A survey of small-scale (<50 m) surface features on the Martian north polar cap using HiRISE

被引:5
作者
Giang Nguyen, T. [1 ]
Radebaugh, Jani [2 ]
Innanen, Alex C. [1 ]
Moores, John E. [1 ]
机构
[1] York Univ, Ctr Res Earth & Space Sci, 4700 Keele St, Keele, ON M3J 1P3, Canada
[2] Brigham Young Univ, Dept Geol Sci, S-389 ESC, Provo, UT 84602 USA
基金
加拿大自然科学与工程研究理事会;
关键词
Mars; North polar cap; Aeolian; Sublimation; TRANSVERSE AEOLIAN RIDGES; MARS; DUNES; MIGRATION; TRANSPORT; RIPPLES; WINDS;
D O I
10.1016/j.pss.2019.104809
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
The surface of the Martian north polar cap hosts a wide array of small scale (<50m) features that are uniform in spacing and orientation. By analysing the spacing, orientation, and morphology of these features, we explore possible processes that can form these regular patterns. Using data from the High Resolution Imaging Scientific Experiment (HiRISE), features less than 50 m are characterized and mapped over the entirety of the northern polar cap. A 2D Fast Fourier Transform is used to measure general spacing and orientation tendencies of surface patterns. Of the 559 observations of features found on the cap, we found 248 features that display uniformity in orientation and spacing, which could be consistent with either aeolian-driven or sublimation-driven features. The orientation of smaller features (<10 m) located at the edge of the cap from 40 degrees E - 80 degrees E significantly align with local winds suggesting that they may be aeolian bedforms. We found no features on the cap that matches the properties of modelled sublimation-driven penitentes.
引用
收藏
页数:9
相关论文
共 36 条
[1]   Transverse Aeolian Ridges (TARs) on Mars [J].
Balme, Matt ;
Berman, Daniel C. ;
Bourke, Mary C. ;
Zimbelman, James R. .
GEOMORPHOLOGY, 2008, 101 (04) :703-720
[2]   VARIATIONS IN EFFECTIVE ELASTIC THICKNESS OF THE NORTH-AMERICAN LITHOSPHERE [J].
BECHTEL, TD ;
FORSYTH, DW ;
SHARPTON, VL ;
GRIEVE, RAF .
NATURE, 1990, 343 (6259) :636-638
[3]   Bedform migration on Mars: Current results and future plans [J].
Bridges, Nathan ;
Geissler, Paul ;
Silvestro, Simone ;
Banks, Maria .
AEOLIAN RESEARCH, 2013, 9 :133-151
[4]   The Mars Science Laboratory (MSL) Bagnold Dunes Campaign, Phase I: Overview and introduction to the special issue [J].
Bridges, Nathan T. ;
Ehlmann, Bethany L. .
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS, 2018, 123 (01) :3-19
[5]   Intra-surface radiative transfer limits the geographic extent of snow penitents on horizontal snowfields [J].
Cathles, L. Maclagan ;
Abbot, Dorian S. ;
MacAyeal, Douglas R. .
JOURNAL OF GLACIOLOGY, 2014, 60 (219) :147-154
[6]   Physical processes causing the formation of penitentes [J].
Claudin, P. ;
Jarry, H. ;
Vignoles, G. ;
Plapp, M. ;
Andreotti, B. .
PHYSICAL REVIEW E, 2015, 92 (03)
[7]   A scaling law for aeolian dunes on Mars, Venus, Earth, and for subaqueous ripples [J].
Claudin, Philippe ;
Andreotti, Bruno .
EARTH AND PLANETARY SCIENCE LETTERS, 2006, 252 (1-2) :30-44
[8]   On aeolian transport: Grain-scale interactions, dynamical mechanisms and scaling laws [J].
Duran, O. ;
Claudin, P. ;
Andreotti, B. .
AEOLIAN RESEARCH, 2011, 3 (03) :243-270
[9]   Multi-spatial analysis of aeolian dune-field patterns [J].
Ewing, Ryan C. ;
McDonald, George D. ;
Hayes, Alex G. .
GEOMORPHOLOGY, 2015, 240 :44-53
[10]   SUBLIMATION AND TRANSPORT OF WATER FROM THE NORTH RESIDUAL POLAR-CAP ON MARS [J].
HABERLE, RM ;
JAKOSKY, BM .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1990, 95 (B2) :1423-1437