大学院教育 Dynamics of ice sheets and glaciers (2010)
Ice sheets and glaciers are an active, dynamic part of the Earth’s climate system on time-scales of decades and more. More than 90% of the terrestrial freshwater reserves are stored in these ice masses. Their complete disintegration would lead to a global sea-level rise of approximately 70 meters and would have severe impacts on the atmospheric and oceanic circulation. Against the background of future global climate warming due to ongoing emissions of greenhouse gases, understanding the behaviour of these ice bodies is of great relevance. In this lecture, based on the general framework of continuum-mechanical balance equations, the dynamics and thermodynamics of ice sheets (including attached ice shelves) and glaciers will be treated.
<The main theme of the lecture>
Based on the general framework of continuum-mechanical balance equations, the dynamics and thermodynamics of ice sheets, ice shelves and glaciers will be treated.
<Concise outline of lecture, activity plan etc>
2. Elements of continuum mechanics
3. Constitutive equations for polycrystalline ice
4. Large-scale dynamics of ice sheets
5. Large-scale dynamics of ice shelves
6. Dynamics of glacier flow
7. Glacial isostasy
<How to assess the class>
Class attendance, quizzes
Greve, R. and H. Blatter, 2009, “Dynamics of ice sheets and glaciers”. Springer, Berlin, Germany etc., 287 pp. ISBN: 978-3-642-03414-5.
<Message, attention points and prerequisites for taking lecture etc>
The lecture will be held in English. Prerequisites: Bachelor degree in Science or Engineering or equivalent qualification, some level of comfort in calculus and linear algebra, good skills in oral and written English. Doctor-course students are also welcome.