Motif d'Images de la Saint Valentin avec la Forme Comme Attribut Seulement (A)

size but also slightly on the refractive index, is around 1.94. Figure 7c shows the low values obtained for the SSA express- ing the strong absorbing capability of these aerosols.

the AMS mass spectra are consistent with the large particle results and that the mass spectra in the largest (below one micron) and in the smallest (below 100 nm) size ranges de-

Further- more the coarse mass variations are weaker than the seasonal and diurnal cycles of the fine fraction (see Table 2), while PM 1−10 and the respective diurnal cycle amplitude

WINDII measures wind, temperature, and emission rate over the altitude range 80 to 300 km by using the visible region airglow emission from these altitudes as a

Between October 15 and November 8, 1988, the Goddard Space Flight Center mobile stratospheric lidar was in place at the (JPL) Table Mountain Facility (located at 34.4øN, 117.7øW)

Our calculations show that the low de- polarization values of the lidar signal from the bottom of the Pinatubo layer can be explained assuming poly- dispersions

(2006) explored the multifractal structure of pedodiversity at global scale estimating the spectra of singu- larities and the spectra of generalized dimensions or R´enyi

Time series of NO 2 enhancement after the solar proton events of October–November 2003 for the Northern Hemisphere polar cap (70–90 ◦ N) at nighttime conditions as measured by MIPAS