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Stationary and Traveling Mesoscale Perturbations in the Kuroshio Extension Current
Mesoscale Perturbations Kuroshio Extension Current
2009/2/9
Several hundred XBT observations in the western North Pacific were collected each month over a 2½ year period 1976–78. They have been assembled into a monthly map sequence of thermocline temper...
Horizontal Eddy Fluxes of Momentum and Kinetic Energy in the Near-Surface of the Kuroshio Extension
Horizontal Eddy Fluxes Kuroshio Extension Kinetic Energy
2009/2/7
Sequential monthly-mean temperature fields in the mid-latitude western North Pacific (30–45°N, 140–180°E), constructed from TRANSPAC XBT (expendable bathythermograph) data over a two-year period, are ...
Meridional Eddy Heat Flux in the Kuroshio Extension Current
Eddy Heat Flux Kuroshio Extension Current
2009/2/7
A set of 19 zonal vertical sections of temperature were collected in 1975 with XBT observations at 80 km spacing, made from ships-of-opportunity transiting the mid-latitude North Pacific. In the regio...
Geostrophic Volume Transport in High Eddy-Energy Areas of the Kuroshio Extension and Gulf Stream
Geostrophic Volume Transport High Eddy-Energy Areas Kuroshio Extension Gulf Stream
2009/1/16
Three new deep hydrographic sections taken in July 1980, May 1981 and May 1982, between 29–41°N along 152°E across the high eddy-energy area of the Kuroshio Extension are used to compute the relative ...
Interannual Variability in the Heat Content of the Kuroshio Extension Associated with the 1982 ENSO Event
Interannual Variability Kuroshio Extension Heat Content
2009/1/10
Interannual variability in vertically averaged temperature over the upper 400 m of ocean (i.e., upper ocean heat content) in the vicinity of the Kuroshio Extension experienced significant changes duri...
Zonal Velocity Structure and Transport in the Kuroshio Extension
Zonal Velocity Structure Kuroshio Extension
2009/1/6
The meridional structure of the zonal flow in the Kuroshio Extension is investigated using a combination of data from hydrographic sections and moored current meter arrays. We emphasize 165°E, between...
Eddy Variability in the Kuroshio Extension as Revealed by Geosat Altimetry：Energy Propagation Away from the Jet, Reynolds Stress, and Seasonal Cycle
Exact Repeat Mission Eddy Variability Seasonal Cycle Reynolds Stress
2008/12/30
Altimetric sea level data around the Kuroshio Extension, collected during the first year of the Geosat Exact Repeat Mission (ERM) (starting in November 1986), have been analyzed for energy propagation...
Estimating the Surface Transport of Meandering Oceanic Jet Streams from Satellite Altimetry：Surface Transport Estimates for the Gulf Stream and Kuroshio Extension
Surface Transport Estimates Kuroshio Extension Gulf Stream Oceanic Jet Streams
2008/12/27
A method has been developed to detect the location, width maximum velocity, and suffice transport of a meandering oceanic jet stream from satellite altimetry. Ale method is based on a nonlinear least ...
Energetics of the Kuroshio Extension at 35°N, 152°E
Kuroshio Extension] 35°N, 152°E Energetics
2008/12/24
A simplistic interpretation of eddy heat fluxes from a two-year current meter mooring deployment in the Kuroshio Extension leads to the conclusion that the eddy field is denying at 152°E, contradictin...
Sea Level Differences across the Gulf Stream and Kuroshio Extension
Sea Level Differences Gulf Stream Kuroshio Extension
2008/12/23
Geosat altimetric data for November 1986 to December 1988 are used to estimate sea level differences between the Sargasso Sea and the slope waters across the Gulf Stream region, averaged between 73° a...
Upper-Ocean Heat Balance in the Kuroshio Extension Region
Upper-Ocean Heat Balance Kuroshio Extension Region two-dimensional mixed-layer model
2008/12/19
A horizontally two-dimensional mixed-layer model is used to study the upper-ocean heat balance in the Kuroshio Extension region (30°–40°N, 141°–175°E). Horizontal dependency is emphasized because, in ...
Zonal Jets over Topography on a Beta-Plane, with Applications to the Kuroshio Extension over the Shatsky Rise
Zonal Jets Beta-Plane Kuroshio Extension Shatsky Rise
2008/12/16
The response of an initially zonal barotropic or baroclinic jet to an isolated seamount or a meridional ridge is investigated here using a three-dimensional primitive equation model with a free surfac...
Validation of Gridded Surface Wind Products Using Spaceborne Microwave Sensors and their Application to Air-Sea Interaction in the Kuroshio Extension Region
Surface Wind Gridded product Validation Buoy measurement AMSR Scatterometer
2010/11/23
We have constructed gridded high resolution global surface wind products from satellite scatterometer Qscat/ SeaWinds (QSW) and radiometer Aqua/AMSR-E. Intercomparison of the two products in the North...
Variability and Energetics of the Kuroshio Extension and Its Recirculation Gyre from the First Two-Year TOPEX Data
sea surface height eddy kinetic energy
2008/12/12
Altimetry data from the first 21-month TOPEX mission (September 1992–June 1994) are analysed to investigate the sea surface height (SSH) fluctuations in the Kuroshio Extension and its southern recircu...
Radiating Instability of Nonzonal Oceanic Shear Flows with Application to the Kuroshio Extension Current
Kuroshio Extension Current Nonzonal Oceanic Shear Flows
2008/12/12
This paper proposes a mechanism to explain the fairly energetic internal temperature fluctuations observed in the regions far away from the axis of the Kuroshio Extension Current (KEC). Based upon the...