Conversions métriques/impériales -- Pouces à centimètres (1/8 pouces) (A)

In the Arctic (60 ◦ –90 ◦ N) in spring, lower stratospheric ozone (Fig. 8b) and total column ozone (Fig. 6e) follow a similar evolution to spring-time Antarctic ozone, but with

In spite of impressive advances in recent years, our present understanding of organic aerosol (OA) compo- sition, physical and chemical properties, sources and trans-

verted into its reservoir species (next subsection) and mixing with ambient air becomes more important, ozone chemistry in the aging plume depends on whether emissions are de-

deep stratospheric intrusion event is further investigated and supported by model cal- culations with the Lagrangian particle model FLEXPART as well as with the ECMWF global

Annual mean radiative forcing by the total (cloud albedo and cloud lifetime) aerosol indirect effect (Wm − 2 ) as simulated using the original parameterizations by (a) LMDZ and

The method is applied to data from an anaerobic digestion process and shows that even a model including a single biomass is sufficient.. Then we apply the same method to the

tation at the global scale of the new generation land surface model ISBA-A-gs and (2) to validate the simulated LAI by using three satellite-derived data sets (ISLSCP-II [Los et

[ 55 ] The Siberian Platform has a high-velocity root extending to 200 – 225 km depth whose eastern boundary closely matches the geologically mapped boundary of the platform along