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  • Aircraft measurements  (1)
  • Eddy-Kuroshio interaction  (1)
  • Mesoscale eddy  (1)
  • 1
    Publication Date: 2022-05-25
    Description: Field observations of the ocean's forced stage response to three hurricanes, Norbert (1984), Josephine (1984) and Gloria (1985), are analyzed and presented in a storm-centered coordinate system. All three hurricanes had a non-dimensional speed of O(1) and produced a strongly rightward biased response of the ocean surface mixed layer (SML) transport and current. The maximum layer-averaged SML currents varried from 0.8 m S-1 in response to Josephine, which was a fairly weak hurricane, to 1.7 m S.l in response to Gloria, which was much stronger. In these two cases the current amplitude is set primarly by the strength of the wind stress and its efficiency of coupling with the SML current, and the depth of vertical mixing of the SML. The Norbert case (SML Burger number ≈ 1/2) was also affected by significant pressure-coupling with the thermocline that caused appreciable upwellng by inertial pumping and strong thermocline-depth currents, up to 0.3 m S-l, under the trailing edge of Norbert. The observed SML current has a vertical shear in the direction of the local wind of up to 0.01 S-l. This vertical shear causes the surface current to be larger than the layer-averaged SML current described above by typically 0.2 m S.l.
    Description: Funding was provided by the Office of Naval Research under grant No. N00014-89-J-I053.
    Keywords: Ocean models ; Wind-driven currents ; Aircraft measurements
    Repository Name: Woods Hole Open Access Server
    Type: Technical Report
    Format: 3034212 bytes
    Format: application/pdf
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  • 2
    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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