The Mathematical Modeling of the Atmospheric Diffusion Equation
International Journal of Environmental Monitoring and Analysis
Volume 2, Issue 2, April 2014, Pages: 112-116
Received: Feb. 12, 2014; Accepted: Apr. 29, 2014; Published: Apr. 30, 2014
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Authors
Khaled Sadek Mohamed Essa, Department of Mathematics and Theoretical Physics, Nuclear Research Centre, Cairo, Egypt
Mohamed Magdy Abd El-Wahab, Astronomy Department, Faculty of Science, Cairo University, Cairo, Egypt
Hussein Mahmoud ELsman, Physics Department, Faculty of science, Monofia University, Monofia, Egypt
Adel Shahta Soliman, Theoretical Physics Department, National Research Centre, Cairo, Egypt
Samy Mahmoud ELGmmal, Physics Department, Faculty of science, Monofia University, Monofia, Egypt
Aly Ahamed Wheida, Theoretical Physics Department, National Research Centre, Cairo, Egypt
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Abstract
The advection diffusion equation (ADE) is solved in two directions to obtain the crosswind integrated concentration. The solution is solved using separation variables technique and considering the wind speed depends on the vertical height and eddy diffusivity depends on downwind and vertical distances. Comparing between the two predicted concentrations and observed concentration data are taken on the Copenhagen in Denmark.
Keywords
Advection Diffusion Equation, Predicted Normalized Crosswind Integrated Concentrations, Separation Variables
To cite this article
Khaled Sadek Mohamed Essa, Mohamed Magdy Abd El-Wahab, Hussein Mahmoud ELsman, Adel Shahta Soliman, Samy Mahmoud ELGmmal, Aly Ahamed Wheida, The Mathematical Modeling of the Atmospheric Diffusion Equation, International Journal of Environmental Monitoring and Analysis. Vol. 2, No. 2, 2014, pp. 112-116. doi: 10.11648/j.ijema.20140202.18
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