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High Wind Drag Coefficient and Sea Surface Roughness in Shallow ...

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We would hope to obta<strong>in</strong> > 10 profiles over l<strong>and</strong> to substantiate the differences with onshore<br />

flow over shallow water <strong>and</strong> open ocean flow over deep water <strong>in</strong> the MBL group. However,<br />

sondes are not permitted to be launched over l<strong>and</strong> so it is rare that such profiles are available<br />

(apparently the <strong>in</strong>l<strong>and</strong> sondes shown here were advected <strong>in</strong>l<strong>and</strong> from offshore or from a bay/<br />

sound (e.g. Onslow Bay, Pamlico Sound, Lake Ponchartra<strong>in</strong>).<br />

C. Rema<strong>in</strong><strong>in</strong>g work<br />

1. Open-ocean deep water profiles<br />

The database will be queried to remove the shallow water data from the open ocean profiles to<br />

better contrast the differences between onshore flow over shallow water <strong>and</strong> open ocean flow<br />

over deep water. Data will be QC’s accord<strong>in</strong>g to process<strong>in</strong>g QC flags, number of samples per<br />

b<strong>in</strong>, st<strong>and</strong>ard error of the b<strong>in</strong> mean, <strong>and</strong> outliers.<br />

2. <strong>Shallow</strong> water profiles<br />

The rema<strong>in</strong>der of the shallow water MBL groups will be analyzed to develop mean w<strong>in</strong>d profiles.<br />

Data will be QC’s accord<strong>in</strong>g to process<strong>in</strong>g QC flags, number of samples per b<strong>in</strong>, st<strong>and</strong>ard<br />

error of the b<strong>in</strong> mean, <strong>and</strong> outliers. Based on experience with the 30-39 m/s MBL group, only<br />

the 20-29 <strong>and</strong> 40-49 MBL groups are expected to have sufficient data to construct mean profiles<br />

to determ<strong>in</strong>e surface layer roughness length, friction velocity, <strong>and</strong> drag coefficient.<br />

3. Analysis<br />

Student’s t tests will be conducted to determ<strong>in</strong>e whether the b<strong>in</strong> means of the shallow <strong>and</strong> deep<br />

water profiles come from different populations. <strong>Surface</strong> layer parameters <strong>and</strong> associated error<br />

bars will be computed from least squares fits of the profiles <strong>and</strong> compared as a function of w<strong>in</strong>d<br />

speed for deep <strong>and</strong> shallow water. Analysis of covariance will be used to exam<strong>in</strong>e the slopes <strong>and</strong><br />

<strong>in</strong>tercepts of the mean log w<strong>in</strong>d profiles <strong>and</strong> determ<strong>in</strong>e whether differences exist between the<br />

shallow <strong>and</strong> deep water profiles. Prelim<strong>in</strong>ary results will be presented at the Interdepartmental<br />

Hurricane Conference <strong>in</strong> March 2008.<br />

References:<br />

Powell, M. D., 2007: <strong>Drag</strong> <strong>Coefficient</strong> Distribution <strong>and</strong> <strong>W<strong>in</strong>d</strong> Speed Dependence <strong>in</strong> Tropical Cyclones.<br />

F<strong>in</strong>al report to the JHT, April 2007, 26 pp.<br />

Walsh, E. J., others, M. D. Powell, Black, <strong>and</strong> F. D Marks, Jr., 2002: Hurricane directional<br />

wave spectrum spatial variation at l<strong>and</strong>fall. J. Physical Ocean., 32, 1667-1684.<br />

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