Combining physics-based and statistics-based approaches to model calving in Antarctica
Surface and basal crevasses are deep fractures in ice that are observed on the surface and the base of the Antarctic ice sheet/ice shelves, respectively. They are a direct pre- cursor of formation of rifts in ice shelves and a consequent calving or breaking off of icebergs. Modelling of calving is c...
Main Author: | |
---|---|
Format: | Thesis |
Language: | English |
Published: |
The Australian National University
2019
|
Subjects: | |
Online Access: | https://dx.doi.org/10.25911/5c765954dc1a1 https://openresearch-repository.anu.edu.au/handle/1885/156513 |
id |
ftdatacite:10.25911/5c765954dc1a1 |
---|---|
record_format |
openpolar |
spelling |
ftdatacite:10.25911/5c765954dc1a1 2023-05-15T14:03:31+02:00 Combining physics-based and statistics-based approaches to model calving in Antarctica Emetc, Veronika 2019 https://dx.doi.org/10.25911/5c765954dc1a1 https://openresearch-repository.anu.edu.au/handle/1885/156513 en eng The Australian National University Antarctica ice shelves ice sheet calving fractures crevasses basal modelling ISSM Other CreativeWork article Thesis (PhD) 2019 ftdatacite https://doi.org/10.25911/5c765954dc1a1 2021-11-05T12:55:41Z Surface and basal crevasses are deep fractures in ice that are observed on the surface and the base of the Antarctic ice sheet/ice shelves, respectively. They are a direct pre- cursor of formation of rifts in ice shelves and a consequent calving or breaking off of icebergs. Modelling of calving is crucial for better estimation of the ice mass balance in Antarctica because ice shelves act like a supporting mechanism for the inland ice preventing it from accelerating into the ocean. While there have been a number of studies that attempted to parameterise calving, each of them has limitations that do not allow to apply them to all the Antarctic ice shelves on a large scale. A more comprehensive calving model needs to include not only parameterisation of calving at ice fronts, but also the history of fracturing of the ice that led to a calving event such as formation, advection and propagation of both surface and basal crevasses. Towards improving a calving parameterisation in ice sheet models we constructed a set of sub-models for predicting surface and basal fracturing, vertical and horizontal propagation as well as advection. Combining statistics-based and physics-based ap- proachers we developed a preliminary calving model that includes the full history of rifts and crevasses, from their initiation to the final break off at the ice front. Thesis Antarc* Antarctic Antarctica Ice Sheet Ice Shelves Iceberg* DataCite Metadata Store (German National Library of Science and Technology) Antarctic The Antarctic |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Antarctica ice shelves ice sheet calving fractures crevasses basal modelling ISSM |
spellingShingle |
Antarctica ice shelves ice sheet calving fractures crevasses basal modelling ISSM Emetc, Veronika Combining physics-based and statistics-based approaches to model calving in Antarctica |
topic_facet |
Antarctica ice shelves ice sheet calving fractures crevasses basal modelling ISSM |
description |
Surface and basal crevasses are deep fractures in ice that are observed on the surface and the base of the Antarctic ice sheet/ice shelves, respectively. They are a direct pre- cursor of formation of rifts in ice shelves and a consequent calving or breaking off of icebergs. Modelling of calving is crucial for better estimation of the ice mass balance in Antarctica because ice shelves act like a supporting mechanism for the inland ice preventing it from accelerating into the ocean. While there have been a number of studies that attempted to parameterise calving, each of them has limitations that do not allow to apply them to all the Antarctic ice shelves on a large scale. A more comprehensive calving model needs to include not only parameterisation of calving at ice fronts, but also the history of fracturing of the ice that led to a calving event such as formation, advection and propagation of both surface and basal crevasses. Towards improving a calving parameterisation in ice sheet models we constructed a set of sub-models for predicting surface and basal fracturing, vertical and horizontal propagation as well as advection. Combining statistics-based and physics-based ap- proachers we developed a preliminary calving model that includes the full history of rifts and crevasses, from their initiation to the final break off at the ice front. |
format |
Thesis |
author |
Emetc, Veronika |
author_facet |
Emetc, Veronika |
author_sort |
Emetc, Veronika |
title |
Combining physics-based and statistics-based approaches to model calving in Antarctica |
title_short |
Combining physics-based and statistics-based approaches to model calving in Antarctica |
title_full |
Combining physics-based and statistics-based approaches to model calving in Antarctica |
title_fullStr |
Combining physics-based and statistics-based approaches to model calving in Antarctica |
title_full_unstemmed |
Combining physics-based and statistics-based approaches to model calving in Antarctica |
title_sort |
combining physics-based and statistics-based approaches to model calving in antarctica |
publisher |
The Australian National University |
publishDate |
2019 |
url |
https://dx.doi.org/10.25911/5c765954dc1a1 https://openresearch-repository.anu.edu.au/handle/1885/156513 |
geographic |
Antarctic The Antarctic |
geographic_facet |
Antarctic The Antarctic |
genre |
Antarc* Antarctic Antarctica Ice Sheet Ice Shelves Iceberg* |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet Ice Shelves Iceberg* |
op_doi |
https://doi.org/10.25911/5c765954dc1a1 |
_version_ |
1766274194592497664 |