Reports on Progress in Physics · 2008 · 243 citations · 197 references
Natural SciencesEarth SciencesPhysicsAtmospheric ElectricityAtmospheric ScienceElectromagnetismAtmospheric ConductivityCloud ElectrificationGlobal Electric CircuitIonospheric ElectrodynamicsLightning PhysicsAir-earth Current DensityAtmospheric Electric FieldAtmospheric Electrical Conductivity ProfilesConduction Current In The AtmosphereEarth Surface Current DensityGlobal Ionospheric CircuitIonospheric CurrentsStratospheric Aerosols
The global atmospheric electric circuit responds to external forces such as cosmic ray flux and solar wind electric fields, as well as internal factors like volcanic and anthropogenic aerosols, producing spatial and temporal variations in the downward ionosphere‑earth current density Jz. This review surveys recent progress in the theory and observation of the global atmospheric electric circuit, emphasizing its direct current characteristics and variability, and examines how changes in the downward ionosphere‑earth current influence cloud microphysics and modest weather and climate variations. The authors synthesize observations and theoretical models of the circuit’s direct current behavior and its temporal variability, and assess how fluctuations in the downward ionosphere‑earth current affect cloud microphysical processes.
This review is an overview of progress in understanding the theory and observation of the global atmospheric electric circuit, with the focus on its dc aspects, and its short and long term variability. The effects of the downward ionosphere-earth current density, Jz, on cloud microphysics, with its variability as an explanation for small observed changes in weather and climate, will also be reviewed. The global circuit shows responses to external as well as internal forcing. External forcing arises from changes in the distribution of conductivity due to changes in the cosmic ray flux and other energetic space particle fluxes, and at high magnetic latitudes from solar wind electric fields. Internal forcing arises from changes in the generators and changes in volcanic and anthropogenic aerosols in the troposphere and stratosphere. All these result in spatial and temporal variation in Jz.
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The mathematical theory of non-uniform gases
Journal of the Franklin Institute · 1953 · 7.7K citations
The mathematical theory of non-uniform gases
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