The authors use data collected by a line of tall current meter moorings deployed across the axis of the Kuroshio Extension (KE) jet at the location of maximum time-mean eddy kinetic energy to characterize the mean jet structure, the eddy variability, and the nature of eddy–mean flow interactions observed during the Kuroshio Extension System Study (KESS). A picture of the 2-yr record mean jet structure is presented in both geographical and stream coordinates, revealing important contrasts in jet strength, width, vertical structure, and flanking recirculation structure. Eddy variability observed is discussed in the context of some of its various sources: jet meandering, rings, waves, and jet instability. Finally, various scenarios for eddy–me...
Eddy momentum fluxes, i.e. Reynold stresses, are computed for the latitude bands of the Gulf Stream ...
Using altimeter data from the Geosat Exact Repeat Mission (ERM), we investigated the mean flow and t...
The Princeton ocean model is employed to study the energy balance of a fast-moving anticyclonic eddy...
Author Posting. © American Meteorological Society, 2011. This article is posted here by permission ...
The Kuroshio current is the western boundary current (WBC) of the North Pacific. It flows north from...
Author Posting. © American Meteorological Society, 2015. This article is posted here by permission ...
Thesis (Ph. D.)--Joint Program in Physical Oceanography (Massachusetts Institute of Technology, Dept...
20 pages, 19 figures, 1 appendixThe Kuroshio Extension region is well known for its strong eddy acti...
Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the M...
A theoretical study on the role of eddy-mean flow interactions in the time-mean dynamics of a zonall...
This paper reports on the strength and structure of the Kuroshio Extension and its recirculation gyr...
The Kuroshio Extension (KE) is the eastward-flowing, free, inertial meandering jet formed by the con...
High spatial resolution isopycnal diffusivities are estimated in the Kuroshio Extension (KE) region ...
Being the extension of a wind-driven western boundary current, the Kuroshio Extension (KE) has long ...
A three-dimensional primitive equations ocean model (POM) is employed to study the momentum and ener...
Eddy momentum fluxes, i.e. Reynold stresses, are computed for the latitude bands of the Gulf Stream ...
Using altimeter data from the Geosat Exact Repeat Mission (ERM), we investigated the mean flow and t...
The Princeton ocean model is employed to study the energy balance of a fast-moving anticyclonic eddy...
Author Posting. © American Meteorological Society, 2011. This article is posted here by permission ...
The Kuroshio current is the western boundary current (WBC) of the North Pacific. It flows north from...
Author Posting. © American Meteorological Society, 2015. This article is posted here by permission ...
Thesis (Ph. D.)--Joint Program in Physical Oceanography (Massachusetts Institute of Technology, Dept...
20 pages, 19 figures, 1 appendixThe Kuroshio Extension region is well known for its strong eddy acti...
Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the M...
A theoretical study on the role of eddy-mean flow interactions in the time-mean dynamics of a zonall...
This paper reports on the strength and structure of the Kuroshio Extension and its recirculation gyr...
The Kuroshio Extension (KE) is the eastward-flowing, free, inertial meandering jet formed by the con...
High spatial resolution isopycnal diffusivities are estimated in the Kuroshio Extension (KE) region ...
Being the extension of a wind-driven western boundary current, the Kuroshio Extension (KE) has long ...
A three-dimensional primitive equations ocean model (POM) is employed to study the momentum and ener...
Eddy momentum fluxes, i.e. Reynold stresses, are computed for the latitude bands of the Gulf Stream ...
Using altimeter data from the Geosat Exact Repeat Mission (ERM), we investigated the mean flow and t...
The Princeton ocean model is employed to study the energy balance of a fast-moving anticyclonic eddy...