Joseph Henry LaCasce

Professor

University of Oslo

Norway

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About

Joseph Henry LaCasce is a Professor at the University of Oslo in Norway. His research focuses on ocean circulation, with recent articles exploring topics such as submesoscale energy spectra, the effects of planetary beta and topography on baroclinic instability, and the dynamics of circulation in the Arctic Mediterranean. He is also investigating the implications of climate change on the Atlantic Meridional Overturning Circulation and the role of surface currents in operational oceanography.

Articles (15)

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2025

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2025

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2025

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2025

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2024

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2024

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2023

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2023

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2023

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2023

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2022

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2022

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2021

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2020

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2020

Collaborators (10)

Pål Erik Isachsen

NORWAY

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Sebastian Krumscheid

Karlsruhe Institute of Technology

GERMANY

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Thomas Meunier

assistant professor

FRANCE

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David P. Marshall

UNITED KINGDOM

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Trevor McDougall

University of New South Wales

AUSTRALIA

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Nikki Vercauteren

NORWAY

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Ada Gjermundsen

Norwegian Meteorological Institute

NORWAY

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Bishakhdatta Gayen

Associate Professor

Melbourne Institute, University of Melbourne

AUSTRALIA

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Silje Christine Iversen

UiT The Arctic University of Norway

NORWAY

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Johan Nilsson

Professor

Stockholms Universitet Naturvetenskapliga fakulteten

SWEDEN

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Joseph Henry LaCasce

Research Interests

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About

Articles (15)

The Wind‐Driven Time‐Variable Circulation in the Arctic Mediterranean

Eddy‐ and Wind‐Driven Circulation in the Enclosed Basins of the Norwegian Sea Evaluated Using a Model and Absolute Geostrophic Flow From Argo

The joint effects of planetary $ \boldsymbol{\beta} $ , topography and friction on baroclinic instability in a two-layer quasi-geostrophic model

Inferring Submesoscale Energy Spectra in the Gulf of Mexico from Surface Drifters

The weakening AMOC under extreme climate change

Vortices over bathymetry

Full‐Depth Eddy Kinetic Energy in the Global Ocean Estimated From Altimeter and Argo Observations

Surface currents in operational oceanography: Key applications, mechanisms, and methods

Deep-Reaching Global Ocean Overturning Circulation Generated by Surface Buoyancy Forcing

Prevalence of Deformation‐Scale Surface Currents

Relative dispersion with finite inertial ranges

Dynamical stability indicator based on autoregressive moving-average models: Critical transitions and the Atlantic meridional overturning circulation

The Finite Size Lyapunov Exponent and the Finite Amplitude Growth Rate

Full‐Depth Global Estimates of Ocean Mesoscale Eddy Mixing From Observations and Theory

Baroclinic Modes over Rough Bathymetry and the Surface Deformation Radius

Collaborators (10)

Pål Erik Isachsen

Sebastian Krumscheid

Thomas Meunier

David P. Marshall

Trevor McDougall

Nikki Vercauteren

Ada Gjermundsen

Bishakhdatta Gayen

Silje Christine Iversen

Johan Nilsson

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