Temps Écoulé Jusqu'à 5 Heures, à Intervalle de 15 Minutes/Secondes (A)

Topographic images of selected dust particles from one to a few tens of micrometres in size show a variety of morphologies, ranging from compact single grains to large porous

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.

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

Here we report measurements of a suite of nine elemental ratios (Li/Ca, B/Ca, Na/Ca, Mg/Ca, Zn/Ca, Sr/Ca, Cd/Ca, Ba/Ca, and U/Ca) in 18 species of benthic marine invertebrates

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

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