Bangor, 10-12/04/06Simpson Retirement Conference1 Numerical Modelling of SImPSon Hans Burchard...

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Bangor, 10-12/04/06 Simpson Retirement Conference 1 Numerical Modelling of SImPSon Hans Burchard Baltic Sea Research Institute Warnemünde Bolding & Burchard Hyrodynamics [email protected]

Transcript of Bangor, 10-12/04/06Simpson Retirement Conference1 Numerical Modelling of SImPSon Hans Burchard...

Page 1: Bangor, 10-12/04/06Simpson Retirement Conference1 Numerical Modelling of SImPSon Hans Burchard Baltic Sea Research Institute Warnemünde Bolding & Burchard.

Bangor, 10-12/04/06 Simpson Retirement Conference 1

Numerical Modelling of SImPSon

Hans Burchard

Baltic Sea Research Institute Warnemünde

Bolding & Burchard Hyrodynamics

[email protected]

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What is SIPS ?

Google says:

Social Inclusion PartnershipsStructural Insulated PanelsSignal Processing SystemsSecure Internet Processing ServicesStatistically Improbable PhrasesSchweizerische Interessengemeinschaft für Polio-Spätfolgen Società Italiana di Psicologia Side Impact Protection SystemStudent Intellectual Property Society ...Strain Induced Periodic Stratification (search for 'sips john simpson bangor')

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Tidal straining during ebb tide

Simpson et al. 1990

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Tidal asymmetry (schematically)

Jay and Musiak 1994

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Tidal asymmetry (numerically)

Burchard and Baumert, 1998

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Tidal straining and estuarine turbidity maxima

Burchard et al. 2004Animation by Manuel Ruiz

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Strain-induced periodic stratification (SIPS)(in Liverpool Bay, temperature & salinity)

Rippeth et al. (2001), Burchard (2002), Simpson et al. (2002)

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Rippeth et al. (2001), Burchard (2002), Simpson et al. (2002)

Strain induced periodic stratification (SIPS)(in Liverpool Bay, dissipation rate)

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A simple model for SIPS

See also Sharples and Simpson (1995)

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Scaling of SIPS equations

See also Baumert and Radach (1992)

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Two independent SIPS parameters

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Non-dimensional SIPS equations

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Measure for SIPS intensity

See also Simpson and Bowers (1981)

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Example calculation for idealised SIPS

Dimensionless relative buoyancy Potential energy anomaly (dimless)

Dimensionless time Dimensionless time

(Pg=0.2, Si=0.01)

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Si

Pg

red: Pg · Si = 0.002

No SIPS

~

Maximum potential density anomaly as function of Si and Pg

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Suggested condition for SIPS:

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What we have ignored:

Varying sea level elevationNon-zero mean surface slopeVarying horizontal density gradientBottom roughness to depth ratioEarth rotationSurface heat fluxSolar radiationSurface momentum fluxSurface wavesInternal waves

Each of these processes would give us at least one more dimensionless number

Conclusion: The real world is too complex for us to understand.