Identify the nature of accurate meteorology and air movement in the boundary layer of the atmosphere, stresses and their impact on the layer adjacent to the earth's surface, the dimensions of movement in the bounded layer. Equations of conservation of energy and moments, equations of diffusion, the nature of non-rheological motion and the definition of the Reynolds number, the equations of motion in the surface layer, the description of the equations of motion by visualization, the conclusion of a finite Reynolds and the definition of total tangential and perpendicular stresses, the definition of the obstruction coefficient.2. Understanding the thermal energy equation: average and boundary energy, the various factors that affect the energy balance, the different energy transformations, the equations of motion for velocities in a neutral atmosphere.· 3. Being able to calculate the coefficients of motion, the influence of stability states, Richardson's number, Richardson's flux, Ladenhof symmetry theory, length scale. Also, understanding the change in velocities and temperature with height in the stable and unstable atmosphere· 4. Acquaintance with Akman's theory to study the finite layer, the height of the finite layer, the vertical velocity in the Akman layer, the change of stresses with height, Rossby's theory of symmetry. Also conducting applications in accurate meteorology: vertical distribution of pollutants, application of diffusion equations for pollutants.
Intended learning outcomes
a. Knowledge and understanding:A.1 The student should know the movement of air in the boundary layer of the atmosphere, thermal equilibrium and exchange of energies, stresses and their impact on the layer adjacent to the earth’s surface, as well as the equations of energy conservation and moments, the equations of diffusion.A.2 The student describes the various factors that affect the energy balance and the equations of motion for velocities in a neutral atmosphere.A.3 That the student explain the change in velocities and temperature with altitude for stable and unstable atmosphereA.4 That the student explain Ackmann's theory for the study of the finite layer and the height of the finite layer.B. Intellectual skills:B.1 That the student derive the Reynolds determinant and the outputs of the equations of motion in the surface layer.B.2 That the student relates the different factors that affect the energy balance and the different energy transformations.B.3 That the student compares the change of velocity and temperature with altitude for stable and unstable atmosphere.B.4 That the student analyze the vertical velocity in the Ackman layer and also the change of stresses with height.C. Practical and professional skills:C. 1 That the student diagnoses the outputs of the equations of motion, the outputs of the equations of conservation of energy and moments, as well as the equations of diffusion.C.2 The student should use the Internet to increase information about the average and boundary energy and the various factors that affect the energy balance.C.3 That the student memorizes the method for calculating motion coefficients as well as velocities and temperature by height for stable and unstable atmospheres.C.4 The student performs some applications to simulate the spread of pollutants near the earth's surface.D. General and transferable skills:D.1 The student should be able to use computer programs to help understand the processes that occur in the layer near the earth's surface, the exchange and transmission of energies, stresses and their impact on the layer adjacent to the earth's surface (tangential and vertical total stresses).D.2 The student should be able to make oral and written presentations regarding Rossby's theory of symmetry and the spread of pollutants in the layer in contact with the earth's surface. .D.3 The student should be able to actively participate in the class, especially in exercises related to calculating motion coefficients.
