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Natural convection near an isothermal wall far downstream from a source - MaRDI portal

Natural convection near an isothermal wall far downstream from a source (Q3557122)

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Natural convection near an isothermal wall far downstream from a source
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    Natural convection near an isothermal wall far downstream from a source (English)
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    22 April 2010
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    natural convection
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    flow instability
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    boundary layers
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    fractals
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