Detection of a dynamic topography signal in last interglacial sea-level records-Reference-Cited by-同舟云学术

Detection of a dynamic topography signal in last interglacial sea-level records

Author:

Austermann Jacqueline¹²^ORCID,Mitrovica Jerry X.²,Huybers Peter²^ORCID,Rovere Alessio³⁴

Affiliation:

1. Department of Earth Sciences, University of Cambridge, Cambridge, UK.

2. Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138, USA.

3. MARUM–Center for Marine Environmental Sciences, University of Bremen, Leobener Straße, 28359 Bremen, Germany.

4. ZMT, Leibniz Centre for Tropical Marine Research, Fahrenheitstraße 6, 28359 Bremen, Germany.

Abstract

Topographic changes due to mantle convection affected the elevation of last interglacial sea-level records across the globe.

Funder

Division of Ocean Sciences

Division of Atmospheric and Geospace Sciences

Royal Society

German Excellence Initiative

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference69 articles.

1. Paleo constraints on future sea-level rise;Kemp A. C.;Curr. Clim. Change Rep.,2015

4. Probabilistic assessment of sea level during the last interglacial stage;Kopp R. E.;Science,2009

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