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Kenneth G. Hughes, James N. Moum, and Emily L. Shroyer

better resolved vertically. Much of our analysis focuses on the GusTs, which were at depths of 0.4, 1.7, 4.2, and 7.7 m. Fast thermistor measurements are continuous for whole deployments. For turbulence calculations, we segment these into 10-min blocks. With each block, we first convert T t to an equivalent horizontal gradient T x = T t / U where U is the 10-min mean flow speed past the sensor. We then calculate the dissipation of thermal variance χ by fitting T x spectra to a theoretical

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