Temps Écoulé Jusqu'à 5 Heures, à Intervalle de 1 Minute (A)

Columnar aerosol size distribution parameters at night- time retrieved by GRASP using different schemes (see Ta- ble 2) show a good coherence and smooth variation when they are

From the analysis of stress distribution, the highest measured stresses are inferred to represent the actual deviatoric stress t whose maximum value gives an estimate of the

This hypothesis was justified for previous magnetospheric missions (Peder- sen, 1995), showing that the potential difference between the spacecraft body and a floating probe (i.e.

Après 4, 5 ou 6 jours de culture, le nombre des cellules germinales est toujours plus élevé dans les ovaires cultivés dans du milieu supplémenté en thymuline, ou en présence. de

Below, we employ these radar measurements of the convection flow, in conjunction with our knowledge of the motion of the OCB, to estimate the dayside reconnection voltage during

We model atmospheric and non-tidal oceanic loading effects on surface gravity variations, us- ing global surface pressure field provided by the European Centre for Medium-range

There are very small discrepancies (usually only in the inclusion or exclusion of a final zero) between the ICT values and some national reprintings of the International

1.5d, Figure 10b), the averaged TC-driven flux anomaly is negative in the North West Atlantic, North West Pacific, North East Pacific, Arabian Sea and South West Indian, and is