Ken Zhao

Ken Zhao
Oregon State University | OSU · College of Earth, Ocean and Atmospheric Sciences

Doctor of Philosophy

About

5
Publications
480
Reads
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19
Citations
Citations since 2016
5 Research Items
19 Citations
20162017201820192020202120220246810
20162017201820192020202120220246810
20162017201820192020202120220246810
20162017201820192020202120220246810
Introduction
Ken Zhao currently works at the Department of Atmospheric and Oceanic Sciences (AOS), University of California, Los Angeles. Ken does research in Physical Oceanography, with a focus on ice-ocean interactions.

Publications

Publications (5)
Article
Glacial fjord circulation modulates the connection between marine-terminating glaciers and the ocean currents offshore. These fjords exhibit a complex 3D circulation with overturning and horizontal recirculation components, which are both primarily driven by water mass transformation at the head of the fjord via subglacial discharge plumes and dist...
Article
Full-text available
Plain Language Summary Glacial fjords are long, narrow, and deep inlets that connect glaciers to the open ocean. These glacial fjords exist around the margins of Greenland, West Antarctica, Alaska, and other regions, and collectively contribute a significant source of ice discharge into the ocean. Over the past two decades, tidewater glaciers in Gr...
Article
Full-text available
Interaction between the atmosphere and ocean in sea ice-covered regions is largely concentrated in leads, which are long, narrow openings between sea ice floes. Refreezing and brine rejection in these leads injects salt that plays a key role in maintaining the polar halocline. The injected salt forms dense plumes that subsequently become baroclinic...
Article
Full-text available
The oceanic connections between tidewater glaciers and continental shelf waters are modulated and controlled by geometrically complex fjords. These fjords exhibit both overturning circulations and horizontal recirculations, driven by a combination of water mass transformation at the head of the fjord, variability on the continental shelf, and atmos...
Article
Full-text available
Bathymetric sills are important features in the ocean-filled cavities beneath a few fast-retreating ice shelves in West Antarctica and northern Greenland. The sills can be high enough to obstruct the cavity circulation and thereby modulate glacial melt rates. This study focuses on the idealized problem of diabatically-driven, sill-constrained overt...

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Projects

Projects (2)
Project
To understand the factors influencing circulation and heat transport from fjords to shelf waters in Greenland.