Division de Coeurs Doux à Trois Chiffres Avec un Diviseur Manquant (A)

Figure 5 shows a two-layer structure of the SABL south of the Hoggar mountains, with a clean air layer (up to 1.5 km above ground level) advected from the east underneath a dust

By comparing the data of relative humidity, temperature and water vapor volume mixing ratio at two different heights (near-surface, ∼ 23 m above the surface), we demonstrate that

The ExoMars Atmospheric Mars Entry and Landing Investigation and Analysis (AMELIA) experiment in 2016 aimed to exploit the engineering data recorded during

H.: Global atmospheric effects of massive smoke injections from a nuclear war: Results from general circulation model simulations, Nature, 308, 21–25, 1984.

In contrast to many studies that adopt a de facto local view of land– atmosphere coupling (i.e., relating the land surface conditions and atmosphere at a particular point or

measured parameters were used to calculate soil parameters such as porosity, water content, density and grain surface area necessary to obtain geohydraulic parameters such as

Variations of the slope M of the linear regression with the mean square root of age, (a) for the South Atlantic Ocean and (b) for the East Indian Ocean... Ridge height variations

the following picture: incident magnetosheath ULF waves (possibly generated near the bow shock) lead to enhanced fluctuation amplitudes at the magnetopause because of res-