The east Antarctic ice: from ice sheet flow to iceberg dissolution
© 1987 Trevor Colin Hamley This thesis investigates the question of the state of balance, mass budget and dynamics of a large section of the East Antarctic Ice Sheet. The distribution and dissolution of icebergs originating from the icesheet outflux is also determined. Comparison of field measuremen...
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ftumelbourne:oai:jupiter.its.unimelb.edu.au:11343/36575 2023-05-15T13:41:15+02:00 The east Antarctic ice: from ice sheet flow to iceberg dissolution Hamley, Trevor Colin 1987 http://hdl.handle.net/11343/36575 eng eng Hamley, T. C. (1987). The east Antarctic ice: from ice sheet flow to iceberg dissolution. Masters Research thesis, Meteorology Department, The University of Melbourne. http://hdl.handle.net/11343/36575 Terms and Conditions: Copyright in works deposited in Minerva Access is retained by the copyright owner. The work may not be altered without permission from the copyright owner. Readers may only download, print and save electronic copies of whole works for their own personal non-commercial use. Any use that exceeds these limits requires permission from the copyright owner. Attribution is essential when quoting or paraphrasing from these works. ice sheets icebergs Antarctica Masters Research thesis 1987 ftumelbourne 2019-10-15T12:07:40Z © 1987 Trevor Colin Hamley This thesis investigates the question of the state of balance, mass budget and dynamics of a large section of the East Antarctic Ice Sheet. The distribution and dissolution of icebergs originating from the icesheet outflux is also determined. Comparison of field measurements collected from oversnow traversing, with balance calculations determined by computer modelling studies, shows that the ice sheet is not likely to be significantly out of balance (i.e. by more than ±10%). By assuming that it is in balance, the ratio of average column velocity to surface velocity is determined to be 0.89. Analysis of the mean strain-rate versus down slope shear-stress indicates values of the commonly used power flow law parameters to be n = 3.2 and k1 = 0.023 bar -n s-1. For the basal ice and high shear zone ice the value of k1 is shown to be k1 = 0.055 bar -n s-1. Comparison of the same results with laboratory work suggests temperatures of the basal ice to be between -5° C and -10° C. The outflux of ice between longitude 90° E and 150° E is estimated to be be 389 km3a-1. Analysis of iceberg size frequency distributions from shipboard observations reveals that Antarctic icebergs (less than 1000m in horizontal dimension) have a median life before breakage, of 0.2 years. This is significantly lower than previously thought. The mean melt rate is estimated to be 0.12 md-1 which agrees broadly with previous laboratory studies for water temperatures averaging + 1°C. More accurate data on iceberg calving, movement and dissolution is required to adequately assess discrepencies from balance computed by ice sheet accumulation and flow studies. Master Thesis Antarc* Antarctic Antarctica Ice Sheet Iceberg* The University of Melbourne: Digital Repository Antarctic East Antarctic Ice Sheet |
institution |
Open Polar |
collection |
The University of Melbourne: Digital Repository |
op_collection_id |
ftumelbourne |
language |
English |
topic |
ice sheets icebergs Antarctica |
spellingShingle |
ice sheets icebergs Antarctica Hamley, Trevor Colin The east Antarctic ice: from ice sheet flow to iceberg dissolution |
topic_facet |
ice sheets icebergs Antarctica |
description |
© 1987 Trevor Colin Hamley This thesis investigates the question of the state of balance, mass budget and dynamics of a large section of the East Antarctic Ice Sheet. The distribution and dissolution of icebergs originating from the icesheet outflux is also determined. Comparison of field measurements collected from oversnow traversing, with balance calculations determined by computer modelling studies, shows that the ice sheet is not likely to be significantly out of balance (i.e. by more than ±10%). By assuming that it is in balance, the ratio of average column velocity to surface velocity is determined to be 0.89. Analysis of the mean strain-rate versus down slope shear-stress indicates values of the commonly used power flow law parameters to be n = 3.2 and k1 = 0.023 bar -n s-1. For the basal ice and high shear zone ice the value of k1 is shown to be k1 = 0.055 bar -n s-1. Comparison of the same results with laboratory work suggests temperatures of the basal ice to be between -5° C and -10° C. The outflux of ice between longitude 90° E and 150° E is estimated to be be 389 km3a-1. Analysis of iceberg size frequency distributions from shipboard observations reveals that Antarctic icebergs (less than 1000m in horizontal dimension) have a median life before breakage, of 0.2 years. This is significantly lower than previously thought. The mean melt rate is estimated to be 0.12 md-1 which agrees broadly with previous laboratory studies for water temperatures averaging + 1°C. More accurate data on iceberg calving, movement and dissolution is required to adequately assess discrepencies from balance computed by ice sheet accumulation and flow studies. |
format |
Master Thesis |
author |
Hamley, Trevor Colin |
author_facet |
Hamley, Trevor Colin |
author_sort |
Hamley, Trevor Colin |
title |
The east Antarctic ice: from ice sheet flow to iceberg dissolution |
title_short |
The east Antarctic ice: from ice sheet flow to iceberg dissolution |
title_full |
The east Antarctic ice: from ice sheet flow to iceberg dissolution |
title_fullStr |
The east Antarctic ice: from ice sheet flow to iceberg dissolution |
title_full_unstemmed |
The east Antarctic ice: from ice sheet flow to iceberg dissolution |
title_sort |
east antarctic ice: from ice sheet flow to iceberg dissolution |
publishDate |
1987 |
url |
http://hdl.handle.net/11343/36575 |
geographic |
Antarctic East Antarctic Ice Sheet |
geographic_facet |
Antarctic East Antarctic Ice Sheet |
genre |
Antarc* Antarctic Antarctica Ice Sheet Iceberg* |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet Iceberg* |
op_relation |
Hamley, T. C. (1987). The east Antarctic ice: from ice sheet flow to iceberg dissolution. Masters Research thesis, Meteorology Department, The University of Melbourne. http://hdl.handle.net/11343/36575 |
op_rights |
Terms and Conditions: Copyright in works deposited in Minerva Access is retained by the copyright owner. The work may not be altered without permission from the copyright owner. Readers may only download, print and save electronic copies of whole works for their own personal non-commercial use. Any use that exceeds these limits requires permission from the copyright owner. Attribution is essential when quoting or paraphrasing from these works. |
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