2018
DOI: 10.1016/j.shpsa.2018.05.004
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Experiencing deep and global currents at a ‘Prototypical Strait’, 1870s and 1980s

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Cited by 5 publications
(1 citation statement)
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“…He immediately proposed to account for circulation with a physical model in which convection and not wind velocity was the main driver. While Carpenter's theory was rejected, his model served as a constraining framework where the behavior of different masses of water was regulated by temperature differentials (Camprubí 2018). It also became clear that salinity enabled identifying water masses and telling them apart from one another, at times despite their physical proximity (for example to identify Mediterranean waters navigating in the North Atlantic).…”
Section: The Example Of Physical Oceanographymentioning
confidence: 99%
“…He immediately proposed to account for circulation with a physical model in which convection and not wind velocity was the main driver. While Carpenter's theory was rejected, his model served as a constraining framework where the behavior of different masses of water was regulated by temperature differentials (Camprubí 2018). It also became clear that salinity enabled identifying water masses and telling them apart from one another, at times despite their physical proximity (for example to identify Mediterranean waters navigating in the North Atlantic).…”
Section: The Example Of Physical Oceanographymentioning
confidence: 99%