Priorité des Opérations sur les Nombres Entiers Positifs Négatifs à Trois Étapes (A)

Applying criteria 1 and 2, we count the magnetopause crossings with electron heat flux. Thereby, we do not dis- tinguish whether the heat flux is due to a streaming of ring

A global coupled thermosphere-ionosphere- plasmasphere model is used to simulate a family of large-scale imperfectly ducted atmospheric gravity waves (AGWs) and associated

Mean monthly occurrence frequencies of Kp index in di€erent magnitude ranges as a function of the phase of the solar cycle: minimum (Min); ascending (Asc); maximum (Max); and

Time series of the total kinetic energy in the rectangular basin subject to constant wind from the West in the long direction (a) and from the South in the cross direction (b)

Abstract. The generation of Hall and ®eld-aligned currents in and in the vicinity of nighttime mid-latitude sporadic E-layers moving under the action of strong acoustic impulses

Variable Estimates Std. The remaining 55 events were divided into two sets, namely, a training set and a validation set. The training dataset, comprising of 46 events, which included

Field-line reso- nances occur when harmonics of the eigenfrequency of the magnetospheric cavity or waveguide match the fundamental eigenfrequency or successive harmonics of

The Millstone Hill Incoherent Scatter Data Acquisition System (MIDAS) is based on an abstract model of an incoherent scatter radar.. This model is implemented in a hierarchical