Abstract
Spatial coherence and phase relationships of inertial-period motions have been inferred from an experiment with four moorings in the northern North Sea where the density profile was almost two-layered. The inertial-period currents showed antiphase between the upper and lower layers; the coherence between both layers was high. The inertial-period temperature fluctuations were in phase throughout the thermocline.
Recommended Citation
Schott, Friedrich. 1971. "Spatial structure of inertial-period motions in a two-layered sea, based on observations." Journal of Marine Research 29, (2). https://elischolar.library.yale.edu/journal_of_marine_research/1204
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