Ice Sheets & Ice Cores:Data Analysis & Stochastic Modelling

Since the discovery of the Ice Ages it has been evident that Earth’s climate is liable to undergo dramatic changes. The previous climatic period known as the Last Glacial saw large oscillations in the extent of ice sheets covering the Northern hemisphere. Understanding these oscillations known as Da...

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Bibliographic Details
Main Author: Mikkelsen, Troels Bøgeholm
Format: Book
Language:English
Published: The Niels Bohr Institute, Faculty of Science, University of Copenhagen 2017
Subjects:
Online Access:https://curis.ku.dk/portal/da/publications/ice-sheets--ice-cores(74d12cf8-5a21-4c86-b22d-3b284c89c9f6).html
https://soeg.kb.dk/permalink/45KBDK_KGL/fbp0ps/alma99122333826705763
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spelling ftcopenhagenunip:oai:pure.atira.dk:publications/74d12cf8-5a21-4c86-b22d-3b284c89c9f6 2023-05-15T14:02:44+02:00 Ice Sheets & Ice Cores:Data Analysis & Stochastic Modelling Mikkelsen, Troels Bøgeholm 2017 https://curis.ku.dk/portal/da/publications/ice-sheets--ice-cores(74d12cf8-5a21-4c86-b22d-3b284c89c9f6).html https://soeg.kb.dk/permalink/45KBDK_KGL/fbp0ps/alma99122333826705763 eng eng The Niels Bohr Institute, Faculty of Science, University of Copenhagen info:eu-repo/semantics/closedAccess Mikkelsen , T B 2017 , Ice Sheets & Ice Cores : Data Analysis & Stochastic Modelling . The Niels Bohr Institute, Faculty of Science, University of Copenhagen . < https://soeg.kb.dk/permalink/45KBDK_KGL/fbp0ps/alma99122333826705763 > book 2017 ftcopenhagenunip 2021-09-23T18:02:08Z Since the discovery of the Ice Ages it has been evident that Earth’s climate is liable to undergo dramatic changes. The previous climatic period known as the Last Glacial saw large oscillations in the extent of ice sheets covering the Northern hemisphere. Understanding these oscillations known as Dansgaard-Oeschger (DO) events would add to our knowledge of the climatic system and – hopefully – enable better forecasts. Likewise, to forecast possible future sea level rise it is crucial to correctly model the large ice sheets on Greenland and Antarctica. This project is divided into two parts. The first part concerns time series analysis of ice core data obtained from the Greenland Ice Sheet. We analyze parts of the time series where DO-events occur using the so-called transfer operator and compare the results with time series from a simple model capable of switching by either undergoing a bifurcation or by jumping at random. We find that the DO event time series is most consistent with the model undergoing a random transition. In the second part, we use a simple model of an ice sheet subject to constant and fluctuating temperatures, respectively. We find that the steady state volume of the ice sheet is lower for fluctuating temperatures than for a constant temperature. This finding may have implications for future long-range ice sheet projections, as the steady state ice sheet volume could be underestimated in studies using a constant temperature. Book Antarc* Antarctica Greenland ice core Ice Sheet University of Copenhagen: Research Greenland
institution Open Polar
collection University of Copenhagen: Research
op_collection_id ftcopenhagenunip
language English
description Since the discovery of the Ice Ages it has been evident that Earth’s climate is liable to undergo dramatic changes. The previous climatic period known as the Last Glacial saw large oscillations in the extent of ice sheets covering the Northern hemisphere. Understanding these oscillations known as Dansgaard-Oeschger (DO) events would add to our knowledge of the climatic system and – hopefully – enable better forecasts. Likewise, to forecast possible future sea level rise it is crucial to correctly model the large ice sheets on Greenland and Antarctica. This project is divided into two parts. The first part concerns time series analysis of ice core data obtained from the Greenland Ice Sheet. We analyze parts of the time series where DO-events occur using the so-called transfer operator and compare the results with time series from a simple model capable of switching by either undergoing a bifurcation or by jumping at random. We find that the DO event time series is most consistent with the model undergoing a random transition. In the second part, we use a simple model of an ice sheet subject to constant and fluctuating temperatures, respectively. We find that the steady state volume of the ice sheet is lower for fluctuating temperatures than for a constant temperature. This finding may have implications for future long-range ice sheet projections, as the steady state ice sheet volume could be underestimated in studies using a constant temperature.
format Book
author Mikkelsen, Troels Bøgeholm
spellingShingle Mikkelsen, Troels Bøgeholm
Ice Sheets & Ice Cores:Data Analysis & Stochastic Modelling
author_facet Mikkelsen, Troels Bøgeholm
author_sort Mikkelsen, Troels Bøgeholm
title Ice Sheets & Ice Cores:Data Analysis & Stochastic Modelling
title_short Ice Sheets & Ice Cores:Data Analysis & Stochastic Modelling
title_full Ice Sheets & Ice Cores:Data Analysis & Stochastic Modelling
title_fullStr Ice Sheets & Ice Cores:Data Analysis & Stochastic Modelling
title_full_unstemmed Ice Sheets & Ice Cores:Data Analysis & Stochastic Modelling
title_sort ice sheets & ice cores:data analysis & stochastic modelling
publisher The Niels Bohr Institute, Faculty of Science, University of Copenhagen
publishDate 2017
url https://curis.ku.dk/portal/da/publications/ice-sheets--ice-cores(74d12cf8-5a21-4c86-b22d-3b284c89c9f6).html
https://soeg.kb.dk/permalink/45KBDK_KGL/fbp0ps/alma99122333826705763
geographic Greenland
geographic_facet Greenland
genre Antarc*
Antarctica
Greenland
ice core
Ice Sheet
genre_facet Antarc*
Antarctica
Greenland
ice core
Ice Sheet
op_source Mikkelsen , T B 2017 , Ice Sheets & Ice Cores : Data Analysis & Stochastic Modelling . The Niels Bohr Institute, Faculty of Science, University of Copenhagen . < https://soeg.kb.dk/permalink/45KBDK_KGL/fbp0ps/alma99122333826705763 >
op_rights info:eu-repo/semantics/closedAccess
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