipolis (1965 - 2019) (UNS) ; COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur ; COMUE Université Côte d'Azur (2015-2019) (COMUE UCA)-Université Côte d'Azur (UCA)-Université Côte d'Azur (UCA)-Centre National de la Recherche Scientifique (CNRS)
Harvard-Smithsonian Center for Astrophysics (CfA) ; Harvard University [Cambridge]-Smithsonian Institution
Department of Physics and Astronomy [Victoria] ; University of Victoria [Canada] (UVIC)
Departamento de Fisica, Ingenieria de Sistemas y Teoria de la Señal [Alicante] (DFESTS) ; Universidad de Alicante
PICS Canada #4638
PICS Canada #4638

Description

We report the orbital distribution of the trans-neptunian objects (TNOs) discovered during the Canada-France Ecliptic Plane Survey (CFEPS), whose discovery phase ran from early 2003 until early 2007. We obtained characterized observations of 321 sq.deg. of sky to depths in the range g ~23.5 - 24.4 AB mag. We provide a database of 169 TNOs with high-precision dynamical classification and known discovery efficiency. From this, we find that the classical belt is a complex region with sub-structures that go beyond the usual splitting of inner (interior to 3:2 mean-motion resonance [MMR]), main (between 3:2 and 2:1 MMR), and outer (exterior to 2:1 MMR). The main classical belt (a=40--47~AU) needs to be modeled with at least three components: the 'hot' component with a wide inclination distribution and two 'cold' components (stirred and kernel) with much narrower inclination distributions. The hot component must have a significantly shallower absolute magnitude (Hg) distribution than the other two components. With 95% confidence, there are 8000^{+1800}_{-1600} objects in the main belt with Hg <= 8.0, of which 50% are from the hot component, 40% from the stirred component and 10% from the kernel; the hot component's fraction drops rapidly with increasing Hg. Because of this, the apparent population fractions depend on the depth and ecliptic latitude of a trans-neptunian survey.

Abstract

59 pages, including tables and figures.

Additional details

Created:
December 4, 2022
Modified:
November 30, 2023