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LIEN AND SANFORD: SPECTRA OF VELOCITY AND VORTICITY FLUXES 12<br />

the sensor size must be smaller th<strong>an</strong> the scales <strong>of</strong> the<br />

<strong>fluxes</strong>. Because the scale <strong>of</strong> the dom<strong>in</strong><strong>an</strong>t <strong>vorticity</strong> flux<br />

is smaller th<strong>an</strong> the scale <strong>of</strong> the dom<strong>in</strong><strong>an</strong>t momentum<br />

flux, a sensor’s scale may be small enough to measure<br />

the momentum flux, but not sufficiently small to measure<br />

the <strong>vorticity</strong> flux.<br />

We def<strong>in</strong>e the fractions <strong>of</strong> momentum flux <strong><strong>an</strong>d</strong> <strong>vorticity</strong><br />

flux that are resolved as a function <strong>of</strong> wavenumbers<br />

as<br />

R uw (k x ) =<br />

R wζy (k x ) =<br />

∫ kx<br />

0<br />

dk x P uw<br />

∫ ∞<br />

0<br />

dk x P uw<br />

, (B1)<br />

∫ kx<br />

0<br />

dk x P wζy<br />

∫ ∞<br />

0<br />

dk x P wζy<br />

. (B2)<br />

On the basis <strong>of</strong> the empirical momentum flux spectrum<br />

<strong>of</strong> Kaimal et al. [1972] <strong><strong>an</strong>d</strong> our proposed <strong>vorticity</strong> flux<br />

cospectrum, R uw <strong><strong>an</strong>d</strong> R wζy are calculated as function <strong>of</strong><br />

Z. At a fixed wavenumber the fraction <strong>of</strong> the resolved<br />

<strong>fluxes</strong> is smaller closer to the bottom (smaller Z) <strong><strong>an</strong>d</strong><br />

the fraction <strong>of</strong> the resolved <strong>vorticity</strong> flux is smaller th<strong>an</strong><br />

that <strong>of</strong> the resolved momentum flux (Figure B1). To<br />

measure more th<strong>an</strong> 95% <strong>of</strong> the <strong>vorticity</strong> flux, the sensor<br />

scale has to be smaller th<strong>an</strong> 0.02 m when the measurement<br />

is taken at 1 mab <strong><strong>an</strong>d</strong> smaller th<strong>an</strong> 0.1 m when the<br />

measurement is taken at more th<strong>an</strong> 2 mab. To measure<br />

more th<strong>an</strong> 95% <strong>of</strong> the momentum flux, the sensor scale<br />

has to be smaller th<strong>an</strong> 0.1 m when the measurement is<br />

taken above 1 mab.<br />

Fraction <strong>of</strong> Resolved Flux<br />

1<br />

0.8<br />

0.6<br />

0.4<br />

95%<br />

R uw Z = 5 m<br />

0.2<br />

(a)<br />

0<br />

10 −4 10 −2 10 0 10 2<br />

k x (m −1 )<br />

R wζy Z = 5 m<br />

R uw Z = 1 m<br />

R wζy Z = 1 m<br />

Z (m)<br />

20<br />

15<br />

10<br />

5<br />

(b)<br />

0<br />

10 −1 10 0 10 1 10 2<br />

k 95% (m −1 )<br />

Figure B1. (a) Fraction <strong>of</strong> <strong>fluxes</strong> resolved (equations<br />

(B1) <strong><strong>an</strong>d</strong> (B2)) at 1 <strong><strong>an</strong>d</strong> 5 meters above bottom (mab).<br />

(b) Cut<strong>of</strong>f wavenumber at which more th<strong>an</strong> 95% <strong>of</strong><br />

<strong>fluxes</strong> are resolved as a function <strong>of</strong> Z. Solid curves are<br />

for momentum <strong>fluxes</strong>, <strong><strong>an</strong>d</strong> dashed curves are for <strong>vorticity</strong><br />

<strong>fluxes</strong>.<br />

On the basis <strong>of</strong> the empirical momentum flux cospectrum,<br />

our model <strong>vorticity</strong> flux spectrum, <strong><strong>an</strong>d</strong> the EMVM<br />

response functions (Figure A1), we calculate the resolved<br />

momentum <strong><strong>an</strong>d</strong> <strong>vorticity</strong> <strong>fluxes</strong> as a function <strong>of</strong><br />

height above the bottom (Figure B2). The EMVM captures<br />

more th<strong>an</strong> 94% <strong>of</strong> the momentum flux <strong><strong>an</strong>d</strong> 90%<br />

<strong>of</strong> the <strong>vorticity</strong> flux above 1 mab.<br />

Z (m)<br />

20<br />

15<br />

10<br />

5<br />

0<br />

0.85 0.9 0.95 1<br />

EMVM / & EMVM /<br />

Figure B2. Fraction <strong>of</strong> momentum flux (solid curve)<br />

<strong><strong>an</strong>d</strong> <strong>vorticity</strong> flux (dashed curve) resolved by the<br />

electro-magnetic <strong>vorticity</strong> meter (EMVM) sensor as a<br />

function <strong>of</strong> Z. Fractions were computed us<strong>in</strong>g the empirical<br />

momentum flux cospectrum, our model <strong>vorticity</strong><br />

flux cospectrum, <strong><strong>an</strong>d</strong> the EMVM sensor response functions.<br />

Acknowledgments. The successful observations taken<br />

<strong>in</strong> Picker<strong>in</strong>g Passage were achieved with the vital help<br />

<strong>of</strong> John Dunlap, James Carlson, Eric Boget, <strong><strong>an</strong>d</strong> Gordon<br />

Welsh. Discussions with Eric Kunze <strong><strong>an</strong>d</strong> Eric D’Asaro have<br />

been very helpful. This research was supported by the Office<br />

<strong>of</strong> Naval Research.<br />

References<br />

Antonia, R. A., <strong><strong>an</strong>d</strong> Y. Zhu, Inertial r<strong>an</strong>ge behaviour <strong>of</strong><br />

the longitud<strong>in</strong>al heat flux cospectrum, Boundary Layer<br />

Meteorol., 70, 429–434, 1994.<br />

Batchelor, G. K., The Theory <strong>of</strong> Homogeneous Turbulence,<br />

Cambridge Univ. Press, New York, 1959.<br />

Bernard, P. S., J. M. Thomas, <strong><strong>an</strong>d</strong> R. A. H<strong><strong>an</strong>d</strong>ler, Vortex<br />

dynamics <strong><strong>an</strong>d</strong> the production <strong>of</strong> Reynolds stress, J. Fluid<br />

Mech., 253, 385–419, 1993.<br />

Blackwelder, R. F., <strong><strong>an</strong>d</strong> H. Eckelm<strong>an</strong>n, Streamwise vortices<br />

associated with the burst<strong>in</strong>g phenomenon, J. Fluid<br />

Mech., 94, 557–594, 1979.<br />

Bowden, K. F., <strong><strong>an</strong>d</strong> S. R. Ferguson, Variation with height

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