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

The relation between wind speed and wave slope variance can be assessed on a global scale using the collocated wind speed measurements from AMSR-E and the variance of the wave

emission line profiles along the slit, after removing the background and hair lines and averaging five spectra. Note the variations in the central intensities. The slit was put at

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

Our experiments with an idealized Atmospheric General Circulation Model and realistic continents show that land surface evaporation must be limited in order to obtain drying over

(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

This confirms that the energy deposited at high latitudes, which leads to the geomagnetic and ionospheric disturbances following a southward turning of the IMF, increases with

(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