Citadins, Jipaï

(1979) stationary neutral atmosphere is likely to under- estimate the Joule heating term (Eq. 7) and thus overestimate L=J in this case, where the background neutral wind is

Based on the salinity field (not shown), we have marked the dominant pathways of BSW. Several paths can be seen, starting with a spreading of the brackish waters at the north, west

The UCL CMAT GCM has been used to simulate the period from 12:00 UT on 23 October to 12:00 UT on 3 November 2003, during which the Earth experienced extremely high levels of

From ionospheric height variations at three stations, one at the magnetic equator, and the others at the low-latitude re- gions, which are magnetically conjugate in the same mag-

Figure 9c shows the discrimi- nating statistic of the reduction error for the energetic ions (tall line) and the surrogate data (short line) corresponding to the difference of

After 11:00 UTC surface air temperature starts to recover (Fig. 2b) although it does not.. Amiridis et al. Title Page Abstract Introduction Conclusions References Tables Figures ◭ ◮

Models that hope to predict global temperature or total ozone over long time scales should be able to duplicate the long-range correlations of temperature and total ozone as shown

simplified calculations, they estimate that the the long term effect of planetary wave activity positive correlation of the temperature with in the upper stratosphere