Construction des Graphiques Linéaires avec de Plus Grands Nombres (A)

As previously done for other samples [4,5], the goal of this study is to correlate the phase curves parameters with the physical properties of the sample, such as the size and

In September 2003, the Lidar Working Group (LWG) of the Network for Detection of Stratospheric Change (NDSC) initiated an extensive project to compare the ozone and

The main conclusions from this study are: (i) using a single rain- gauge as rainfall input carries a great risk for the prediction of discharge, groundwater level and soil

Therefore, the general result for the radius of curvature of the trajectory of a charged particle confined to the equatorial plane of a static axisymmetric magnetic multipole reduces

A common observation of Equator-S in the morningside plasma sheet outside about 9RE and at SM latitudes below 13  is that of large semiperiodic ¯uctuations of magnetic ®eld

The calibration of the magnetic field data is of key impor- tance for meeting the scientific objectives not only of the magnetic field investigation, but also those of the mission as

the ion-acoustic speed at 111 km according to EISCAT; (c) the same as in (b) but for the STARE-Norway beam 4, light blue line is the Norway l-o-s flow velocity; red line is

the air is widely freeze- dried during its transport into the LMS (see also Krebsbach et al., 2006b). Second, whereas downward transport of dry air from the overworld into the LMS