This second volume presents basic elements of physical oceanography in relation to the observations of the H.M.S. Challenger. Our approach is built around W.B. Carpenter’s idea, which advocated that the temperature distribution in the ocean was closely related to the world ocean circulation and that it might be possible to have a better understanding of the global currents from an accurate temperature measurement. After a history of underwater temperature measurement techniques, we introduced general concepts of geostrophic flow and developed a simplified model of the thermocline by introducing some original formulations. We concluded with more general notions concerning the wind effect, the water body transport, the coupling between the oceanic layers (OML, geostrophic and bottom boundary layers) and the thermohaline circulation.
We also noted the relevance of the Challenger’s physical observations and particularly the temperature measurements that are very consistent with the proposed models and with more recent oceanographic surveys.
Volume 2 only partially deals with the subject and does not in itself constitute a complete treatise on oceanography. However, its deliberately pedagogical approach to concepts and basic notions and, in addition, the comparison of modeling and experimental results (from Challenger data and the EPIC database) should help students in fluid mechanics and physical oceanography in their study of these disciplines.
Table C.1. Relationships of authors’ model for the thermocline
General equations of motion | [3.20–3.24] |
Equation of state | [3.25bis] |
Characteristic scale of depth | [3.33] |
Vertical velocity at the base | [3.35] |
Temperature at the top | [4.37bis] |
Density evolution equation | [4.39] |
Temperature evolution equation | [4.40] |
Table C.2. Relationships of authors’ model for the OML
Wind stress | [4.27 sphere] |
Vertical velocity at the base | [4.35] |
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