Valeurs de position (unités aux centaines) (A)

The annual contours of the EW (zonal) and NS (meridional) components of the mean winds, as functions of height versus time, are shown in Fig.. The height co-ordinates are dif- ferent

The tradi- tional K¨ohler theory that describes the equilibrium growth of a droplet as a function of supersaturation explains well the CCN activation of water soluble

(2005) observed an early/fast type VLF perturbation in association with an optical elve captured during the EuroSprite2003 campaign, which constitutes indirect evidence for

By using data collected by the JULIA radar, along with TEC and GPS scintillations, we have constructed a very com- plete diagnostic of the background and the turbulent state of

A well established kinetic model predicts that steady upward field-aligned cur- rents should be linearly related to the potential drop along the field line, but collisionless

We concluded from these simulation studies that, if QP echoes were the result of the projection movement of gravity wave packets along the radar beam, then we can identify the slope

IRIS keeps the full ISSA resolution, it includes well-calibrated point sources, and the diffuse emission calibration at scales smaller than 1  was corrected for the variation of

The absence of a clear enhance- ment of the HONO-formation under UV-A light, as expected from the UV-A experiments on the humic acid coatings (i.e. by a factor of ≈3 under