New energy, angle momentum and entropy balance approach to modelling climate and macroturbulent atmospheric dynamics, heat and mass transfer at macroscale. I. General Formalism

Abstract

New energy, angle momentum and entropy balance approach to modelling climate and macroturbulent atmospheric dynamics, heat and mass transfer at macroscale. I. General Formalism We present elements of a new non-stationary balance approach to modelling global mechanisms of climate and macro turbulent atmospheric low-frequency processes, including processes of heat-mass transfer at spatial and temporal macro scales, teleconnection effects etc. The main forming factor is a triplet of interacting solitons: "the planetary soliton of Hadley cells-the entire complex of atmospheric fronts-the Rossby soliton wave packet". The approach is based on the using balance relationships for entropy, energy and angular momentum, spectral theory of atmospheric macroturbulence, atmospheric moisture flow in further connection with the continuity of atmospheric circulation forms (teleconnection, genesis of fronts). Particular application is studying a spatial-temporal picture of the long-term atmospheric pollutants (including distribution of radionuclides after accidents at the nuclear power plant like Fukushima etc) in the atmosphere with accounting for the macro turbulent, circulation low-frequency processes.

New energy, angle momentum and entropy balance approach to modelling climate and macroturbulent atmospheric dynamics, heat and mass transfer at macroscale. III. Low-frequency approximation and singularities in fields of meteoelements

“…In modern climate physics, the need to develop special methods for observing lowfrequency oscillations of non-equilibrium thermodynamic processes in the geosphere has been determined [1,2,[20][21][22][23][24][25]. To date, methods of physical and statistical analysis and processing of data sets of the network of ground or satellite measurements are used to indicate such phenomena.…”

“…However, these techniques are far from standardized and to some extent unique for each of these long-term processes. Therefore, the development of methods for monitoring the most low-frequency processes on a planetary scale to observe some geophysical factors, summarize the contributions of low-frequency fluctuations, especially relevant in the long-term physics of climate forecasts [1,2,[20][21][22][23]. Currently, this problem is far from being solved, although a number of indirect steps in this direction have been made in a number of works (see, for example, [1][2][3][4][5][6][7][8][9][10][11][12][13][14][15][16][17][18][19][20][26][27][28][29][30][31][32]).…”

“…This paper goes on our work on quantitative studying energy, angle momentum and entropy balance relationships in modelling climate and macroturbulent atmospheric dynamics, heat and mass transfer in atmospheric environment at macroscale. Really, one could remind [1,2] that understanding global mechanisms in atmospheric macroturbulent processes, teleconnection effects etc attracts a fundamental interest in a modern physics of climate and heat-and mass transfer in complex aerodispersed (atmospheric) systems [1][2][3][4][5][6][7][8][9][10][11][12][13][14][15][16][17][18][19][20]. As it is earlier indicated [1,2], nowdays there are different, quite consistent approaches to modelling global atmospheric macroprocesses in atmosphere and other geospheres (look for example, review in [1,2]).…”

“…Really, one could remind [1,2] that understanding global mechanisms in atmospheric macroturbulent processes, teleconnection effects etc attracts a fundamental interest in a modern physics of climate and heat-and mass transfer in complex aerodispersed (atmospheric) systems [1][2][3][4][5][6][7][8][9][10][11][12][13][14][15][16][17][18][19][20]. As it is earlier indicated [1,2], nowdays there are different, quite consistent approaches to modelling global atmospheric macroprocesses in atmosphere and other geospheres (look for example, review in [1,2]). Such known methods as MLDP0 (Modèle Lagrangien de Dispersion de Particules d'ordre 0), HYSPLIT (Hybrid Single-Particle Lagrangian Integrated Trajectory Model), NAME (Numerical Atmospheric-dispersion Modelling Environment), RATM (Regional Atmospheric Transport Model), FLEXPART (Lagrangian Particle Dispersion Model), model of the European Center for Mdium-Range Weather Forecasts (ECMWF) and others are usually mentioned (e.g.…”

“…In ref. [1,2] there are considered the elements of a generalized approach, which is based on the entropy, energy, moment balance relationships for the global atmospheric lowfrequency processes, theory of atmospheric macroturbulence and circulation over the position of the front sections. It has been stressed that the main process-forming factor is a triplet of interacting solitons: "the planetary soliton of Hadley cells -the entire complex of atmospheric fronts -the Rossby soliton wave packet".…”