Present-day mass wasting of the north polar ice cap on Mars

Mars is a dynamic planet, exhibiting diverse active processes across its surface. Driven by variations in the obliquity of the rotation axis and the eccentricity of the orbit, the surface of Mars has experienced successive episodes of deposition and removal of water ice. At the end of the last ice a...

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Bibliographic Details
Main Author: Su, Shu
Other Authors: Oberst, Jürgen, Technische Universität Berlin, Hiesinger, Harald, Portyankina, Ganna
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: 2024
Subjects:
Online Access:https://depositonce.tu-berlin.de/handle/11303/22120
https://doi.org/10.14279/depositonce-20921
Description
Summary:Mars is a dynamic planet, exhibiting diverse active processes across its surface. Driven by variations in the obliquity of the rotation axis and the eccentricity of the orbit, the surface of Mars has experienced successive episodes of deposition and removal of water ice. At the end of the last ice age, about 0.4 Myr ago, water ice has finally deposited at the two poles, at the expense of loss from the mid-latitudes. Since then, these polar ice deposits have been undergoing reworking with erosion and retreat in response to climate change. In particular, at the north polar ice cap, prevalent surface changes, such as avalanches and ice block falls, have been observed from high-resolution satellite images. Ice block falls are likely the most active erosional process that are consistently affecting the topography of the north polar ice cap. Although avalanches are also prevailing, they are thought to carry mostly CO2 ice and dust. Research on how ice block falls have been shaping the north polar ice cap, are limited and incomplete. Therefore, in this work, I will address this interesting and significant task. The main efforts of this thesis are as follows. 1). I have designed a pipeline to process the High Resolution Imaging Science Experiment (HiRISE) raw images, generate HiRISE Digital Terrain Models (DTMs), and carry out orthorectification, by using the Ames Stereo Pipeline software. The produced DTMs generally conform to the criteria for orthorectifying raw images. This pipeline is crucial for this work as the orthorectified HiRISE images are essential for monitoring meter-scale changes at the north polar region through time. 2). I have proposed a solution to search for the sources of ice block falls at the marginal steep scarps of the North Polar Layered Deposits (NPLD). The idea is to identify the shadows of the detached ice-fragments, because the changes in shadow patterns can attest to ice block fall events. An automated intensity-based change detection method has been developed, and successfully applied to ...