Placer en Ordre de Fractions et de Nombres Fractionnaires Négatifs avec des Numérateurs Semblables (A)

A case study objectively selected by means of a rotated principal component analysis over the diabatic field is analyzed to test the proposed parametrization.. This study highlights

Time evolution of the (NO) mixing ratio in the model box: 1, narrow plume; 2, basic, 3, wide plume, and circles, measured (NO) in cross section of various exhaust plumes over

Two conclusions are reached: (1) with an optimal set of solar-wind data available, the AE predictions are not markedly improved by the Dst input, but (2) the AE predictions are

Thermal, pressure and wind fields at ground level in the area of the Italian base at Terra Nova Bay, Victoria Land, Antarctica, as observed by a network of automatic weather

We ®nd, for instance, that in cases where the electron temperature is striated along B0 and low frequency waves (x  Xci) are excited in this environ- ment, for instance by a

From comparison of ground observations of auroral forms with meridional pro®les of particle ¯ux measured simultaneously by the low-altitude NOAA satellites above the ground

In layer 1 there are no magnetic field components for the VED (i.e. Computations of the electric field compo- nents are made following the procedure described in Sect. 4.2 using

In order to quantify the relative importance of the QBO cycle with respect to the annual variation in UV erythemal dose, we calculated the peak-to-peak amplitudes of the an- nual