Experiencing deep and global currents at a 'Prototypical Strait', 1870s and 1980s

Deep ocean currents are not accessible to direct human perception. Their insertion into global structures of circulation is even more profoundly removed from individual sensorial experience. But oceanographers tend to use wider concepts of experience to include instruments, traditions of observation and theoretical models. Historians and philosophers of science, as well as STS scholars, have also redefined scientific experience as operational and collective transformations of parts of the world around us into fragments of larger bodies of knowledge. This paper pursues this definition to follow the instrumental and epistemological resources available to those "observing" deep-water circulation at the Strait of Gibraltar in two very distinct moments, ca. 1870 and ca. 1985, respectively through the works of scientists like William B. Carpenter and the transnational team involved in the Gibraltar Experiment. Detecting and mapping the Gibraltar undercurrent necessitated taking data of temperature and salinity as proxies for masses of water. Making it relevant to world ocean currents required the use of models and moving across scales. In both contexts, empires of global reach provided the globalizing motivations and infrastructures.