Recent formation and evolution of northern Martian polar layered deposits as inferred from a Global Climate Model

Benjamin Levrard 1, 2 Francois Forget 3 Franck Montmessin 4 Jacques Laskar 1
1 IMCCE - Institut de Mécanique Céleste et de Calcul des Ephémérides
2 CRAL - Centre de Recherche Astrophysique de Lyon
3 LMD - Laboratoire de Météorologie Dynamique (UMR 8539)
4 SA - Service d'aéronomie
Abstract : We present a time-marching model which simulates the exchange of water ice between the Martian northern cap, the tropics and a high-latitude surface reservoir. Net annual exchange rates of water and their sensitivity to variations in orbital/rotational parameters are examined using the Martian water cycle modeled by the LMD 3-D Global Climate Model. These rates are propagated over the last 10 Myr to follow the thickness of the reservoirs. The effect of a sublimation dust lag is taken account to test simple models of layer formation. Periods of high mean polar summer insolation ($\sim$ 5-10 Ma ago) lead to a rapid exhaustion of a northern polar cap and a prolonged formation of tropical glaciers. The formation of a northern cap and of a high-latitude icy mantle may have started 4 Ma ago with the average decrease of polar insolation. Tropical ice may have disappeared around 2.7 Ma ago, but small glaciers could have formed during the last peaks of polar summer insolation. Over the last 4 Myr, most of the present cap may have formed at the expense of tropical and high-latitude reservoirs forming distinct layers at almost each $\sim$ 51-kyr/120-kyr insolation cycle. Layers thickness ranges from 10 to 80 meters, variations being produced by the modulation of the obliquity with $\sim$ 2.4 and 1.3 Myr periods. Because only $\sim$ 30 insolation cycles have occured since 4 Ma ago, we found an inconsistency between the recent astronomical forcing, the observed number of layers and simple astronomically-based scenarios of layers formation.
Keywords : Mars Paleoclimatology Rotational and orbital dynamics Polar caps
Type de document :
Article dans une revue
Journal of Geophysical Research. Planets, Wiley-Blackwell, 2007, 112 (E06012), pp.1-18. 〈10.1029/2006JE002772〉
Liste complète des métadonnées
https://hal-ens-lyon.archives-ouvertes.fr/ensl-00158333
Contributeur : Benjamin Levrard <>
Soumis le : jeudi 28 juin 2007 - 15:28:42
Dernière modification le : mercredi 19 septembre 2018 - 01:19:59
Document(s) archivé(s) le : lundi 27 juin 2011 - 16:36:37

Fichiers

JGR_levrard_2007.pdf
Fichiers éditeurs autorisés sur une archive ouverte

Identifiants

Collections

ENS-PARIS | OBSPM | IMCCE | INSU | ENS-LYON | ENPC-LMD | ENPC | CRAL | X | X-LMD | PARISTECH | X-DEP-MECA | UPMC | LMD | UVSQ | PSL | AERONOMIE | UNIV-LYON1

Citation

Benjamin Levrard, Francois Forget, Franck Montmessin, Jacques Laskar. Recent formation and evolution of northern Martian polar layered deposits as inferred from a Global Climate Model. Journal of Geophysical Research. Planets, Wiley-Blackwell, 2007, 112 (E06012), pp.1-18. 〈10.1029/2006JE002772〉. 〈ensl-00158333〉

Exporter

BibTeX TEI DC DCterms EndNote

Partager

Métriques

Consultations de la notice

478

Téléchargements de fichiers

172

Contact

support.ccsd.cnrs.fr
hal.support@ccsd.cnrs.fr
Logo CCSD