Fig. 1: Map over the study area and temperature sections. | Nature Communications

Fig. 1: Map over the study area and temperature sections.

From: Observational evidence for on-shelf heat transport driven by dense water export in the Weddell Sea

Fig. 1

Temperature sections a west and b east of the Filchner Trough (purple/green line in c, respectively). The divergent colormap highlights the depth of the thermocline, with Winter Water above (in blue) and (modified) Warm Deep Water below (in red). c Map over the study area with bathymetry27 in blue shading according to the color bar and the 500 m isobath highlighted in black. The circulation in the area is shown with blue (outflow of Ice Shelf Water) and red (the Antarctic Slope Current and the Antarctic Coastal Current) arrows34,35. Dashed arrows indicate seasonal flow35,36. Floating ice shelves are shown in dark gray and land in light gray. The location of Conductivity-Temperature-Depth (CTD) stations on the continental slope is marked with white dots. FT indicates the Filchner Trough, and FIS is the Filchner Ice Shelf. d Mean current from moorings listed in Table 1. Currents observed within the dense plume are shown in blue, and currents observed above/outside the plume are shown in red. The black arrow on the shelf gives the velocity scale. Note that there is a factor three difference between the blue and red scales. Isobaths are shown every 250 m with the 500 m isobath in bold, and the area is marked with a red rectangle in d. e A map showing the location of the study area in the southwestern Weddell Sea (red square).

Back to article page