Kohei Mizobata
Kohei Mizobata
Polar oceanography / Satellite oceanography

Kohei Mizobata

I study ocean circulation, heat transport, and ice–ocean–sea ice interactions in polar oceans, with a particular focus on East Antarctica. My research combines satellite remote sensing, ship-based observations, mooring observations, and data analysis to understand how ocean heat reaches Antarctic continental shelves and ice-shelf cavities.

East Antarctica Southern Ocean Satellite altimetry Dynamic ocean topography Ocean heat transport Ice-shelf melting Sea ice In situ observations

Research Overview

My research addresses how relatively warm offshore waters are transported toward the Antarctic continental shelf and eventually into ice-shelf cavities. Around the Totten and Cook ice-shelf sectors in East Antarctica, this oceanic heat transport is a key process linking offshore ocean circulation, coastal dynamics, and ice-sheet change.

A major focus is the role of mesoscale eddies, the Antarctic Slope Current and Antarctic Slope Undercurrent, coastal gyres, shelf-break topography, and large-scale atmospheric variability such as the Southern Annular Mode. I use satellite-derived sea level and dynamic ocean topography together with hydrographic and velocity observations to diagnose these processes.

Main research themes
Ocean heat transport toward East Antarctic ice shelves

Satellite remote sensing of polar ocean circulation

Ice–ocean–sea ice interactions in the Southern Ocean

Antarctic coastal marine heatwaves and upper-ocean variability

Selected Research Topics

East Antarctic heat transport

Observational and satellite-based studies of how warm water is transported from offshore basins to the continental shelf and ice-shelf fronts.

Dynamic ocean topography

Development and application of satellite-altimeter-based dynamic ocean topography fields to infer polar ocean circulation, including sea-ice-covered regions.

Coastal variability

Analysis of how atmospheric variability, coastal sea level, gyres, eddies, and shelf-slope currents modulate poleward heat transport.

Research Context

Schematic overview of ocean heat transport toward Antarctic ice shelves

Ocean circulation transports warm water from offshore basins to the continental shelf and into ice-shelf cavities, where ocean heat can control basal melting.

Data Sharing

Research datasets distributed by Kohei Mizobata are available from the data-sharing page. The datasets include upper-ocean XCTD profiles used for reproducibility of Antarctic coastal marine heatwave analysis and ADS-registered monthly dynamic ocean topography datasets derived from satellite radar altimeters.

CV / Profile Links

Please see the following external profiles for publications, research projects, and researcher identifiers.

Contact

Affiliation Tokyo University of Marine Science and Technology
Department of Ocean Sciences, School of Marine Resources and Environment
Address 4-5-7 Konan, Minato-ku, Tokyo 108-8477, Japan

Office Building 9, Room 605