Calving front dynamics : External forces that lead to specific sized calving events
Currently there is no extended study that explicitly focuses on themagnitude, frequency and timing of glacial calving resulting from externalforces. Past studies have identified the size and timing of calving events butthe links between them and the external factors that cause them are stillmissing....
Main Author: | |
---|---|
Format: | Bachelor Thesis |
Language: | English |
Published: |
Uppsala universitet, Institutionen för geovetenskaper
2014
|
Subjects: | |
Online Access: | http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-237686 |
id |
ftuppsalauniv:oai:DiVA.org:uu-237686 |
---|---|
record_format |
openpolar |
spelling |
ftuppsalauniv:oai:DiVA.org:uu-237686 2023-05-15T16:21:16+02:00 Calving front dynamics : External forces that lead to specific sized calving events Wainwright, Daniel 2014 application/pdf http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-237686 eng eng Uppsala universitet, Institutionen för geovetenskaper Examensarbete vid Institutionen för geovetenskaper, 1650-6553 297 http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-237686 info:eu-repo/semantics/openAccess Greenland calving climate photography glacier tidewater Physical Geography Naturgeografi Student thesis info:eu-repo/semantics/bachelorThesis text 2014 ftuppsalauniv 2023-02-23T21:46:10Z Currently there is no extended study that explicitly focuses on themagnitude, frequency and timing of glacial calving resulting from externalforces. Past studies have identified the size and timing of calving events butthe links between them and the external factors that cause them are stillmissing. Here I present a method to identify the size, time and frequency ofcalving events on the Rink Glacier in Greenland. Using time lapse imagesspaced 30 minutes apart of the calving front, coupled with weather and tidedata, I plan on identifying the main driving force for calving. Results showthat atmospheric pressure and temperature have no positive correlation withcalving magnitude or size. Tidal influences and sea surface temperatureappear to have the strongest influence on the frequency of calving. As seasurface temperatures rapidly decrease though the study period, calvingfrequency also reduces. Strong calving correlations for the entire studyperiod were difficult to identify for tidal influences, as images could only betaken during the sunlit periods of the day. As this study was conductedduring autumn when atmospheric temperatures remained below 0°C, theavailability of melt water for crevasse creation and basal lubrication was notpresent. Therefore it is suggested that future studies on glacial stabilityshould use external forces to measure ice loss over the entire calving season. Bachelor Thesis glacier Greenland Tidewater Uppsala University: Publications (DiVA) Greenland |
institution |
Open Polar |
collection |
Uppsala University: Publications (DiVA) |
op_collection_id |
ftuppsalauniv |
language |
English |
topic |
Greenland calving climate photography glacier tidewater Physical Geography Naturgeografi |
spellingShingle |
Greenland calving climate photography glacier tidewater Physical Geography Naturgeografi Wainwright, Daniel Calving front dynamics : External forces that lead to specific sized calving events |
topic_facet |
Greenland calving climate photography glacier tidewater Physical Geography Naturgeografi |
description |
Currently there is no extended study that explicitly focuses on themagnitude, frequency and timing of glacial calving resulting from externalforces. Past studies have identified the size and timing of calving events butthe links between them and the external factors that cause them are stillmissing. Here I present a method to identify the size, time and frequency ofcalving events on the Rink Glacier in Greenland. Using time lapse imagesspaced 30 minutes apart of the calving front, coupled with weather and tidedata, I plan on identifying the main driving force for calving. Results showthat atmospheric pressure and temperature have no positive correlation withcalving magnitude or size. Tidal influences and sea surface temperatureappear to have the strongest influence on the frequency of calving. As seasurface temperatures rapidly decrease though the study period, calvingfrequency also reduces. Strong calving correlations for the entire studyperiod were difficult to identify for tidal influences, as images could only betaken during the sunlit periods of the day. As this study was conductedduring autumn when atmospheric temperatures remained below 0°C, theavailability of melt water for crevasse creation and basal lubrication was notpresent. Therefore it is suggested that future studies on glacial stabilityshould use external forces to measure ice loss over the entire calving season. |
format |
Bachelor Thesis |
author |
Wainwright, Daniel |
author_facet |
Wainwright, Daniel |
author_sort |
Wainwright, Daniel |
title |
Calving front dynamics : External forces that lead to specific sized calving events |
title_short |
Calving front dynamics : External forces that lead to specific sized calving events |
title_full |
Calving front dynamics : External forces that lead to specific sized calving events |
title_fullStr |
Calving front dynamics : External forces that lead to specific sized calving events |
title_full_unstemmed |
Calving front dynamics : External forces that lead to specific sized calving events |
title_sort |
calving front dynamics : external forces that lead to specific sized calving events |
publisher |
Uppsala universitet, Institutionen för geovetenskaper |
publishDate |
2014 |
url |
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-237686 |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
glacier Greenland Tidewater |
genre_facet |
glacier Greenland Tidewater |
op_relation |
Examensarbete vid Institutionen för geovetenskaper, 1650-6553 297 http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-237686 |
op_rights |
info:eu-repo/semantics/openAccess |
_version_ |
1766009284802379776 |