Deep Sea Research Part A. Oceanographic Research Papers
Synoptic three-dimensional circulation in an onshore-flowing filament of the California Current
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Evolution and sub-surface characteristics of a sea-surface temperature filament and front in the northeastern Arabian Sea during November-December 2012
2015, Journal of Marine SystemsCitation Excerpt :Hickox et al. (2000) studied SST fronts in East China Sea, Yellow Sea, and Bohai Sea and found the cross-frontal SST range up to 4 °C, with the fronts exhibiting strong seasonal variability in this region. Apart from such high horizontal gradients, upwelling velocities tend to be higher in a frontal regime (Klein and Lapeyre, 2009; Mahadevan and Tandon, 2006) and enhanced vertical mixing and nutrient flux is observed in the filaments and frontal zones (Johnston et al., 2011; Niiler et al., 1989). Observations show that the vertical extent of the Kuroshio front is ~ 100 m (Park and Chu, 2006) and the Agulhas front is mainly a subsurface front, with high horizontal temperature gradients beneath 100–150 m (Belkin and Gordon, 1996).
Temporal and spatial patterns of microbial community biomass and composition in the Southern California Current Ecosystem
2015, Deep-Sea Research Part II: Topical Studies in OceanographyCitation Excerpt :In the southern portion of the CCE Point Conception marks a transition zone, as the primary orientation of the coast line abruptly shifts from north–south to east–west, becoming the northern portion of the Santa Barbara Basin (SBB). A poleward flowing California Undercurrent originates in the eastern tropical Pacific, bringing warm, saline water from offshore and the south and forming the Southern California eddy which is centered approximately near San Nicholas Island (Lynn and Simpson, 1987; Niiler et al., 1989; Bray et al., 1999). The interactions of these currents in the California Bight and offshore regions set up distinct floristic zones, defined by water masses and floral patterns, that can be used to split the region into northern and southern nearshore, and offshore regions (Hayward and Venrick, 1998; Venrick, 2002, 2009).
Statistics from Lagrangian observations
2008, Progress in OceanographyWater masses in the Monterey Bay during the summer of 2000
2007, Continental Shelf ResearchSurface circulation in the central Mediterranean Sea as deduced from Lagrangian drifters in the 1990s
2007, Continental Shelf ResearchA state variable for characterizing water masses and their diffusive stability: Spiciness
2002, Progress in Oceanography