The maximum depth of the mixed layer in which net growth can occur is called the critical depth.
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The water surface profile displays how the flow depth changes over a distance between critical depth and normal depth.
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Also shown are the critical energy or minimum energy, E c and the corresponding critical depth value, y c.
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The energy associated with the critical depth is found by placing the critical depth expression into the specific energy equation.
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The energy associated with the critical depth is found by placing the critical depth expression into the specific energy equation.
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In biological oceanography, his Critical Depth Hypothesis published in 1953 was a significant milestone in the explanation of phytoplankton spring blooms.
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As long as there are adequate nutrients available, net primary production occurs whenever the mixed layer is shallower than the critical depth.
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Critical depth can be used to determine the specific discharge, " q ", the discharge per unit width in a rectangular channel.
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Despite criticism of Sverdrup's Critical Depth Hypothesis, it is still regularly cited due to unresolved questions surrounding the initiation of spring blooms.
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For rectangular channels, the critical depth can be calculated by taking the derivative of the energy equation and setting it equal to zero.
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