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ssc-367 - Ship Structure Committee

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H~ is the significantwave height, and<br />

‘m<br />

is the<br />

frequency of maximum spectral energy.<br />

The Bretschneider equation<br />

may be written in terms of the peak period<br />

instead of the peak frequency, by substituting urn=2iT/T.<br />

P<br />

S(u) = (5/16)*(ti)2* [(21r)4/(u5*(T)4)]*<br />

exp[-l~25*(2~q/(~*T )4] p<br />

A.3.2<br />

Pierson-Moskowitz Spectrum<br />

The Pierson-Moskowitz (Reference A.4) spectrum was created to fit<br />

North Atlantic weather data. The P-M spectrum is the same as the<br />

Bretschneider spectrum, but with the H* and Mm dependence merged<br />

into a single parameter. The frequency used in the exponential has -<br />

also been made a function of reported wind speed. The equation for<br />

the Pierson-Moskowitz spectrum is as follows.<br />

S(u) = a*g2/~S)*exp[-~*(~0/~)4]<br />

where:<br />

a<br />

: 0.0081<br />

B<br />

= 0.74<br />

&l<br />

o<br />

= g/u<br />

and, U<br />

is the wind speed reported by the weather ships.<br />

The Pierson-Moskowitz spectrum equation may be obtained from the<br />

Bretschneider equation by using one of the following relations<br />

between H~ and Wm.<br />

A-12<br />

--;”,<br />

:“,< L.

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