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Title: Magdalena%20Andres1,%20Jae-Hun%20Park1,%20Mark%20Wimbush1,


1
Observations of Kuroshio Variability in the East
China Sea
May 24, 2007 The 14th PAMS/JECSS Workshop
  • Magdalena Andres1, Jae-Hun Park1, Mark Wimbush1,
  • Kyung Il Chang2, Hiroshi Ichikawa3
  • 1 Graduate School of Oceanography, University of
    Rhode Island
  • 2 School of Earth and Environmental Sciences,
    Seoul National University
  • 3 Institute of Observational Research for Global
    Change, JAMSTEC

2
Observational highlights of Kuroshio in the ECS
  • Introduce study area and instruments
  • Velocity
  • mean cross-section
  • depth of maximum velocity
  • near-bottom velocity time series
  • Transport
  • mean
  • time series
  • spectrum

3
Study area (Dec. 2002 Nov. 2004)
East China Sea
Near PN-line
4
Study area
East China Sea
Near PN-line
PIES CPIES 23 months
ADCPs 13 months (K.I. Chang)
5
CPIES ( Current- Pressure- sensor-equipped
Inverted Echo Sounder)
  • Emits 12 kHz sound pulses at sea floor
  • Measure (hourly)
  • t echo time from surface
  • P bottom pressure
  • V deep horizontal current
  • Calculate
  • geostrophic shear from t (using dynamic height
    inferred from a lookup table)
  • deep geostrophic flow from P
  • reference deep flow with the current, V
  • ABSOLUTE VELOCITY AND TRANSPORT

6
13-month mean absolute velocity
Cross-section
Schematic Plan view
7
Depth of maximum velocity
Bimodal distribution
53 0.4 2.0 m/s
47 0.3 1.1 m/s
8
Near-bottom velocity
23-month means
C1
C6
9
Transport component
Positive flow,
countercurrent,
recirculation
24.0 Sv
-0.5 Sv
-4.9 Sv
10
Net transport
18.5 Sv
11
Absolute Velocity (m/s)
Net Transport
12
Net transport spectrum
13
Net transport spectrum
  • 11 day
  • James et al., 1999
  • Fastest growing instability spectral model
  • 15 day
  • Johns et al., 2001
  • Inflow east of Taiwan
  • 64 day
  • K.I. Chang, B.-H. Lim, J.-H. Park
  • Related to winds over ECS

14
Summary of Observational highlights
  • Mean velocity cross-section
  • Positive (northeastward flow)
  • Countercurrent (along slope beneath positive
    flow)
  • Recirculation (off-shore of positive flow)
  • Near-bottom velocity
  • Positive flow extends to bottom 50-100 km seaward
    of shelfbreak
  • Persistent countercurrent along slope
  • High frequency variability on the upper slope
  • Transport
  • Mean
  • Net 18.5 Sv (mse 0.8 Sv s 4.0 Sv)
  • Positive 24.0 Sv (mse 0.9 Sv s 4.4 Sv)
  • Recirculation -4.9 Sv (mse 0.3 Sv s 1.8
    Sv)
  • Range in net transport 4 29 Sv
  • Spectral characteristics
  • 64, 15, 11 day peaks in transport

15
Many thanks to the following individuals and
organizations
  • Karen Tracey
  • Gerry Chaplin
  • Capt. Sadao Ishida and the crew aboard the R/V
    Yokosuka of JAMSTEC
  • Capt. Bong-Won Lee and the crew aboard the R/V
    Onnuri of KORDI
  • Capt. Sunao Masumitsu and the crew aboard the T/V
    Kagoshima-maru of Kagoshima University
  • Capt. Jeoung Chang Kim and the crew aboard the
    R/V Tamyang of Pukyong National University
  • CTD data used in the GEM calculations were kindly
    provided by the Nagasaki Marine Observatory,
    Japan Meteorological Agency
  • ONR
  • KORDI
  • JAMSTEC
  • NRL
  • URI/GSO
  • PAMS/JECCS Organizing Committee
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