Priorité des Opérations sur les Nombres Naturels à Trois Étapes (Sans Exposents) (A)

(7), calculated for each 5 min averaging period and averaged over each nominal latitude bin, were used as proxies for uncertain- ties. Table S2 summarises the total uncertainty on

At Schauinsland, a mountain station in south- western Germany, even though the spatial resolution of REMO is not fine enough to reproduce transport processes induced by

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)

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

These hybrid melts eventually reach the surface as the shield-building lava series (the Older Series Figure 11. Model of decompression melting in a lithologically heterogeneous

Using the method of characteristics to invert ground-based data of the ground magnetic ®eld distur- bance and of the ionospheric electric ®eld, we obtain spatial distributions