West Antarctica snow accumulation trend study (1979-2011) from Snow Radar and ice core profiles
Ice sheets are under threat from increasing air and ocean temperatures. For Antarctica, observed changes are most apparent near the margins; inland the effects of a warming atmosphere and changing circulation patterns are less clear. Snow accumulation to the ice sheet offsets ice losses near the mar...
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ftunivkansas:oai:kuscholarworks.ku.edu:1808/18674 2023-05-15T13:32:09+02:00 West Antarctica snow accumulation trend study (1979-2011) from Snow Radar and ice core profiles Feng, Boyu Braaten, David Slocum, Terry Li, Xingong 2014 119 pages http://hdl.handle.net/1808/18674 http://dissertations.umi.com/ku:13644 en eng University of Kansas http://dissertations.umi.com/ku:13644 http://hdl.handle.net/1808/18674 Copyright held by the author. openAccess Geography Physical geography automatic weather station ice core ice sheet meteorological model Snow Radar Thesis 2014 ftunivkansas 2022-08-26T13:16:16Z Ice sheets are under threat from increasing air and ocean temperatures. For Antarctica, observed changes are most apparent near the margins; inland the effects of a warming atmosphere and changing circulation patterns are less clear. Snow accumulation to the ice sheet offsets ice losses near the margin, and characterizing ice sheet accumulation rate is necessary for understanding ice sheet mass balance and predicting future sea level rise. Ice penetrating radar systems enable the measurement of ice sheet properties beneath the surface, such as ice thickness and internal layering. This study concentrates on mapping the depth of internal layers, and linking the layers to a chronology that allows snow accumulation rates over particular time periods to be determined. The focus is on one particular ice penetrating radar system: Snow Radar from the Center for Remote Sensing of Ice Sheet (CReSIS). The Snow Radar is a 2-8 GHz ultra-wideband (UWB), frequency-modulated, continuous-wave (FMCW) radar, having a ~5cm vertical resolution. The chronology of Snow Radar detected layers is validated to be annual layers using nearby ice core data and the results of a regional climate model (RACMO2.1/ANT). The measurement error of a manual layer picking procedure, and proximity of ice core density profiles to the Snow Radar data have been examined. The results show that the average error variance in manual picking is as small as 3.0e-4 m, and that it is reasonable to use ice core density profiles in Snow Radar data processing. Using Snow Radar data, a snow accumulation rate time series has been determined along two flight lines over West Antarctica. The spatiotemporal distribution of snow accumulation has been analyzed and possible explanations for such distribution are discussed. No significant trend is found in snow accumulation during the 33-year study period (1979-2011). The snow accumulation spatial distribution has been related to topography and wind, showing that snow accumulation has a negative correlation with elevation and ... Thesis Antarc* Antarctica ice core Ice Sheet West Antarctica The University of Kansas: KU ScholarWorks West Antarctica |
institution |
Open Polar |
collection |
The University of Kansas: KU ScholarWorks |
op_collection_id |
ftunivkansas |
language |
English |
topic |
Geography Physical geography automatic weather station ice core ice sheet meteorological model Snow Radar |
spellingShingle |
Geography Physical geography automatic weather station ice core ice sheet meteorological model Snow Radar Feng, Boyu West Antarctica snow accumulation trend study (1979-2011) from Snow Radar and ice core profiles |
topic_facet |
Geography Physical geography automatic weather station ice core ice sheet meteorological model Snow Radar |
description |
Ice sheets are under threat from increasing air and ocean temperatures. For Antarctica, observed changes are most apparent near the margins; inland the effects of a warming atmosphere and changing circulation patterns are less clear. Snow accumulation to the ice sheet offsets ice losses near the margin, and characterizing ice sheet accumulation rate is necessary for understanding ice sheet mass balance and predicting future sea level rise. Ice penetrating radar systems enable the measurement of ice sheet properties beneath the surface, such as ice thickness and internal layering. This study concentrates on mapping the depth of internal layers, and linking the layers to a chronology that allows snow accumulation rates over particular time periods to be determined. The focus is on one particular ice penetrating radar system: Snow Radar from the Center for Remote Sensing of Ice Sheet (CReSIS). The Snow Radar is a 2-8 GHz ultra-wideband (UWB), frequency-modulated, continuous-wave (FMCW) radar, having a ~5cm vertical resolution. The chronology of Snow Radar detected layers is validated to be annual layers using nearby ice core data and the results of a regional climate model (RACMO2.1/ANT). The measurement error of a manual layer picking procedure, and proximity of ice core density profiles to the Snow Radar data have been examined. The results show that the average error variance in manual picking is as small as 3.0e-4 m, and that it is reasonable to use ice core density profiles in Snow Radar data processing. Using Snow Radar data, a snow accumulation rate time series has been determined along two flight lines over West Antarctica. The spatiotemporal distribution of snow accumulation has been analyzed and possible explanations for such distribution are discussed. No significant trend is found in snow accumulation during the 33-year study period (1979-2011). The snow accumulation spatial distribution has been related to topography and wind, showing that snow accumulation has a negative correlation with elevation and ... |
author2 |
Braaten, David Slocum, Terry Li, Xingong |
format |
Thesis |
author |
Feng, Boyu |
author_facet |
Feng, Boyu |
author_sort |
Feng, Boyu |
title |
West Antarctica snow accumulation trend study (1979-2011) from Snow Radar and ice core profiles |
title_short |
West Antarctica snow accumulation trend study (1979-2011) from Snow Radar and ice core profiles |
title_full |
West Antarctica snow accumulation trend study (1979-2011) from Snow Radar and ice core profiles |
title_fullStr |
West Antarctica snow accumulation trend study (1979-2011) from Snow Radar and ice core profiles |
title_full_unstemmed |
West Antarctica snow accumulation trend study (1979-2011) from Snow Radar and ice core profiles |
title_sort |
west antarctica snow accumulation trend study (1979-2011) from snow radar and ice core profiles |
publisher |
University of Kansas |
publishDate |
2014 |
url |
http://hdl.handle.net/1808/18674 http://dissertations.umi.com/ku:13644 |
geographic |
West Antarctica |
geographic_facet |
West Antarctica |
genre |
Antarc* Antarctica ice core Ice Sheet West Antarctica |
genre_facet |
Antarc* Antarctica ice core Ice Sheet West Antarctica |
op_relation |
http://dissertations.umi.com/ku:13644 http://hdl.handle.net/1808/18674 |
op_rights |
Copyright held by the author. openAccess |
_version_ |
1766024578917728256 |