A Computational Study of the Transformation of Global Gas Flows in the Earth’s Atmosphere over the Course of a Year

DOI: 10.4236/ojfd.2014.44029   PDF   HTML   XML   2,682 Downloads   3,127 Views   Citations


A mathematical model, developed earlier in the Polar Geophysical Institute, is applied to investigate the transformation of global gas flows in the Earth’s atmosphere over the course of a year. The model is based on the numerical solution of the system of gas dynamic equations. The mathematical model produces three-dimensional distributions of the gas dynamic parameters of the atmosphere in the height range from 0 to 126 km over the Earth’s surface. To investigate the seasonal transformation of the global circulation of the lower and middle atmosphere, simulations are performed for conditions corresponding to twelve dates, which belong to twelve different months. Results of simulations indicate that the variations of the solar illumination of the Earth’s atmosphere, conditioned by different positions of the Earth along its trajectory around the Sun, influence considerably the transformation of the planetary circulation of the lower and middle atmosphere over the course of a year.

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Mingalev, I. , Orlov, K. and Mingalev, V. (2014) A Computational Study of the Transformation of Global Gas Flows in the Earth’s Atmosphere over the Course of a Year. Open Journal of Fluid Dynamics, 4, 379-402. doi: 10.4236/ojfd.2014.44029.

Conflicts of Interest

The authors declare no conflicts of interest.


[1] Manabe, S. and Hahn, D.G. (1981) Simulation of Atmospheric Variability. Monthly Weather Review, 109, 2260-2286.
[2] Cariolle, D., Lasserre-Bigorry, A., Royer, J.F. and Geleyn J.F. (1990) A General Circulation Model Simulation of the Springtime Antarctic Ozone Decrease and Its Impact on Mid-Latitudes. Journal of Geophysical Research, 95, 1883-1898.
[3] Rasch, P.J. and Williamson, D.L. (1991) The Sensitivity of a General Circulation Model Climate to the Moisture Transport Formulation. Journal of Geophysical Research, 96, 13123-13137.
[4] Graf, H.F., Kirchner, I., Sausen, R. and Schubert, S. (1992) The Impact of Upper-Tropospheric Aerosol on Global Atmospheric Circulation. Annales Geophysicae, 10, 698-707.
[5] Stott, P.A. and Harwood, R.S. (1993) An Implicit Time-Stepping Scheme for Chemical Species in a Global Atmospheric Circulation Model. Annales Geophysicae, 11, 377-388.
[6] Christiansen, B., Guldberg, A., Hansen, A.W. and Riishojgaard, L.P. (1997) On the Response of a Three-Dimensional General Circulation Model to Imposed Changes in the Ozone Distribution. Journal of Geophysical Research, 102, 13051-13077.
[7] Galin, V.Y. (1997) Parametrization of Radiative Processes in the DNM Atmospheric Model. Izvestiya AN, Physics of Atmosphere and Ocean, 34, 380-389. (Russian Issue)
[8] Gibelin, A.L. and Deque, M. (2002) Anthropogenic Climate Change over the Mediterranean Region Simulated by a Global Variable Resolution Model. Climate Dynamics, 20, 327-339.
[9] Mendillo, M., Rishbeth, H., Roble, R.G. and Wroten, J. (2002) Modelling F2-Layer Seasonal Trends and Day-to-Day Variability Driven by Coupling with the Lower Atmosphere. Journal of Atmospheric and Solar-Terrestrial Physics, 64, 1911-1931.
[10] Harris, M.J., Arnold, N.F. and Aylward, A.D. (2002) A Study into the Effect of the Diurnal Tide on the Structure of the Background Mesosphere and Thermosphere Using the New Coupled Middle Atmosphere and Thermosphere (CMAT) General Circulation Model. Annales Geophysicae, 20, 225-235.
[11] Langematz, U., Claussnitzer, A., Matthes, K. and Kunze, M. (2005) The Climate during Maunder Minimum: A Simulation with Freie Universitat Berlin Climate Middle Atmosphere Model (FUB-CMAT). Journal of Atmospheric and Solar-Terrestrial Physics, 67, 55-69.
[12] Smith, A.K., Garcia, R.R., Marsh, D.R. and Richter, J.H. (2011) WACCM Simulations of the Mean Circulation and Trace Species Transport in the Winter Mesosphere. Journal of Geophysical Research, 116, Article ID: D20115, 17 p.
[13] Mingalev, I.V. and Mingalev, V.S. (2005) The Global Circulation Model of the Lower and Middle Atmosphere of the Earth with a Given Temperature Distribution. Mathematical Modeling, 17, 24-40. (In Russian)
[14] Mingalev, I.V., Mingalev, V.S. and Mingaleva, G.I. (2007) Numerical Simulation of Global Distributions of the Horizontal and Vertical Wind in the Middle Atmosphere Using a Given Neutral Gas Temperature Field. Journal of Atmospheric and Solar-Terrestrial Physics, 69, 552-568.
[15] Picone, J.M., Hedin, A.E., Drob, D.P. and Aikin, A.C. (2002) NRLMSISE-00 Empirical Model of the Atmosphere: Statistical Comparisons and Scientific Issues. Journal of Geophysical Research, 107, Article ID: 1468, 16 p.
[16] Mingalev, I.V., Mingalev, O.V. and Mingalev, V.S. (2008) Model Simulation of Global Circulation in the Middle Atmosphere for January Conditions. Advances in Geosciences, 15, 11-16.
[17] Mingalev, I.V., Mingalev, V.S. and Mingaleva, G.I. (2012) Numerical Simulation of the Global Neutral Wind System of the Earth’s Middle Atmosphere for Different Seasons. Atmosphere, 3, 213-228.
[18] Mingalev, I.V. and Mingalev, V.S. (2012) Numerical Modeling of the Influence of Solar Activity on the Global Circulation in the Earth’s Mesosphere and Lower Thermosphere. International Journal of Geophysics, 2012, Article ID: 106035, 15 p.
[19] Mingalev, I., Mingaleva, G. and Mingalev, V. (2013) A Simulation Study of the Effect of Geomagnetic Activity on the Global Circulation in the Earth’s Middle Atmosphere. Atmospheric and Climate Sciences, 3, 8-19.
[20] Wardill, P. and Jacka, F. (1986) Vertical Motions in the Thermosphere over Mawson, Antarctica. Journal of Atmospheric and Terrestrial Physics, 48, 289-292.
[21] Crickmore, R.I., Dudeney, J.R. and Rodger, A.S. (1991) Vertical Thermospheric Winds at the Equatorward Edge of the Auroral Oval. Journal of Atmospheric and Terrestrial Physics, 53, 485-492.
[22] Ishii, M. (2005) Relationship between Thermospheric Vertical Wind and the Location of Ionospheric Current in the Polar Region. Advances in Polar Upper Atmosphere Research, 19, 63-70.
[23] Mingalev, V.S. (1993) Transport Equations for the Upper Atmosphere in a Rotating Reference Frame. Geomagnetizm i Aeronomiya, 33, 106-112. (Russian Issue)
[24] Obukhov, A.M. (1988) Turbulence and Dynamics of Atmosphere. Hydrometeoizdat, Leningrad. (In Russian)
[25] Mingalev, V.S., Mingalev, I.V., Mingalev, O.V., Oparin, A.M. and Orlov, K.G. (2010) Generalization of the Hybrid Monotone Second-Order Finite Difference Scheme for Gas Dynamics Equations to the Case of Unstructured 3D Grid. Computational Mathematics and Mathematical Physics, 50, 877-889.

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