From November 2 to 5, 1996, an intense extratropical cyclone was near the National Data Buoy Center buoy 46035 in the Bering Sea. At the storm's extremes, the buoy measured minimum sea-level pressure (= 966.1 mbar), 10 m wind speed (= 28.2 m/s), peak gust (= 38.9 m/s), significant wave height (= 15.4 m), and peak period (= 16.7 s). During this period, 41 hourly observations were recorded when the waves were not fully developed; these records are the subject of our detailed analysis. It is shown that the wind–pressure relation was governed by the cyclostrophic equation; stability was neutral (i.e., the logarithmic wind profile law is useful); the relation between dimensionless wave height and period as normalized by the wind speed and the friction velocity follows the formulas found in the literature. Further determination of the friction velocity using the gust factor concept is successful to incorporate both tropical and extratropical cyclones.