The Fluid Ionosphere
Abstract
:1. Introduction
2. The System
2.1. Smooth and Deterministic: The Continua
- the system is formed by parcels with thermodynamic numbers of particles (3);
- the statistical mechanics of these particles converges to space- and time-differentiable emerging variables (6);
- the system is locally in thermal equilibrium, hence described via a kinetic theory converging to a local equilibrium thermodynamics.
2.2. The System: Matter and Interactions
2.3. Fluid Matter Variables
2.4. Dynamical Variables for Matter
- Neutral particles. Various molecules or atoms (e.g., O, N, O2, N2, CO2, NH4 and so on) with zero electric charge: These ones are the major part, both numerically as well as massively, of all the high atmosphere, up to the level of about 1000 km height, the starting point of a region where practically all the matter is ionized. From that point on, one speaks about plasmasphere.If each neutral species is indicated with the index , the speed of their center of mass is point by point some field , defined as follows in terms of partial matter densities and velocities :This velocity undergoes a proper dynamics that may be attributed to the neutral matter as a unique fluid .
- Negative ions. These are the species which have captured one or more electrons. These particles are very rare and their presence is practically negligible in general. Nevertheless, one should consider them when dealing with the lower part of the ionosphere, as the region D and the lower E [10]. Negative ion abundance is reasonably non-negligible only under 95 km, even if, in particular conditions, this can be false. Sometimes, a coefficient is defined for each negative ion as
- Positive ions. These are the neutrals that have lost one or more electrons. Actually, the 2- or 3-valent positive ions are very rare, so we can restrict ourselves to the study of 1-valent positive ions. When the constraint (13) holds and no negative ions exist, positive ions have a numerical density equal to that of free electrons.
- Electrons. Electrons are the most important element for ionospheric phenomenology as far as electromagnetic disturbances are concerned, because of their very small mass, which gives them a great mobility [9], making them very effective in producing local and travelling electromagnetic fields.
2.5. Electromagnetic Dynamical Variables
3. Equations of Motion
3.1. Mass Balance
3.2. Chemical Space Formalism
3.3. Momentum Balance (Newton’s )
- the electromagnetic fields and defined at its position;
- the gravitational field defined at its position;
- the inertial forces measured in the reference frame co-rotating with the Earth (the SERF);
- the remaining part of the system which interacts with at the border through the nearby parcels;
- the other systems with ;
- the mechanical waves passing by the position of .
3.4. Internal Energy Balance
3.5. Some More Relationships
3.6. Maxwell Equations
- the displacement current is considered much smaller than the matter currents
- the magnetic field produced by ionospheric currents is much smaller than the geomagnetic one
- electric charge densities producing important electric fields are very small, and so are their time derivatives
3.7. Neutral Components
3.8. Charged Components
3.8.1. Ion Motions
3.8.2. Electron Motions
4. The Quiet Ionosphere
4.1. Thermal Homogeneity and the NeWReF
4.2. An Anisotropic Conductor: Role of
4.3. Ohm’s Law for the Ionosphere
4.4. Ionospheric Electrostatic Fields
4.5. Electric Field “Propagation”
4.5.1. Pole to Equator “Propagation”
4.5.2. Current Injection and Perturbation Fields
5. Conclusions
Funding
Acknowledgments
Conflicts of Interest
Abbreviations
LIM | Local Ionospheric Medium |
SERF | Solid Earth Reference Frame |
NeWReF | Neutral Wind Reference Frame |
MKSA | Meter–Kilogram–Second–Ampere (International unit reference) |
FD | Fluid Dynamics |
BBGKY | Bogoljubov–Born–Green–Kirkwood-Yvon |
SO(3) | Group of Special Orthogonal matrices |
CoM | Center of Mass |
R2CoM | Relative to Center of Mass |
PDE | Partial Derivative Equation |
GRB | Gamma Ray Burst |
MIDAS | Multi-Instrument Data Analysis System |
MDPI | Multidisciplinary Digital Publishing Institute |
DOAJ | Directory of open -access journals |
Appendix A. Lagrangian Time Derivative of the Internal Energy
Appendix B. Navier–Stokes Equation for the Neutral Wind
Appendix C. Irrelevance of in an Experimental Example
Appendix D. The -Parallel vs. -Perpendicular Decomposition of Velocities
Appendix E. The Electric Current Calculations
Appendix F. Solving the PDE for ϕ in the Anisotropic Conductor
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Materassi, M. The Fluid Ionosphere. Atmosphere 2025, 16, 147. https://doi.org/10.3390/atmos16020147
Materassi M. The Fluid Ionosphere. Atmosphere. 2025; 16(2):147. https://doi.org/10.3390/atmos16020147
Chicago/Turabian StyleMaterassi, Massimo. 2025. "The Fluid Ionosphere" Atmosphere 16, no. 2: 147. https://doi.org/10.3390/atmos16020147
APA StyleMaterassi, M. (2025). The Fluid Ionosphere. Atmosphere, 16(2), 147. https://doi.org/10.3390/atmos16020147