Remote GPS in Antarctica

Slides:



Advertisements
Similar presentations
Swinging gate or Saloon Doors? Do we need a new model of WAIS deglaciation? Robert P. Ackert Jr. Harvard University WAIS 2008.
Advertisements

The general equation for gravity anomaly is: where:  is the gravitational constant  is the density contrast r is the distance to the observation point.
Deformation of the Crust
Ten Fifteen Years of Development on UMISM: Application to Advance and Retreat of the Siple Coast Region James L Fastook Jesse V Johnson Sean Birkel We.
CHAPTER 5: Earth dynamics
Observing Glacial Rebound Using GPS Giovanni Sella and Seth Stein Northwestern University Michael Craymer Geodetic Survey Division, Natural Resources Canada.
Roosevelt Island: a good place for an ice core H. Conway, Nancy Bertler, David Bromwich, Ed Brook, Dorthe Dahl- Jensen, Karl Kreutz, Andrei Kurbatov, Paul.
Glacial Rebound Glacial Rebound Studies depend on many factors. What are they ? Ice load History of the load Ocean water load on coastlines and globally.
Isostasy can be seen where the Earth's lithosphere (crust) presses down on the weaker asthenosphere )mantle) which, over deep geological time, flows sideways.
IINTRUSIVE VOLCANIC FEATURES
Thanks SO Much for ALL the Data: The Amundsen Sea Sector Data Set: Applications with UMISM: Where and How Much WATER? What WILL happen in the future? James.
Tradeoff between climate and thickness histories at Siple Dome during the past 25 ka Ed Waddington, Howard Conway, Eric Steig, Richard Alley, Ed Brook,
The Hunting of the SNARF Giovanni F. Sella Seth Stein Northwestern University Timothy H. Dixon University of Miami "What's the good of Mercator's North.
Background to >10 years of BIFROST activities Jan M. Johansson 1, Hans-Georg Scherneck 1, Rüdiger Haas 1, Sten Bergstrand 1 Martin Lidberg 1,2, Lotti Jivall.
Deformation Analysis in the North American Plate’s Interior Calais E, Purdue University, West Lafayette, IN, Han JY,
Observing Glacial Rebound Using GPS Giovanni Sella.
©2010 Elsevier, Inc. 1 Chapter 14 Cuffey & Paterson.
An improved and extended GPS derived velocity field of the postglacial adjustment in Fennoscandia Martin Lidberg 1,3, Jan M. Johansson 1, Hans-Georg Scherneck.
Projectiles Horizontal Projection Horizontally: Vertically: Vertical acceleration g  9.8 To investigate the motion of a projectile, its horizontal and.
Using Flubber to Study Glaciers A Hands-on Experience.
Subglacial Landform Analysis and Reconstruction of Miocene Paleotopography of Marie Byrd Land Perry Spector 1,2, Christine Siddoway 1, and Paul Morin 2.
Gravity 2. Geoid, spheroid Measurement of gravity Absolute measurements Relative measurements True gravitational Acceleration Difference in gravitational.
The Plausible Range of GIA Contributions to 3-D Motions at GPS Sites in the SNARF Network 2004 Joint AssemblyG21D-03 Mark Tamisiea 1, Jerry Mitrovica 2,
Western Antarctica & Antarctic Ice Shelves Eric Leibensperger EPS 131.
Reference Frame Theory & Practice: Implications for SNARF SNARF Workshop 1/27/04 Geoff Blewitt University of Nevada, Reno.
3 rd International ACES Meeting Maui, Hawaii May 6-10, 2002 Sponsored by NASA and NSF.
05/12/1005/08/ Lec Lec Principles of the Global Positioning System Lecture 23 Prof. Thomas Herring Room ;
1 6.2 The Theory of Plate Tectonics. 2 How is water in a pot that is held over a flame become heated throughout, even though the flame touches only the.
Assessing the GIA Contribution to SNARF Mark Tamisiea and Jim Davis Harvard-Smithsonian Center for Astrophysics.
ISOSTASY A Plate Tectonic Process of Equilibrium.
Aug 6, 2002APSG Irkutsk Contemporary Horizontal and Vertical Deformation of the Tien Shan Thomas Herring, Bradford H. Hager, Brendan Meade, Massachusetts.
Response of an Elastic Half Space to an Arbitrary 3-D Vector Body Force Smith and Sandwell, JGR 2003 Develop the three differential equations relating.
Unit D: Energy Flow in Global Systems. The Biosphere.
POST- GLACIAL REBOUND. The adjustment of land that was depressed by the weight of ice sheets that were created in the last glacial period. DEFINITION.
Activities of the Italian Geodetic Observatory in Antarctica
Glacio-isostatic Response in the Puget Lowland
The Earth’s structure.
Contemporary Horizontal and Vertical Deformation of the Tien Shan
6.2 The Theory of Plate Tectonics
Weather The condition of the atmosphere at a given place
IN: What force, do you suppose causes the plates to move?
Gravity II: Gravity anomaly due to a simple-shape buried body
Stable North American Reference Frame (SNARF): Version 1
Geodesy & Crustal Deformation
Objectives Summarize the principle of isostasy.
Sea level data for the Iberian Peninsula
Your Guide for Learning
Chapter 1: Maps as Models of the Earth
Plate Boundaries.
The Last Glacial Maximum (LGM)
The Earth’s structure.
Chapter 7 Section 2 Pages Continental Drift.
Chapter 7 Section 2 Pages Continental Drift.
Horizontal GIA Velocities and Reference-Frame Determination
Vertical Velocity or Precipitation
Weather Variables: Air Pressure and Wind
Dee1 View from back of back plate
Remote GPS Networks: Rationale
Chapter 1 Section 9 How do you read a topographic map?
Layers of the Earth What Lies Beneath?.
A Map Grid and Index.
Glaciers and Earthquakes
Earth Science- The Earth’s Moving Plates
Theme 2: Changing Environments 2.4 Climate Change – Cause & Effect
GPS: GLOBAL POSITIONING SYSTEM Satellites transmit radio signals Receivers on ground record signals and find their position from the time the signals arrive.
Chapter 7 Section 2 Pages Continental Drift.
Aim: How do the plates of the Earth move?
Exploring Antarctica and the Southern Ocean
Exploring Antarctica and the Southern Ocean
Stable North American Reference Frame (SNARF): Version 1
Presentation transcript:

Remote GPS in Antarctica Andrea Donnellan and Bruce Luyendyk Thanks to: Mark Smith, Tom Rebold, Henry Awaya, Demetri Capetanopoulos, Russell Knight, Shannon Jackson, Alan Hogan, Charles Day, and Timothy Stough. Kenneth Hurst for data processing and Donald Argus for the plate rotation. Eric Ivins for discussions of postglacial rebound modeling. Supported by US NSF OPP 9725876 and NASA.

Location maps

Post Glacial Rebound The thick ice sheet pushes down on the earth As the ice thins the mantle flows back The surface of the earth rebounds

Ford Ranges from the air

At Siple Dome…

Installing MBL1 Rockefeller Mountains

MBL1, Mt. Patterson, Rockefeller Mts., Marie Byrd Land Antenna is still in place…

Length time series; wrt Davis, McMurdo MBL3 data not used for 2002

Absolute Horizontal Velocities

Residual Horizontal Velocities Plate rotation about Davis removed

Vertical time series MBL3 data not used for 2002

Vertical Velocities

Conclusions so far… No horizontal strain >2 mm/yr in wMBL, across Ross Embayment, or between WANT and EANT Vertical motion due to rebound since late Holocene retreat - load was in east Ross Sea Continuous power source is key to continuous GPS Steve Tucker