. TRINITY PENIN^ Fig. 11. Vertical section of salinity: Livingston Island to Trinity Peninsula, April 1927. STATION 202 LIVINGSTON 1. 0-0° 203 204 205 206 -0-5° TRINITY PENIN* \ >oo°: 0 0' 1 — -n-s° ' i ~~ 1 , _^y — h0°. L_ / 500m- ^___y -"27-70 V 2780 — Fig. 13. Vertical section of density (<r,): Livingston Island to Trinity Peninsula, April 1927. traces of warm deep water inside the strait the water is formed from the dense water of Weddell Sea origin which mixes with the surface water in the remainder of the strait and in winter is rendered more saline by the removal of water in
. TRINITY PENIN^ Fig. 11. Vertical section of salinity: Livingston Island to Trinity Peninsula, April 1927. STATION 202 LIVINGSTON 1. 0-0° 203 204 205 206 -0-5° TRINITY PENIN* \ >oo°: 0 0' 1 — -n-s° ' i ~~ 1 , _^y — h0°. L_ / 500m- ^___y -"27-70 V 2780 — Fig. 13. Vertical section of density (<r,): Livingston Island to Trinity Peninsula, April 1927. traces of warm deep water inside the strait the water is formed from the dense water of Weddell Sea origin which mixes with the surface water in the remainder of the strait and in winter is rendered more saline by the removal of water in the form of ice. The more saline water then sinks to form the bottom water.
Size: 3298px × 1515px
Photo credit: © The Bookworm Collection / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: ., bookcentury1900, booksubjectocean, booksubjectscientificexpediti
