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Kim I. Martini

Researcher at University of Alaska Fairbanks

Publications -  14
Citations -  548

Kim I. Martini is an academic researcher from University of Alaska Fairbanks. The author has contributed to research in topics: Internal wave & Internal tide. The author has an hindex of 10, co-authored 14 publications receiving 418 citations. Previous affiliations of Kim I. Martini include University of Washington & Pacific Marine Environmental Laboratory.

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Hotspots of deep ocean mixing on the Oregon continental slope

TL;DR: In this article, two deep ocean hotspots of turbulent mixing were found over the Oregon continental slope, and Thorpe-scale analyses indicate time-averaged turbulent energy dissipation rates of e > 10−7 W/kg and eddy diffusivities of Kρ ∼ 10−2 m2/s at both hotspots.
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Argo Data 1999–2019: Two Million Temperature-Salinity Profiles and Subsurface Velocity Observations From a Global Array of Profiling Floats

Annie P. S. Wong, +101 more
TL;DR: The history of the global Argo Program, from its aspiration arising out of the World Ocean Circulation Experiment, to the development and implementation of its instrumentation and telecommunication systems, and the various technical problems encountered, is described in this article.
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Observations of Internal Tides on the Oregon Continental Slope

TL;DR: In this paper, a 40-day moored deployment spans three spring and two neap tides, during which the proportions of the locally and remotely forced internal tides vary vary, and energy flux exhibits complex spatial and temporal patterns throughout both tidal periods.
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The Cascade of Tidal Energy from Low to High Modes on a Continental Slope

TL;DR: In this paper, a theoretical framework for low-wavenumber energy transfer is derived from "flat bottom" vertical modes and evaluated with observations from the Oregon continental slope, where local tidal dynamics are modeled with a superposition of two idealized numerical simulations, one forced by local surface-tide velocities and the other by an obliquely incident internal tide generated at the Mendocino Escarpment 315 km southwest of the study site.
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Diagnosing a partly standing internal wave in Mamala Bay, Oahu

TL;DR: In this article, an internal standing wave in Mamala Bay, Hawaii is studied using new observations and the Princeton Ocean Model (POM) using new energy flux measurements with shipboard ADCP/CTD confirm that Makapuu Point is the eastern source.