Abstract
In situ data compiled during Cruise 52 of the R/VMikhail Lomonosov in May 1990 have been used to study the space-time variability of the near-surface temperature, with weak wind blowing. Temperature fluctuations within the layer of diurnal warming are shown to be primarily controlled by the heterogeneity of the wind-induced mixing and to be capable of indicating internal waves. The data on the manifestation of internal waves over a bottom rise are submitted, along with the statistical characteristics of temperature fluctuations in a cycle of solar warming.
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Translated by Vladimir A. Puchkin.
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Lebedev, N.E., Pustovoitenko, V.V., Savoskin, V.M. et al. Experimental investigations of the spatial and temporal variability of temperature in the near-surface layer with weak wind blowing. Phys. Oceanogr. 7, 455–460 (1996). https://doi.org/10.1007/BF02509659
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DOI: https://doi.org/10.1007/BF02509659