Distribution of deep near-inertial waves observed in the Kuroshio Extension
The distribution of deep near-inertial waves (NIWs) is investigated using data mainly from an array of 46 near-bottom acoustic current meter sensors spanning a 600 km × 600 km region as part of the Kuroshio Extension System Study during 2004–2006. The deep NIW distribution is interpreted in the context of both upper-layer and near-bottom mapped circulations. The wintertime-mean mixed-layer NIW energy input, modeled from observed wind stress, has the same range of values north and south of the Kuroshio Extension in this region. Yet, the wintertime-mean deep NIW energy distribution reveals a sharp factor-of-5 decrease from north to south of the Kuroshio jet. This direct observational evidence shows that the Kuroshio Extension blocks the equatorward propagation of NIWs. The NIW energy that does reach the sea floor within the subset of wintertime observations in the subtropical gyre arrives with patchy spatial and temporal distribution. Elevated NIW energy in deep water is associated with anticyclones in the deep barotropic flow and unassociated with upper layer eddies.
KeywordsNear-inertial wave Kuroshio acoustic current meter inverted echo sounder deep eddies Kuroshio Extension System Study
Unable to display preview. Download preview PDF.
- Garrett, C. (2001): What is the “Near-Inertial” band and why is it different from the rest of the internal wave spectrum. J. Phys. Oceanogr., 31, 727–742.Google Scholar
- Kennelly, M., K. Donohue, A. Greene, K. L. Tracey and D. R. Watts (2008): Inverted echo sounder data report: Kuroshio Extension System Study (KESS), April 2004 to July 2006. GSO Tech. Rep. 2008-02, Graduate Sch. of Oceanogr., Univ. of R. I., Narragansett (available at http://www.po.gso.uri.edu/dynamics/publications/tech_rpts/KESSdatareport.pdf).