Articles | Volume 32, issue 8 
            
                
                    
            
            
            https://doi.org/10.5194/angeo-32-1011-2014
                    © Author(s) 2014. This work is distributed under 
the Creative Commons Attribution 3.0 License.
                the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/angeo-32-1011-2014
                    © Author(s) 2014. This work is distributed under 
the Creative Commons Attribution 3.0 License.
                the Creative Commons Attribution 3.0 License.
Pre-onset auroral signatures and subsequent development of substorm auroras: a development of ionospheric loop currents at the onset latitudes
                                            Office Geophysik, Ogoori, Japan
                                        
                                    K. Hayashi
                                            University of Tokyo, Tokyo, Japan
                                        
                                    M. Thomsen
                                            Los Alamos National Laboratory, Los Alamos, NM, USA
                                        
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                                        Osuke Saka
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                                    Manuscript not accepted for further review 
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                                    Short summary
                                            
                                                Auroral spirals known as northern lights are a spectacular light show in the polar night sky. Internal processes in the polar ionosphere initiate northern lights by producing charge separations along the field lines. Parallel electric fields generated above the ionosphere by charge separations are steady-state electric fields. They occasionally discharge to produce northern lights, analogous to lightning flash in a thunderstorm.
                                            
                                            
                                        Osuke Saka
                                    Ann. Geophys., 41, 369–373, https://doi.org/10.5194/angeo-41-369-2023, https://doi.org/10.5194/angeo-41-369-2023, 2023
                                    Short summary
                                    Short summary
                                            
                                                Transverse electric fields transmitted from the magnetosphere and those generated by the neutral winds yield a local breakdown of the charge neutrality at the boundaries between the thermosphere and mesosphere. The breakdown may create parallel electric fields in the thermosphere to produce spiral auroras and outflows. This explanation supposes an auroral generator located not in a distant space, but rather in our much nearer upper atmosphere.
                                            
                                            
                                        Osuke Saka
                                        Ann. Geophys. Discuss., https://doi.org/10.5194/angeo-2021-66, https://doi.org/10.5194/angeo-2021-66, 2021
                                    Revised manuscript not accepted 
                                    Short summary
                                    Short summary
                                            
                                                Auroral spirals known as northern lights are a spectacular light show in the polar night sky. We show that auroral spirals are produced in the polar ionosphere by the internal processes that ensure quasi-neutral equilibrium of the polar ionosphere which is often violated during field line dipolarization. The internal driver produces spiral auroras in a manner different from the field line mapping scenario.
                                            
                                            
                                        Osuke Saka
                                    Ann. Geophys., 39, 455–460, https://doi.org/10.5194/angeo-39-455-2021, https://doi.org/10.5194/angeo-39-455-2021, 2021
                                    Short summary
                                    Short summary
                                            
                                                The ionosphere is a partly ionized medium above the atmosphere. Because of its anisotropic properties, the imposed electric fields from the magnetosphere produce space charge. Polarization electric fields induced in the ionosphere by this process generate ion drifts (Pedersen currents) and plasma evaporation along the field lines, thus achieving a quasi-neutral equilibrium of the ionosphere. The evaporation grows as a large-scale parallel potential structure in the magnetosphere.
                                            
                                            
                                        Osuke Saka
                                    Ann. Geophys., 38, 467–479, https://doi.org/10.5194/angeo-38-467-2020, https://doi.org/10.5194/angeo-38-467-2020, 2020
                                    Short summary
                                    Short summary
                                            
                                                The first 10 min interval of Pi2 onset is the most active period of substorms composed of field line deformations associated with an increase in curvature radius of flux tubes and their longitudinal expansion. The flux tube deformations were triggered by the ballooning instability of slow magnetoacoustic waves upon arrival of the dipolarization front from the tail. They preceded the classical dipolarization caused by the reduction of cross-tail currents and resulting pileup of the field lines.
                                            
                                            
                                        Osuke Saka
                                    Ann. Geophys., 37, 381–387, https://doi.org/10.5194/angeo-37-381-2019, https://doi.org/10.5194/angeo-37-381-2019, 2019
                                    Short summary
                                    Short summary
                                            
                                                Flow channel extending in north–south directions is produced in the initial pulse of Pi2 pulsations associated with the field line dipolarization. Drifts in the ionosphere of the order of kilometers per second accumulated plasmas at the low-latitude end of the flow channel. The plasma compression in the ionosphere produced field-aligned currents, parallel electric fields, and auroral expansion. We called the compressive ionosphere a "dynamic ionosphere".
                                            
                                            
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