Turbulent diffusion is usually described by a turbulent diffusion coefficient.
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Turbulent diffusion is usually described by a turbulent diffusion coefficient.
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The second deviation from the explicit treatment is related to the turbulent diffusion in vertical direction.
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To avoid this, vertical turbulent diffusion is treated using the second order Crank Nicolson method.
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These include work on the classification of estuaries, estimates of turbulent diffusion, and studies of the impact of volcanoes on climate.
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This is because these methods involve ideal flow, which cannot simulate the conditions of turbulent flow necessary for developing turbulent diffusion models.
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The turbulent diffusion constant D = v \ delta is then independent of the scale length and is approximately equal to the Bohm value.
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Substituting into the first continuity equation and ignoring reactions, sources, and molecular diffusion results in the following differential equation considering only the turbulent diffusion approximation in eddy diffusion:
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With the advancement in computer-aided modeling and programming, scientists have been able to simulate turbulent flow in order to better understand turbulent diffusion in the atmosphere and in fluids.
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As technology and computer abilities are rapidly expanding, these methods will also improve greatly, and will more than likely be at the forefront of future research on modeling turbulent diffusion.
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