Dynamics of Ocean
Currents and Fronts
KESS: US KESS | Mapping Array Highlights | MOVIES | Feature Survey Highlights | Ocean Sciences 2006 2008 2010 | Data | Proposals
The overall goal of the Kuroshio Extension System Study (KESS) is to
identify and quantify the dynamic and
thermodynamic processes governing the variability of and the
interaction between the Kuroshio Extension and the
recirculation gyre. Investigators from three US institutions (University of
Rhode Island, Woods Hole Oceanographic Institution and University of Hawaii)
deployed a state-of-the-art array consisting of moored-profiler and
current-meter moorings and inversted echo sounders equipped with near-bottom
pressure and current sensors
from 2004 to 2006.
KESS array of inverted echo sounders equipped with bottom pressure gauges and current meters (CPIES, diamonds), moored profilers (MPs, stars) equipped with upward-looking acoustic Doppler current profilers (ADCPs) and deep current meters, and KEO surface buoy (triangle). Argo profiling floats were deployed within the green boxed region to measure the temperature and salinity fields. Thin light blue lines indicate Jason 1 ground tracks. Solid lines are the GDEM mean surface dynamic height contours in dyn cm from Teague et al. (1990). The 2000 and 4000 m isobaths are shaded dark and light gray respectively. Eddy kinetic energy > 0.18 and 0.23 m2s-2 is color shaded yellow and orange respectively. CTD/SADCP observations were made at all CPIES sites.
The moored array was designed to measure the time-varying density and velocity fields with the 4-D mesoscale resolution required to determine dynamical balances and cross-frontal exchanges of heat, salt, momentum, and PV. The high-resolution in situ instrument array was centered on the first quasi-stationary meander trough east of Japan, indicated by the GDEM mean surface dynamic height contours (black in above figure). The array was located in the region of highest eddy kinetic energy (yellow and orange shadings).
The in situ observations spanned a two-year period. The instruments were deployed on a cruise aboard the R/V Thompson in Spring 2004 (Deployment Cruise Summary). On a mid-experiment cruise conducted during June-July 2005 aboard the R/V Revelle, the moored profiler moorings were recycled and their data collected. Daily measurements of pressure, travel time and currents were telemetered to the ship from the CPIES and a CTD/ADCP feature survey was conducted. The moored instruments were recovered during May and June 2006 on a cruise aboard the R/V Melville.
Additional information about the KESS cruises, including cruise reports, may be found on the US KESS website under the cruises link.
Satellite altimetry shows the Kuroshio Extension alternates between relatively stable and vigorous meandering intervals on decadal time scales (Qiu and Chen, 2005). The Kuroshio extension transitioned between these two states in fall 2004. SSH fields for the stable period (below left) show two nearly stationary meanders and a westward propagating warm core ring in the KESS region. During the active period (below right), a steep trough develops and a cold core ring forms.
During the stable period (below left), the upper mean streamfunction shows a well-defined KE front and recirculation gyre SW of a mean weak meander trough. Anticyclonic circulation in the deep streamfunction is the deep expression of the southern recirculation gyre. There is weak cross-frontal flow under the trough. During the active period (below right), there is increased meandering which produces weaker lateral gradients across the KE mean front. Both the trough and cold core ring are evident in the mean. Deep features are intensified during the active period.
From May to September 2004 (below left, the green hatched area in SSH (m) time series) a series of rapid, eastward propagating (25-30 km/d) meanders were observed by the CPIES. These short wavelength (160 km) meanders were not resolved by satellite SSH (below right, SSH colors and contours in cm).
A meander trough steepens during December 2004 and pinches off a cold core ring. A movie shows this ring formation in more detail. Deep cyclones and anticyclones move from the northeast to southwest. Upper and deep layers interact and jointly intensify. Deep eddies play an important role in the pinch-off process. Velocity is shown by arrows in cm s-1. SSH is shown by contours (in cm) and color (in dbar), red is high and blue is low. Peak values are -0.25 and 0.25 dbar.
|Movie 1:||Movie 2:||Movie 3:|
|Daily Maps for the two-year
1 June 2004 to 1 May 2006 (82 Mb)
|Daily Maps with superimposed
Argo Float tracks for the two year
period 1 June 2004 to 1 May 2006
|Daily Maps for the period of Ring 04B formation, 15 November 2004 to
31 January 2005 (13 Kb)
KESS is funded by the National Science Foundation under Grant Numbers 0221008 and 0851246.
Disclaimer: Any opinions, findings and conclusions or recomendations expressed in this material are those of the author(s) and do not necessarily reflect the views of the National Science Foundation (NSF).
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