The contribution of glacial isostatic adjustment to projections of sea‐level change along the Atlantic and Gulf coasts of North America

Author:

Love Ryan12,Milne Glenn A.3,Tarasov Lev2,Engelhart Simon E.4,Hijma Marc P.56,Latychev Konstantin7,Horton Benjamin P.89,Törnqvist Torbjörn E.5

Affiliation:

1. Department of Physics University of Ottawa Ottawa Ontario

2. Department of Physics and Physical Oceanography Memorial University of Newfoundland St. John's Newfoundland and Labrador Canada

3. Department of Earth and Environmental Sciences University of Ottawa Ottawa Ontario

4. Department of Geosciences The University of Rhode Island Kingston Rhode Island USA

5. Department of Earth and Environmental Sciences Tulane University New Orleans Louisiana USA

6. Department of Applied Geology and Geophysics Deltares Utrecht Netherlands

7. Department of Physics University of Toronto Toronto Ontario Canada

8. Department of Sea Level Research Department of Marine and Coastal Sciences Rutgers New Brunswick, New Jersey USA

9. Earth Observatory of Singapore Asian School of the Environment, Nanyang Technological University Singapore

Funder

Past Global Changes

Natural Sciences and Engineering Research Council of Canada

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),General Environmental Science

Reference236 articles.

1. Origin and evolution of Sabine Lake, Texas‐Louisiana;Anderson J. B.;Gulf Coast Assoc. Geol. Soc. Trans.,1991

2. Andrews P. B.(1967) Facies and genesis of a hurricane washover fan St. Joseph island central Texas coast Ph.D. thesis.

3. Preliminary archaeological investigations at Ray Hole Spring in the eastern Gulf of Mexico;Anuskiewicz R. J.;Fla. Anthropol.,1988

4. Arendt A. et al.(2014) Randolph Glacier Inventory – A Dataset of Global Glacier Outlines: Version 3.2. Global Land Ice Measurements from Space.

5. Late Quaternary relative sea-level change in the western Gulf of Maine: Evidence for a migrating glacial forebulge

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