Abstract
Formation and breaking of internal gravity waves contributing to a very significant increase in turbulence in the atmospheric surface layer over the Atlantic Ocean off Long Island, New York are reported. Contrary to the bursts that are characteristically of short duration, this increase in turbulence lasted for more than one hour and was typical of what one would observe during unstable atmospheric conditions. However, mean temperature profiles indicated strong stable conditions.
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This research was performed under the auspices of the United States Department of Energy Under Contract No. EY-76-C-02-0016.
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Sethuraman, S. A case of persistent breaking of internal gravity waves in the atmospheric surface layer over the ocean. Boundary-Layer Meteorol 19, 67–80 (1980). https://doi.org/10.1007/BF00120311
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DOI: https://doi.org/10.1007/BF00120311