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  • Kuroshio  (2)
  • 162-980A; 162-980B; 162-980C; AGE; Boron/Calcium ratio; Carbonate ion; Date/Time of event; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Half; Isotope ratio mass spectrometry; Joides Resolution; Latitude of event; Leg162; Longitude of event; Ocean Drilling Program; ODP; pH; Sample code/label; South Atlantic Ocean; Standard deviation; δ11B  (1)
  • 2015-2019  (3)
  • 2000-2004
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  • 2015-2019  (3)
  • 2000-2004
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  • 1
    Publication Date: 2024-01-09
    Keywords: 162-980A; 162-980B; 162-980C; AGE; Boron/Calcium ratio; Carbonate ion; Date/Time of event; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Half; Isotope ratio mass spectrometry; Joides Resolution; Latitude of event; Leg162; Longitude of event; Ocean Drilling Program; ODP; pH; Sample code/label; South Atlantic Ocean; Standard deviation; δ11B
    Type: Dataset
    Format: text/tab-separated-values, 383 data points
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  • 2
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2017. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Oceans 122 (2017): 3519–3542, doi:10.1002/2016JC012519.
    Description: Observations from two companion field programs—Origins of the Kuroshio and Mindanao Current (OKMC) and Observations of Kuroshio Transport Variability (OKTV)—are used here to examine the Kuroshio's temporal and spatial evolution. Kuroshio strength and velocity structure were measured between June 2012 and November 2014 with pressure-sensor equipped inverted echo sounders (PIESs) and upward-looking acoustic Doppler current profilers (ADCPs) deployed across the current northeast of Luzon, Philippines, and east of Taiwan with an 8 month overlap in the two arrays' deployment periods. The time-mean net (i.e., integrated from the surface to the bottom) absolute transport increases downstream from 7.3 Sv (±4.4 Sv standard error) northeast of Luzon to 13.7 Sv (±3.6 Sv) east of Taiwan. The observed downstream increase is consistent with the return flow predicted by the simple Sverdrup relation and the mean wind stress curl field over the North Pacific (despite the complicated bathymetry and gaps along the North Pacific western boundary). Northeast of Luzon, the Kuroshio—bounded by the 0 m s−1 isotach—is shallower than 750 dbar, while east of Taiwan areas of positive flow reach to the seafloor (3000 m). Both arrays indicate a deep counterflow beneath the poleward-flowing Kuroshio (–10.3 ± 2.3 Sv by Luzon and −12.5 ± 1.2 Sv east of Taiwan). Time-varying transports and velocities indicate the strong influence at both sections of westward propagating eddies from the ocean interior. Topography associated with the ridges east of Taiwan also influences the mean and time-varying velocity structure there.
    Description: Office of Naval Research (ONR) Grant Numbers: N00014-15-12593 , N00014-16-13069; Taiwan's Ministry of Science and Technology Grant Numbers: NSC 101-2611-M-002-018-MY3 , MOST 103-2611-M-002-011 , MOST 105-2119-M-002-042; ONR Grant Numbers: N00014-10-1-0308 , N00015-10-1-0469
    Description: 2017-11-02
    Keywords: Kuroshio ; PIES ; ADCP ; Eddies ; Western boundary current ; Altimetry
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 3
    Publication Date: 2022-05-25
    Description: Author Posting. © American Geophysical Union, 2015. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 42 (2015): 8098–8105, doi:10.1002/2015GL065814.
    Description: The influence and fate of westward propagating eddies that impinge on the Kuroshio were observed with pressure sensor-equipped inverted echo sounders (PIESs) deployed east of Taiwan and northeast of Luzon. Zero lag correlations between PIES-measured acoustic travel times and satellite-measured sea surface height anomalies (SSHa), which are normally negative, have lower magnitude toward the west, suggesting the eddy-influence is weakened across the Kuroshio. The observational data reveal that impinging eddies lead to seesaw-like SSHa and pycnocline depth changes across the Kuroshio east of Taiwan, whereas analogous responses are not found in the Kuroshio northeast of Luzon. Anticyclones intensify sea surface and pycnocline slopes across the Kuroshio, while cyclones weaken these slopes, particularly east of Taiwan. During the 6 month period of overlap between the two PIES arrays, only one anticyclone affected the pycnocline depth first at the array northeast of Luzon and 21 days later in the downstream Kuroshio east of Taiwan.
    Description: Ministry of Science and Technology (MOST) of Taiwan Grant Number: NSC-101-2611-M-002-018-MY3; US Office of Naval Research (ONR) Grant Number: N00014-12-1-0445; MA Grant Number: N00014-15-1-2593; ONR Grant Numbers: N00014-10-1-0397, N00014-10-1-0308, N00014-10-1-0468
    Description: 2016-03-08
    Keywords: Kuroshio ; Mesoscale eddy ; Eddy-Kuroshio interaction ; Pressure sensor-equipped inverted echo sounder
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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