Priorité des Opérations sur les Nombres Naturels à Quatre Étapes (A)

ison to the corresponding data retrieved from traditional balloon borne solar occulta- tion measurements performed by the LPMA/DOAS (Limb Profile Monitor of the Atmo-

Figure 11 shows from South to North (see section 2 for description of the units): the Muya basin (part of the active North Baikal Rift System); the ophiolitic units thrusting

(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

(1999) estimated the azimuthal phase veloc- ity of compressional pulsations using close conjunction of Equator-S and Geotail satellites for the 9 March 1998 event.. The

Several individual topics are then discussed, including eclipse e€ects, the asymmetries of the `equatorial trough', variations with longitude, the semiannual variation, the e€ects

Classical regression analysis provides a basis for predicting water levels relative to current, but in the cluster regression line approach, reliable predictions are only

In these three examples it was found that, within the error limits and at least at one ofthe receiver sites, the perpendicular anisotropy is aligned in the direction of the plasma