USER MANUAL SWAN Cycle III version 40.72A

USER MANUAL SWAN Cycle III version 40.72A USER MANUAL SWAN Cycle III version 40.72A

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88 Chapter 4 ’fname’ name of the file to which the wave field is written. Note: for parallel MPI runs, more than one hotfile will be generated depending on the number of processors (fname-001, fname-002, etc.). STOP This required command marks the end of the commands in the command file. Note that the command STOP may be the last command in the input file; any information in the input file beyond this command is ignored.

Appendix A Definitions of variables In SWAN a number of variables are used in input and output. Most of them are related to waves. The definitions of these variables are mostly conventional. HSIGN Significant wave height, denoted as H s in meters, and defined as H s = 4√ ∫ ∫ E(ω,θ)dωdθ where E(ω,θ) is the variance density spectrum and ω is the absolute radian frequency determined by the Doppler shifted dispersion relation. However, for ease of computation, H s can be determined as follows: H s = 4√ ∫ ∫ E(σ,θ)dσdθ HSWELL Significant wave height associated with the low frequency part of the spectrum, denoted as H s,swell in meters, and defined as H s,swell = 4√ ∫ ωswell 0 ∫ 2π 0 E(ω,θ)dωdθ TMM10 with ω swell = 2πf swell and f swell = 0.1 Hz by default (this can be changed with the command QUANTITY). Mean absolute wave period (in s) of E(ω,θ), defined as ∫ ∫ ∫ ω T m−10 = 2π −1 E(ω,θ)dωdθ ∫ ∫ ω E(ω,θ)dωdθ = 2π∫ −1 E(σ,θ)dσdθ ∫ ∫ E(σ,θ)dσdθ TM01 Mean absolute wave period (in s) of E(ω,θ), defined as (∫ ∫ ) −1 (∫ ∫ ) −1 ωE(ω,θ)dωdθ T m01 = 2π ∫ ∫ ωE(σ,θ)dσdθ E(ω,θ)dωdθ = 2π ∫ ∫ E(σ,θ)dσdθ 89

Appendix A<br />

Definitions of variables<br />

In <strong>SWAN</strong> a number of variables are used in input and output. Most of them are related<br />

to waves. The definitions of these variables are mostly conventional.<br />

HSIGN<br />

Significant wave height, denoted as H s in meters, and defined as<br />

H s = 4√ ∫ ∫ E(ω,θ)dωdθ<br />

where E(ω,θ) is the variance density spectrum and ω is the absolute<br />

radian frequency determined by the Doppler shifted dispersion relation.<br />

However, for ease of computation, H s can be determined as follows:<br />

H s = 4√ ∫ ∫ E(σ,θ)dσdθ<br />

HSWELL<br />

Significant wave height associated with the low frequency part of<br />

the spectrum, denoted as H s,swell in meters, and defined as<br />

H s,swell = 4√ ∫ ωswell<br />

0<br />

∫ 2π<br />

0 E(ω,θ)dωdθ<br />

TMM10<br />

with ω swell = 2πf swell and f swell = 0.1 Hz by default (this can be changed<br />

with the command QUANTITY).<br />

Mean absolute wave period (in s) of E(ω,θ), defined as<br />

∫ ∫ ∫ ω<br />

T m−10 = 2π<br />

−1 E(ω,θ)dωdθ<br />

∫ ∫ ω<br />

E(ω,θ)dωdθ<br />

= 2π∫ −1 E(σ,θ)dσdθ<br />

∫ ∫ E(σ,θ)dσdθ<br />

TM01<br />

Mean absolute wave period (in s) of E(ω,θ), defined as<br />

(∫ ∫ ) −1 (∫ ∫ ) −1<br />

ωE(ω,θ)dωdθ<br />

T m01 = 2π ∫ ∫ ωE(σ,θ)dσdθ<br />

E(ω,θ)dωdθ<br />

= 2π ∫ ∫ E(σ,θ)dσdθ<br />

89

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