Addition et Soustraction d'un Nombre à 4 Chiffres par un Nombre à 3 Chiffres SANS retenue (Gros Caractère) (A)

The evolution, and dynamics of Es clouds can be studied from backscatter data obtained by the different radar beams over a period of time.. Velocities can be determined by plotting

Lors- qu’on ne sait pas si le verbe est au mode indicatif ou subjonctif parce qu’il se prononce de la même façon, on suggère de le remplacer par un verbe comme faire ou partir, dont

A comparison of results obtained using steady-state and time-dependent models with the same mean conditions (cross-polar-cap voltage, »pc, and polar cap area) has been undertaken

Phase functions have been calculated using the Monte Carlo/geometric ray tracing method for single hexagonal pyramidal ice crystals (such as solid and hollow bullets) randomly

Ozone vertical profiles derived from nadir mea- surements of the GOME instrument on board the ERS-2 satellite, by means of the FURM algorithm of the Univer- sity of Bremen,

change in the calculated wave azimuth. W can also be calculated from the average of the line-of-sight velocities in the o€-vertical beams, i.e. Figure 6 shows a visible-light

In this case we can expect variation of the energetic particle source amplitude (which is proportional to the electron density in a cloud), pitch-angle anisotropy, and

A surprising result was that for pulsation signals away from the local ®eld line resonance (FLR) frequency the phase of the ionospheric Doppler oscillations was found to