SOUTH ATLANTIC OCEAN (4)
CTD (4)
Attribution-ShareAlike 4.0 International (CC BY-SA 4.0) (5)
Physics > Subsurface salinity (8)
Physics > Subsurface temperature (8)
The Current Meter and Sediment Trap Recovery Shelf Chemistry on the Africana Voyage 114, June 1993 was conducted from 21 June 1993 to June 30 1993. The main objectives of the cruise were to recover and redeploy the inshore time series current meter array deployed in 168m off Cape Columbine. To locate and attempt recovery of the inshore current meter deployed in 132m off Hondeklip Bay; to locate and attempt recovery of the offshore current meter sediment trap array deployed in 686m off Hondeklip Bay; to attempt location and recovery of the offshore current meter array deployed in 278m off Cape Columbine. To conduct research into the shelf geochemistry on a line off Hondeklip Bay and, if time, in St Helena Bay and to conduct a survey of nearshore dissolved oxygen in the vicinity of Port Nolloth to link in with research on Namagualand stocks being undertaken by the Rock Lobster section.
Here we present processed Conductivity-Temperature-Depth (CTD) discrete data from the upcast collected, between 21 June and 30 June 1993, during voyage 114 in the Benguela Current Large Marine Ecosystem (BCLME) region on the west coast of Southern Africa. Neil Brown MK3 and MK4 CTD instruments were used to measure pressure, temperature and conductivity through the water column during research and monitoring cruises between 1983 and 2000.
Here we present processed downcast Conductivity-Temperature-Depth (CTD) continuous data collected, between 21 June and 30 June 1993, during the Current Meter and Sediment Trap Recovery Shelf Chemistry on the Africana Voyage 114, in the Benguela Current Large Marine Ecosystem (BCLME) region on the west coast of Southern Africa. Neil Brown MK3 and MK4 Conductivity-Temperature-Depth (CTD) instruments were used to measure pressure, temperature and conductivity through the water column during research and monitoring cruises between 1983 and 2000.
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