Clinton Conrad

Professor

University of Oslo

Norway

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About

Clinton Conrad is a Professor at the University of Oslo, Norway. His research focuses on seismic anisotropy, solid earth structure, and mantle dynamics, with significant contributions to understanding the evolution of the Greenland ice sheet and global sea-level changes. His recent work explores topics including mantle flow, water distribution in the lower mantle, and the effects of ice melt on geological uplift in Southeast Greenland.

Articles (18)

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2025

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Valentina Roberta Barletta

Technical University of Denmark

DENMARK

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Grace Shephard

Honorary Senior Lecturer

Australian National University

AUSTRALIA

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Ana Ferreira

Reader (Associate Professor) in Seismology

University College London

UNITED KINGDOM

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Clinton Conrad

Research Interests

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About

Articles (18)

Importance of solid earth structure for understanding the evolution of the Greenland ice sheet

Evaluating IPCC Projections of Global Sea‐Level Change From the Pre‐Satellite Era

Depth-dependent azimuthal seismic anisotropy governed by Couette/Poiseuille flow partitioning in the asthenosphere

Mantle Flow and Anisotropy in Subduction Zones: Modeling and Clustering of Olivine Textures

Hydrous Regions of the Mantle Transition Zone Lie Beneath Areas of Continental Intraplate Volcanism

Lower mantle water distribution from ab initio proton diffusivity in bridgmanite

Recent ice melt above a mantle plume track is accelerating the uplift of Southeast Greenland

Prolonged Multi‐Phase Magmatism Due To Plume‐Lithosphere Interaction as Applied to the High Arctic Large Igneous Province

Grain size reduction by plug flow in the wet oceanic upper mantle explains the asthenosphere's low seismic Q zone

Modeling Viscoelastic Solid Earth Deformation Due To Ice Age and Contemporary Glacial Mass Changes in ASPECT

Convective Self‐Compression of Cratons and the Stabilization of Old Lithosphere

Solid Earth Uplift Due To Contemporary Ice Melt Above Low‐Viscosity Regions of the Upper Mantle

Constraining Upper Mantle Viscosity Using Temperature and Water Content Inferred From Seismic and Magnetotelluric Data

On the Relation Between Basal Erosion of the Lithosphere and Surface Heat Flux for Continental Plume Tracks

Spatiotemporal Variations in Surface Heat Loss Imply a Heterogeneous Mantle Cooling History

Evolving Viscous Anisotropy in the Upper Mantle and Its Geodynamic Implications

Core-mantle boundary topography and its relation to the viscosity structure of the lowermost mantle

How Thermochemical Piles Can (Periodically) Generate Plumes at Their Edges

Collaborators (8)

John Naliboff

Timo Heister

Sönke Dangendorf

Valerie Maupin

Thorsten W. Becker

Valentina Roberta Barletta

Grace Shephard

Ana Ferreira

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