Unfortunately, the strong intraseasonal variability of the AMOC revealed by the RAPID / MOCHA array seriously constrains our ability to recreate AMOC variability over the modern observational period, since synoptic
hydrographic sections are the
Not exact matches
In this paper, we examine the causes of the observed sea level rise in the region south of Australia, using 13 years of repeat
hydrographic data from the WOCE SR3
sections, and the SURVOSTRAL XBT and surface salinity data.
• To determine full water column distributions of selected trace elements and isotopes, including their concentration, chemical speciation, and physical form, along a sufficient number of
sections in each ocean basin to establish the principal relationships between these distributions and with more traditional
hydrographic parameters;