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

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

They were later discriminated into tangential or rotational according to their characteristics: the former possess no ®eld normal to the discontinuity surface but show a

Using the method of superposition of epoches, the mean occurrence probability of F-spread for the set of earthquakes with M > 5.5, R < 1000 km, h < 80 km is calculated..

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,

(4) and (5), the values of kx and kz are chosen to be the dominant horizontal and vertical wave numbers at each integer hour (shown in Fig. 2), respectively; the values u; w and ma

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

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