Figure 7. Transect of isopycnal displacement (absolute value in m) calculated from a 6â7 hr repeat transect across the canyon channel 4 km downstream of the ROV dive site.The southern side of the canyon (where the A. excavata-N. pycnodonte biotope was found) is on the right side of the figure. A scale is shown to the right, CTD locations by âxâ and the seabed by the black line. The parallel white lines across the transect indicate a possible beam of high isopycnal displacement associated with an internal wave emanating from the northern canyon wall.
Image published in: Johnson MP et al. (2013)
Image downloaded from an Open Access article in PubMed Central. © 2013 Johnson et al
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