{"refrec":{"BRefID":204990,"RR":"<b>D'Asaro, E.; Lee, C.; Rainville, L.; Harcourt, R.; Thomas, L.N.</b> (2011). Enhanced turbulence and energy dissipation at ocean fronts. <i>Science (Wash.) 332(6027)</i>: 318-322. <a href=\"https://dx.doi.org/10.1126/science.1201515\" target=\"_blank\">https://dx.doi.org/10.1126/science.1201515</a>","BEntID":197145,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 332(6027)</i>: 318-322. <a href=\"https://dx.doi.org/10.1126/science.1201515\" target=\"_blank\">https://dx.doi.org/10.1126/science.1201515</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"D'Asaro, E.; Lee, C.; Rainville, L.; Harcourt, R.; Thomas, L.N.","OrigTitleTranslFlag":0,"Authorstringtrunc":"D'Asaro, E. <i>et al.</i>","Englishabstract":"The ocean surface boundary layer mediates air-sea exchange. In the classical paradigm and in current climate models, its turbulence is driven by atmospheric forcing. Observations at a 1-kilometer-wide front within the Kuroshio Current indicate that the rate of energy dissipation within the boundary layer is enhanced by one to  for the turbulence. The data quantitatively support the hypothesis that winds aligned with the frontal velocity catalyzed a release of energy from the front to the turbulence. The resulting boundary layer is stratified in contrast to the classically well-mixed layer. 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