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

This sequence of tests proved su fficient to detect even small errors (some digitising errors, some errors in the originally recorded data) with statistical techniques, but it

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