Glider observations of the North Equatorial Current in the western tropical Pacific

TitleGlider observations of the North Equatorial Current in the western tropical Pacific
Publication TypeJournal Article
Year of Publication2015
AuthorsSchonau M.C, Rudnick D.L
JournalJournal of Geophysical Research-Oceans
Date Published2015/05
Type of ArticleArticle
ISBN Number2169-9275
Accession NumberWOS:000356628100023
Keywordsinterannual; intermediate water; mindanao current; north equatorial current; philippine coast; potential vorticity field; sea-surface salinity; spice variance; subtropical mode water; undercurrent jets; Underwater glider; underwater gliders; upper-ocean; variability

The North Equatorial Current (NEC) of the Pacific Ocean advects subtropical, subpolar, and tropical water masses. Repeat underwater glider observations of the NEC from June 2009 to January 2014 along 134.3 degrees E provide absolute zonal geostrophic velocity, transport, and water mass structure at length scales of 10-1000 km. The NEC is strongest near the surface and persistent eastward undercurrents are identified deeper than potential density surface 26 kg m(-3) at 9.6 degrees N and 13.1 degrees N. Mean transport from the surface to 27.3 kg m(-3) and 8.5 degrees N-16.5 degrees N is 37.6 Sv (10(6) m(3) s(-1)), with a standard deviation of 15.6 Sv. The transport variability is greatest deeper than 26 kg m(-3) due to undercurrent variability. Wavelet analysis at scales of 10-80 km reveals extrema of fine-scale salinity variance along isopycnals (spice variance). High spice variance is found in the North Pacific Tropical Water (NPTW) and the North Pacific Intermediate Water (NPIW), with a spice variance minimum between water masses at 25.5 kg m(-3). A horizontal Cox number, C-H, relates salinity variance at fine scales (10-80 km) to that at greater length scales (120-200 km). As a function of density, C-H is nearly vertically uniform, indicating that the stirring of mean salinity gradients enhances fine-scale salinity variance. NPTW, with an estimated horizontal eddy diffusivity of order 10(4) m s(-2), is a useful tracer for the region and may be used to relate the fine-scale salinity variance to an eddy diffusivity.

Short TitleJ Geophys Res-Oceans
Student Publication: