G44A:
Glacial Isostatic Adjustment and the Importance of High-Quality Instrumental and Geological Constraints I


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Session ID#: 57907

Session Description:
Models of the Glacial Isostatic Adjustment (GIA) process continue to play a fundamental role in our understanding of Earth-Ice-Ocean interactions. The increasing availability of high-quality constraints on sea level evolution, crustal motion and the gravitational field of the planet has provided further insight on the evolution of the dynamic Earth system. In this session, we invite contributions that are focused upon: (1) the development and analysis of instrumental and geological records relevant to the study of the GIA process (which include, but are not limited to, geological reconstructions of relative sea level change, tide gauge records, satellite altimetry measurements, space-geodetic measurements of crustal motion and satellite gravimetric measurements); (2) the refinement of regional and global GIA models based upon this information (including new information on the viscosity structure of the Earth and on the evolution of continental ice cover); and (3) the insights on paleoclimate evolution that such analyses provide.
Primary Convener:  Keven Roy, Nanyang Technological University, Asian School of the Environment, Singapore, Singapore
Conveners:  Ben Horton, Nanyang Technological University, Asian School of the Environment, Singapore, Singapore and Nicole Khan, Nanyang Technological University, Asian School of the Environment, Singapore, Singapore
Primary Liaison:  Keven Roy, Nanyang Technological University, Asian School of the Environment, Singapore, Singapore
Chairs:  Keven Roy1, Ben Horton2 and Nicole Khan2, (1)University of Toronto, Toronto, ON, Canada(2)Nanyang Technological University, Asian School of the Environment, Singapore, Singapore
OSPA Liaison:  Nicole Khan, Nanyang Technological University, Asian School of the Environment, Singapore, Singapore

Cross-Listed:
  • C - Cryosphere
  • GC - Global Environmental Change
  • OS - Ocean Sciences
  • PP - Paleoceanography and Paleoclimatology
Index Terms:

Abstracts Submitted to this Session:

Eelco Johan Rohling, Australian National University, Research School of Earth Sciences, Canberra, Australia
Jacqueline Austermann, Columbia University, Lamont-Doherty Earth Observatory, Palisades, United States, Christine Y. Chen, Massachusetts Institute of Technology, Earth, Atmospheric and Planetary Sciences, Cambridge, United States, Harriet C. P. Lau, Brown University, Earth, Environmental, and Planetary Sciences, Providence, United States and Konstantin Latychev, Harvard University, Department of Earth and Planetary Sciences, Cambridge, NY, United States; Lamont-Doherty Earth Observatory, Columbia University, New York, NY, United States
W Richard Peltier, University of Toronto, Physics, Toronto, ON, Canada and Gordan R Stuhne, Department of Physics, Physics, Toronto, ON, Canada
Christopher G Piecuch, Woods Hole Oceanographic Institution, Physical Oceanography, Woods Hole, MA, United States, Peter J Huybers, Harvard University, Department of Earth and Planetary Sciences, Cambridge, MA, United States, Carling Hay, Harvard University, Earth and Planetary Sciences, Cambridge, MA, United States, Jerry X Mitrovica, Harvard University, Department of Earth and Planetary Sciences, Cambridge, United States, Christopher M Little, Atmospheric and Environmental Research, Inc., Lexington, United States, Rui M Ponte, Verisk Atmospheric and Environmental Research, Lexington, United States, Martin Tingley, Pennsylvania State University Main Campus, University Park, PA, United States and Andrew Kemp, Tufts University, Department of Earth and Ocean Sciences, Medford, United States
Riccardo Riva1, Yu Sun2,3, Pavel Ditmar2 and Roelof Rietbroek4, (1)Delft University of Technology, Department of Geoscience and Remote Sensing, Delft, Netherlands, (2)Delft University of Technology, Delft, Netherlands, (3)Fuzhou University, Fuzhou, China, (4)University of Bonn, Institute of Geodesy and Geoinformation, Bonn, Germany
Lambert Caron, Jet Propulsion Laboratory, Pasadena, United States and Erik Roman Ivins, JPL/Caltech, Pasadena, United States
Evelyn M Powell1, Natalya Gomez2, Mark Hoggard1, Konstantin Latychev3, Harriet C. P. Lau4 and Jerry X Mitrovica5, (1)Harvard University, Department of Earth and Planetary Sciences, Cambridge, MA, United States, (2)McGill University, Earth and Planetary Sciences, Montreal, QC, Canada, (3)Harvard University, Department of Earth and Planetary Sciences, Cambridge, NY, United States, (4)Brown University, Earth, Environmental, and Planetary Sciences, Providence, United States, (5)Harvard University, Department of Earth and Planetary Sciences, Cambridge, United States
Robert Smalley Jr1, Michael G Bevis2, Pedro Skvarca3, Eric C Kendrick2, Demián Gómez4,5, Sergio Cimbaro6, Hector Parra7 and Luis Eduardo Lenzano8, (1)University of Memphis, Center for Earthquake Research and Information, Memphis, TN, United States, (2)The Ohio State University, School of Earth Sciences, Columbus, United States, (3)Glaciarium-Glacier Interpretive Center, El Calafate, Argentina, (4)Instituto Geográfico Nacional, Dirección de Geodesia, Buenes Aires, Argentina, (5)Ohio State University Main Campus, Columbus, United States, (6)Instituto Geográfico Nacional, Buenos Aires, Argentina, (7)Instituto Geográfico Militar Chile, Departamento de Geodesia, Santiago, Chile, (8)El Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales, Mendoza, Argentina

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