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University of Oxford

Modelling Ice Sheets - Oxford Mathematics Research Seminar

University of Oxford via YouTube

Overview

Explore the mathematical modeling of ice sheets in Greenland and Antarctica through this Oxford Mathematics Research Seminar. Delve into the complexities of ice sheet dynamics, including their movement, fluid properties, and the equations governing their behavior. Learn about the motivation behind studying ice sheets, their impact on global climate, and the challenges in predicting their future. Discover key concepts such as accumulation elevation feedback, depth-integrated models, and surface boundary layers. Gain insights into the scale of Antarctica and the role of moulins in ice sheet dynamics. This seminar provides a comprehensive look at cutting-edge research in glaciology and climate science, offering valuable knowledge for those interested in environmental mathematics and climate modeling.

Syllabus

Introduction
Motivation
Antarctica
How Ice Sheets Work
How Ice Sheets Move
Ice as a Fluid
Ice Sheet Model
Ice Sheet Equation
Accumulation Elevation Feedback
Depth Integrated Models
How large is Antarctica
Surface boundary layer
Equations
Moulins

Taught by

Oxford Mathematics

Reviews

4.7 rating, based on 3 Class Central reviews

Start your review of Modelling Ice Sheets - Oxford Mathematics Research Seminar

  • Profile image for Wulan Octavieny
    Wulan Octavieny
    The Modelling Ice Sheets: Oxford Mathematics Research Seminar, hosted by the University of Oxford and available on their YouTube channel, is a comprehensive and engaging series of lectures that delve into the complexities of ice sheet modeling. The…
  • Raka Syaiful Rohman
    Modelling Ice Sheets seminar provided deep insights into cutting-edge research in Oxford Mathematics. Engaging discussions and innovative approaches highlighted the complexities of ice sheet dynamics
  • Tallyson Kayky
    muito bom o curso, muito bem elaborado e o professor demonstrou que tem total domínio sobre o assunto abordado no curso. ótimo

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