Ice discharge of eastern Dome C drainage area, Antarctica, determined from airborne radar survey and satellite image analysis
Eastern Dome C, southern Talos Dome and northern Taylor Dome are drained by the Priestley, Reeves, David, Mawson and Mackay outlet glaciers, which flow into the Scott Coast on the west side of the Ross Sea, Antarctica. Airborne radar surveys were conducted on these glaciers to determine ice thicknes...
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Online Access: | http://hdl.handle.net/2122/6966 https://doi.org/10.3189/172756500781832855 |
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ftingv:oai:www.earth-prints.org:2122/6966 2023-05-15T14:01:36+02:00 Ice discharge of eastern Dome C drainage area, Antarctica, determined from airborne radar survey and satellite image analysis Frezzotti, M. Tabacco, I. E. Zirizzotti, A. Frezzotti, M. Tabacco, I. E. Zirizzotti, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia #PLACEHOLDER_PARENT_METADATA_VALUE# Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia 2000-03 http://hdl.handle.net/2122/6966 https://doi.org/10.3189/172756500781832855 en eng International Glaciological Society Journal of Glaciology 153/46 http://hdl.handle.net/2122/6966 doi:10.3189/172756500781832855 open Mass balance Antarctica 02. Cryosphere::02.02. Glaciers::02.02.06. Mass balance article 2000 ftingv https://doi.org/10.3189/172756500781832855 2022-07-29T06:05:56Z Eastern Dome C, southern Talos Dome and northern Taylor Dome are drained by the Priestley, Reeves, David, Mawson and Mackay outlet glaciers, which flow into the Scott Coast on the west side of the Ross Sea, Antarctica. Airborne radar surveys were conducted on these glaciers to determine ice thickness and bed morphology along transverse and longitudinal profiles of the grounded and floating segments. A new analysis of a Landsat Thematic Mapper satellite image using a tracking technique was used to measure ice velocity at grounding lines and along ice tongues. The integration of radar and satellite data helped to locate grounding lines and to calculate the ice discharge. Changes in ice fluxes of floating glaciers were used to determine basal melting and freezing rates. The ice discharge calculated is less than half that required for a zero net surface mass balance according to the inputs given by the accumulation estimates widely adopted at present. The basal melting rates of meteoric ice represent 50% of the net ablation rate. Published 253-264 3.8. Geofisica per l'ambiente JCR Journal open Article in Journal/Newspaper Antarc* Antarctica Journal of Glaciology Ross Sea Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) Mackay ENVELOPE(168.517,168.517,-77.700,-77.700) Priestley ENVELOPE(161.883,161.883,-75.183,-75.183) Reeves ENVELOPE(-67.983,-67.983,-67.133,-67.133) Ross Sea Scott Coast ENVELOPE(162.500,162.500,-76.500,-76.500) Talos Dome ENVELOPE(158.000,158.000,-73.000,-73.000) Taylor Dome ENVELOPE(157.667,157.667,-77.667,-77.667) Journal of Glaciology 46 153 253 264 |
institution |
Open Polar |
collection |
Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) |
op_collection_id |
ftingv |
language |
English |
topic |
Mass balance Antarctica 02. Cryosphere::02.02. Glaciers::02.02.06. Mass balance |
spellingShingle |
Mass balance Antarctica 02. Cryosphere::02.02. Glaciers::02.02.06. Mass balance Frezzotti, M. Tabacco, I. E. Zirizzotti, A. Ice discharge of eastern Dome C drainage area, Antarctica, determined from airborne radar survey and satellite image analysis |
topic_facet |
Mass balance Antarctica 02. Cryosphere::02.02. Glaciers::02.02.06. Mass balance |
description |
Eastern Dome C, southern Talos Dome and northern Taylor Dome are drained by the Priestley, Reeves, David, Mawson and Mackay outlet glaciers, which flow into the Scott Coast on the west side of the Ross Sea, Antarctica. Airborne radar surveys were conducted on these glaciers to determine ice thickness and bed morphology along transverse and longitudinal profiles of the grounded and floating segments. A new analysis of a Landsat Thematic Mapper satellite image using a tracking technique was used to measure ice velocity at grounding lines and along ice tongues. The integration of radar and satellite data helped to locate grounding lines and to calculate the ice discharge. Changes in ice fluxes of floating glaciers were used to determine basal melting and freezing rates. The ice discharge calculated is less than half that required for a zero net surface mass balance according to the inputs given by the accumulation estimates widely adopted at present. The basal melting rates of meteoric ice represent 50% of the net ablation rate. Published 253-264 3.8. Geofisica per l'ambiente JCR Journal open |
author2 |
Frezzotti, M. Tabacco, I. E. Zirizzotti, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia #PLACEHOLDER_PARENT_METADATA_VALUE# Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia |
format |
Article in Journal/Newspaper |
author |
Frezzotti, M. Tabacco, I. E. Zirizzotti, A. |
author_facet |
Frezzotti, M. Tabacco, I. E. Zirizzotti, A. |
author_sort |
Frezzotti, M. |
title |
Ice discharge of eastern Dome C drainage area, Antarctica, determined from airborne radar survey and satellite image analysis |
title_short |
Ice discharge of eastern Dome C drainage area, Antarctica, determined from airborne radar survey and satellite image analysis |
title_full |
Ice discharge of eastern Dome C drainage area, Antarctica, determined from airborne radar survey and satellite image analysis |
title_fullStr |
Ice discharge of eastern Dome C drainage area, Antarctica, determined from airborne radar survey and satellite image analysis |
title_full_unstemmed |
Ice discharge of eastern Dome C drainage area, Antarctica, determined from airborne radar survey and satellite image analysis |
title_sort |
ice discharge of eastern dome c drainage area, antarctica, determined from airborne radar survey and satellite image analysis |
publisher |
International Glaciological Society |
publishDate |
2000 |
url |
http://hdl.handle.net/2122/6966 https://doi.org/10.3189/172756500781832855 |
long_lat |
ENVELOPE(168.517,168.517,-77.700,-77.700) ENVELOPE(161.883,161.883,-75.183,-75.183) ENVELOPE(-67.983,-67.983,-67.133,-67.133) ENVELOPE(162.500,162.500,-76.500,-76.500) ENVELOPE(158.000,158.000,-73.000,-73.000) ENVELOPE(157.667,157.667,-77.667,-77.667) |
geographic |
Mackay Priestley Reeves Ross Sea Scott Coast Talos Dome Taylor Dome |
geographic_facet |
Mackay Priestley Reeves Ross Sea Scott Coast Talos Dome Taylor Dome |
genre |
Antarc* Antarctica Journal of Glaciology Ross Sea |
genre_facet |
Antarc* Antarctica Journal of Glaciology Ross Sea |
op_relation |
Journal of Glaciology 153/46 http://hdl.handle.net/2122/6966 doi:10.3189/172756500781832855 |
op_rights |
open |
op_doi |
https://doi.org/10.3189/172756500781832855 |
container_title |
Journal of Glaciology |
container_volume |
46 |
container_issue |
153 |
container_start_page |
253 |
op_container_end_page |
264 |
_version_ |
1766271551488917504 |