Long term evolution and chaotic diffusion of the insolation quantities of Mars

被引:710
作者
Laskar, J
Correia, ACM
Gastineau, M
Joutel, F
Levrard, B
Robutel, P
机构
[1] CNRS, UMR8028, IMCCE, F-75014 Paris, France
[2] Observ Geneva, CH-1290 Sauverny, Switzerland
[3] Univ Aveiro, Dept Fis, P-3810193 Aveiro, Portugal
关键词
Mars; climate; rotational dynamics; resonances; planetary dynamics;
D O I
10.1016/j.icarus.2004.04.005
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
As the obliquity of Mars is strongly chaotic, it is not possible to give a solution for its evolution over more than a few million years. Using the most recent data for the rotational state of Mars, and a new numerical integration of the Solar System, we provide here a precise solution for the evolution of Mars' spin over 10 to 20 Myr. Over 250 Myr, we present a statistical study of its possible evolution, when considering the uncertainties in the present rotational state. Over much longer time span, reaching 5 Gyr, chaotic diffusion prevails, and we have performed an extensive statistical analysis of the orbital and rotational evolution of Mars, relying on Laskar's secular solution of the Solar System, based on more than 600 orbital and 200,000 obliquity solutions over 5 Gyr. The density functions of the eccentricity and obliquity are specified with simple analytical formulas. We found an averaged eccentricity of Mars over 5 Gyr of 0.0690 with standard deviation 0.0299, while the averaged value of the obliquity is 37.62degrees with a standard deviation of 13.82degrees, and a maximal value of 82.035degrees. We find that the probability for Mars' obliquity to have reached more than 60degrees in the past 1 Gyr is 63.0%, and 89.3% in 3 Gyr. Over 4 Gyr, the position of Mars' axis is given by a uniform distribution on a spherical cap limited by the obliquity 58.62degrees, with the addition of a random noise allowing a slow diffusion beyond this limit. We can also define a standard model of Mars' insolation parameters over 4 Gyr with the most probable values 0.068 for the eccentricity and 41.80degrees for the obliquity. (C) 2004 Elsevier Inc. All rights reserved.
引用
收藏
页码:343 / 364
页数:22
相关论文
共 80 条
  • [11] Long-term evolution of the spin of Venus I. Theory
    Correia, ACM
    Laskar, J
    de Surgy, OM
    [J]. ICARUS, 2003, 163 (01) : 1 - 23
  • [12] Costard F, 2002, SCIENCE, V295, P110, DOI [10.1126/science.1066698, 10.1126/science.1064419]
  • [13] deSurgy ON, 1997, ASTRON ASTROPHYS, V318, P975
  • [14] QUASI-PERIODIC ATMOSPHERE-REGOLITH-CAP CO2 REDISTRIBUTION IN THE MARTIAN PAST
    FANALE, FP
    SALVAIL, JR
    [J]. ICARUS, 1994, 111 (02) : 305 - 316
  • [15] Interior structure and seasonal mass redistribution of Mars from radio tracking of Mars Pathfinder
    Folkner, WM
    Yoder, CF
    Yuan, DN
    Standish, EM
    Preston, RA
    [J]. SCIENCE, 1997, 278 (5344) : 1749 - 1752
  • [16] A NUMERICAL-SIMULATION OF CLIMATE CHANGES DURING THE OBLIQUITY CYCLE ON MARS
    FRANCOIS, LM
    WALKER, JCG
    KUHN, WR
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1990, 95 (B9): : 14761 - 14778
  • [17] GANS RF, 1972, J GEOPHYS RES, V77, P360, DOI 10.1029/JB077i002p00360
  • [18] INCLINATION OF SATELLITE ORBITS ABOUT AN OBLATE PRECESSING PLANET
    GOLDREICH, P
    [J]. ASTRONOMICAL JOURNAL, 1965, 70 (01) : 5 - +
  • [19] Grimmett G., 2001, Probability and random processes
  • [20] HABERLE RM, 2000, P LUN PLAN SCI C 31