Empirical 3D basis for the internal density of a planet
Autor: | Frédéric Chambat, Yanick Ricard |
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Přispěvatelé: | Laboratoire de Sciences de la Terre (LST), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-École normale supérieure - Lyon (ENS Lyon), Laboratoire Sciences De La Terre, Umr5570, École normale supérieure de Lyon (ENS de Lyon)-Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) |
Jazyk: | angličtina |
Rok vydání: | 2005 |
Předmět: |
010504 meteorology & atmospheric sciences
[PHYS.PHYS.PHYS-GEO-PH] Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] [SDE.MCG]Environmental Sciences/Global Changes Inverse [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] 010502 geochemistry & geophysics 01 natural sciences [SDE.MCG] Environmental Sciences/Global Changes Geophysics Classical mechanics Gravitational field Geochemistry and Petrology Planet Seismic tomography Norm (mathematics) Geoid [SDU.STU.GP] Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph] Statistical physics 0105 earth and related environmental sciences Mathematics |
Zdroj: | Geophysical Journal International Geophysical Journal International, Oxford University Press (OUP), 2005, 162, pp.32-35 HAL Geophysical Journal International, 2005, 162, pp.32-35 |
ISSN: | 0956-540X 1365-246X |
Popis: | International audience; Various papers have discussed the forward relationships between internal density anomalies of a planet and its external gravity field. The inverse modeling, i.e. finding the internal density anomalies from the external potential is known to be highly non unique. In this research note, we explain how a 3D basis can be built to represent the internal density variations which includes a subset that explicitly spans the kernel of the forward gravity operator. This representation clarifies the origin of the non-uniqueness of the gravity sources and implies the existence of a natural minimal-norm inverse for the internal density. We illustrate these ideas by comparing a tomographic model of the mantle to the minimal norm density. |
Databáze: | OpenAIRE |
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