Research Field Area
Here is an index map showing where I spend
my winters (which are really summers...)
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Classes I teach
Fall 2005
Spring 2005
- GSC 10 - Geology of the National Parks
- GSC 496 - Anything but Excel
Fall 2004
- GSC 483 - Time Series Analysis
Spring 2004
Fall 2003
Fall 2002
- GSC 497 - Special Topics in Antarctic Geosciences
Spring 2003
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The goal of the ONSET project is to gain a better understanding
of the physical processes governing ice stream flow, particuarly near the
onset region. This project is collaborative with colleagues at the University
of Texas at Austin and the British Antarctic Survey.
The West Antarctic Ice Sheet (WAIS) is a marine ice sheet, grounded
below sea level and potentially unstable in reponse to sea-level rise and/or
climate warming. The flowof this ice sheet is variable on timescales ranging
from centuries to millenia. The future of this ice sheet is a topic of cosiderable
debate.
The ice streams of the Ross Sea Embayment (A--F) drain the interior West
Antarctic Ice Sheet by rapidly moving vast quantities of ice to the calving
front of the Ross Ice Shelf. These ice streams are key
factors in any discussion of WAIS stability because they are strongly out
of balance.Understanding the role of the ice streams as buffers between the
interior ice and the floating ice shelves; the reasons for their fast flow;
the factors controlling their current grounding-line-, margin-, and head-positions
are crucial to any attempt at modeling the WAIS system and predicting the
future of the ice sheet.
A new project to study the structure of the Trans Antarctic Mountains
(TAM) and the East Antarctic craton. We (Doug Wiens of Washington
University in St. Louis, Andy Nyblade of Penn State
Univ. and myself) will install three arrays
of seismometers in the TAM (about 100 km North and South of McMurdo) and
on the East Antarctic Ice Sheet (a line about half way to Dome C and another
line to the Gamburtsev Mountains) to record local and teleseismic earthquakes.
These data will be used to determine the crust and mantle structure beneath
the arrays..
We have installed eight stations (in 2000-01) and will install the
remaining 42 in 2001-02. The stations will be active until Jan, 2004. The
instrumentation is on loan from PASSCAL.
The International Geophysical Year (1957-58) was conceived as an
attempt to coordinate globe-wide measurements of the Earth, the oceans, the
atmosphere, and the Sun. Such a large undertaking required and
successfully acheived international cooperation in a time of
increasing geopolitical tension. The 50th anniversary of the IGY is
in 2007-08 and could and should herald in a new wave of geophysical
exploration of Antarctica to answer many outstanding questions of the
role of the continent in global environmental change, and of its
structure and history.
A project to install a network of seismic stations in Antarctica
that will plug a hole in the global seismic dataset. These stations are something
of an engineering challenge because of the cold and remoteness of the continent.
Some of the stations will be powered and heated by propane tanks and some
by wind (during the winter) and solar power during the summer.
Here is the terminator for today (the line separating night and day)
in Antarctica, at local noon at Byrd Surface Camp. The dark shading is night.
Antarctic Digital Database
I have converted the ADD continent
coastline, the Ross Ice Shelf outline, Filchner-Ronne Ice Shelf, some islands/ice-rises
in these ice shelves, and the Larsen, Risser and Amery Ice Shelves to geographic
coordinates. A test GMT script ADDtest.gmt will produce this Postscript image. I have `tar'-ed and `gzip'-ed
the six files and made them available for download.
The ADD copyright:
The text in this manual and the data provided on the CD are copyright.
Reproduction for scientific research, environmental conservation, educational
or other non-commercial purposes is authorised without prior permission from
the copyright holder. Reproduction for resale or any other commercial purpose
is prohibited without the prior written permission of the copyright holder.
Thanks to Michael Studinger
for pointing out a problem in the original conversion that I had posted to
the GMT mailing list. Which, of course, brings up the next disclaimer: caveat
emptor!
Influence of subglacial geology on
the position of a West Antarctic ice stream from seismic observations.
Tidal forcing of basal seismicity
These are in PDF format and you need a viewer (Adobe Acrobat Reader)
to look at it. I can mail it to you if you prefer. Send email to me at the
address below.
The SOAR workshop of March 18-19, 1996 was held at the National Science Foundation headquarters.
The SOAR
homepage
[Summer 2001] The McMurdo Area Users
Committee priority recommendation to RPSC is to bring
together the information needed for evaluating an overland traverse route
to S. Pole through W. Antarctica. There is strong scientific support for
an overland traverse, briefly summarized in a document prepared by S. Anandakrishnan
and the MAUC.
Science Justification for an Overland Traverse
to Resupply S. Pole.
Gravity Pier
[2001] The Thiel gravity base station is complete. The facilities
include an inside pier (1m square), and an outside pad (2.5m square).
[23 Dec 2000] The Thiel gravity base station is nearly completed.
Here are the ties between Hugo's Hut and other sites.
[02 Dec 1998] The latest plan is to convert the pumphouse that used
to service the buildings up the hill behind science cargo (the nuclear reactor)
into the new Gravity Hut.
[Jan 1998] A new location for the gravity pier is being considered.
This map of proposed pier locations around the
Crary Lab is a starting point for further discussion. Please contact me with comments and suggestions.
Go to the PSU Geophysics home
page.
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