Carbon dioxide, hydrographic, and chemical data obtained during the R/V Meteor Cruise 11/5 in the South Atlantic and Northern Weddell Sea areas (WOCE sections A-12 and A-21)

• Main Authors: Chipman, D. W., Takahashi, T., Breger, D., Sutherland, S. C., Kozyr, A., Gaslightwala, A. F.
• Other Authors: United States. Department of Energy.
• Format: Report
• Language: English
• Published: Oak Ridge National Lab., TN (United States). Carbon Dioxide Information Analysis Center 1994
• Subjects: Oceanic Circulation 540320; Atlantic Ocean; Nitrates; Carbon Dioxide; Chemicals Monitoring And Transport; Silicon Oxides; Sampling; Carbon Cycle; 54 Environmental Sciences; Ecological Concentration; Weddell Sea; Compiled Data; Temperature Measurement; Nitrites; Argentina; Drake Passage; Ushuaia; Weddell; South Atlantic Ocean
• Online Access: https://doi.org/10.2172/10191502; https://digital.library.unt.edu/ark:/67531/metadc1399298/

This document presents the procedures and methods used to obtain carbon dioxide (CO{sub 2}), hydrographic, and chemical data during R/V Meteor Expedition 11/5 in the South Atlantic Ocean, including the Drake Passage; the Northern Weddell Sea; and the Eastern South Atlantic Ocean. This cruise was conducted as part of the World Ocean Circulation Experiment (WOCE). The cruise started from Ushuaia, Argentina, on January 23, 1990, and ended at Capetown, South Africa on March 8, 1990. Samples were collected at 78 stations that covered the Drake Passage; the Northern Weddell Sea; a section along the 58 W parallel; and two segmented S-N sections between the Northern Weddell Sea and Capetown, South Africa. Measurements taken at WOCE sections A-12 and A-21 included pressure, temperature, salinity measured by the Conductivity, Temperature and Depth sensor (CTD); bottle salinity; oxygen; phosphate; nitrate; nitrate; silicate; total carbon concentration (TCO{sub 2}); and partial pressure of CO{sub 2} (pCO{sub 2}) measured at 20 C. In addition, potential density at 0 decibar (dbar) and potential temperature were calculated from the measured variables. The TCO{sub 2} concentration in seawater samples was measured using a coulometer with an estimated precision of approximately {+-} {mu}mol/kg.