  Air-sea drag governs the momentum transfer between the atmosphere and the
ocean, and remains largely unknown in hurricane winds. We revisit the momentum
budget and eddy-covariance methods to estimate the surface drag coefficient in
the laboratory. Our drag estimates agree with field measurements in
low-to-moderate winds, and previous laboratory measurements in hurricane-force
winds. The drag coefficient saturates at $2.6 \times 10^{-3}$ and $U_{10}
\approx 25\ m\ s^{-1}$, in agreement with previous laboratory results by
Takagaki et al. (2012). During our analysis, we discovered an error in the
original source code used by Donelan et al. (2004). We present the corrected
data and describe the correction procedure. Although the correction to the data
does not change the key finding of drag saturation in strong winds, its
magnitude and wind speed threshold are significantly changed. Our findings
emphasize the need for an updated and unified drag parameterization based on
field and laboratory data.
