Geodetic and Seismic Observations of Ice-Stream Dynamics

The mass balance of large ice sheets is controlled by the dynamics of fast moving ice streams and outlet glaciers. In this work, I use geodetic and passive seismic observations to constrain rates of change in the flow of ice streams and illumi- nate fundamental processes that govern their behavior....

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Main Author: Winberry, Jeremy Paul
Other Authors: Sridhar Anandakrishnan, Richard B. Alley, Charles J. Ammon, Derrick L. Lampkin
Format: Text
Language:English
Published: Penn State 2008
Subjects:
Online Access:http://etda.libraries.psu.edu/theses/approved/WorldWideIndex/ETD-2833/index.html
id ftpennstate:OAI:PSUETD:ETD-2833
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spelling ftpennstate:OAI:PSUETD:ETD-2833 2023-05-15T16:42:00+02:00 Geodetic and Seismic Observations of Ice-Stream Dynamics Winberry, Jeremy Paul Sridhar Anandakrishnan Richard B. Alley Charles J. Ammon Derrick L. Lampkin 2008-08-16 application/pdf http://etda.libraries.psu.edu/theses/approved/WorldWideIndex/ETD-2833/index.html en eng Penn State WorldWide Copyright information available at source archive http://etda.libraries.psu.edu/theses/approved/WorldWideIndex/ETD-2833/index.html Geoscience text 2008 ftpennstate 2011-09-13T08:15:34Z The mass balance of large ice sheets is controlled by the dynamics of fast moving ice streams and outlet glaciers. In this work, I use geodetic and passive seismic observations to constrain rates of change in the flow of ice streams and illumi- nate fundamental processes that govern their behavior. An investigation of the flow field near the onset of Bindschadler Ice Streams reveals that the ice stream onset location is presently stable. Using passive seismic observations to monitor subglacial processes on MacAyeal Ice Stream, a set of harmonic glacial tremors were observed. The tremors are characterized by the sustained arrival 3 Hz energy for over 10 minutes, during which the source location migrates. The duration, monochromatic nature, and movement indicate the source mechanism is transient flow in the subglacial water system. A detailed investigation of the stick-slip mo- tion on Whillans Ice Stream is undertaken using detailed GPS observations of the surface velocity. These observations reveal that most aspects of stick-slip motion are modulated by the tides of the Ross Sea. The tides affect ice stream by introducing rates in which stress is accumulated during the time periods between slip events. Text Ice Stream A MacAyeal Ice Stream Ross Sea Whillans Ice Stream PennState: Electronic Theses and Dissertations (eTD) MacAyeal Ice Stream ENVELOPE(-143.000,-143.000,-80.000,-80.000) Ross Sea Whillans ENVELOPE(-64.250,-64.250,-84.450,-84.450) Whillans Ice Stream ENVELOPE(-145.000,-145.000,-83.667,-83.667)
institution Open Polar
collection PennState: Electronic Theses and Dissertations (eTD)
op_collection_id ftpennstate
language English
topic Geoscience
spellingShingle Geoscience
Winberry, Jeremy Paul
Geodetic and Seismic Observations of Ice-Stream Dynamics
topic_facet Geoscience
description The mass balance of large ice sheets is controlled by the dynamics of fast moving ice streams and outlet glaciers. In this work, I use geodetic and passive seismic observations to constrain rates of change in the flow of ice streams and illumi- nate fundamental processes that govern their behavior. An investigation of the flow field near the onset of Bindschadler Ice Streams reveals that the ice stream onset location is presently stable. Using passive seismic observations to monitor subglacial processes on MacAyeal Ice Stream, a set of harmonic glacial tremors were observed. The tremors are characterized by the sustained arrival 3 Hz energy for over 10 minutes, during which the source location migrates. The duration, monochromatic nature, and movement indicate the source mechanism is transient flow in the subglacial water system. A detailed investigation of the stick-slip mo- tion on Whillans Ice Stream is undertaken using detailed GPS observations of the surface velocity. These observations reveal that most aspects of stick-slip motion are modulated by the tides of the Ross Sea. The tides affect ice stream by introducing rates in which stress is accumulated during the time periods between slip events.
author2 Sridhar Anandakrishnan
Richard B. Alley
Charles J. Ammon
Derrick L. Lampkin
format Text
author Winberry, Jeremy Paul
author_facet Winberry, Jeremy Paul
author_sort Winberry, Jeremy Paul
title Geodetic and Seismic Observations of Ice-Stream Dynamics
title_short Geodetic and Seismic Observations of Ice-Stream Dynamics
title_full Geodetic and Seismic Observations of Ice-Stream Dynamics
title_fullStr Geodetic and Seismic Observations of Ice-Stream Dynamics
title_full_unstemmed Geodetic and Seismic Observations of Ice-Stream Dynamics
title_sort geodetic and seismic observations of ice-stream dynamics
publisher Penn State
publishDate 2008
url http://etda.libraries.psu.edu/theses/approved/WorldWideIndex/ETD-2833/index.html
long_lat ENVELOPE(-143.000,-143.000,-80.000,-80.000)
ENVELOPE(-64.250,-64.250,-84.450,-84.450)
ENVELOPE(-145.000,-145.000,-83.667,-83.667)
geographic MacAyeal Ice Stream
Ross Sea
Whillans
Whillans Ice Stream
geographic_facet MacAyeal Ice Stream
Ross Sea
Whillans
Whillans Ice Stream
genre Ice Stream A
MacAyeal Ice Stream
Ross Sea
Whillans Ice Stream
genre_facet Ice Stream A
MacAyeal Ice Stream
Ross Sea
Whillans Ice Stream
op_source http://etda.libraries.psu.edu/theses/approved/WorldWideIndex/ETD-2833/index.html
op_rights WorldWide
Copyright information available at source archive
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