Spectral nudging in regional climate modelling: How strongly should we nudge?

7 Correlation of observed ERSST time series averaged between 0 and 60 ◦ N in the Atlantic against the SST field in (a) ERSST (b-c) NUDG and HIST respectively, (d-e) DEC3 at

In the case of the Alps, the simulated increase of winter precipitation could offset temperature effects beyond a certain altitude, resulting in a less pronounced decrease or even

However, the text claims that only one class (group 1) does so. 29) that the DTE is to be seen as a complementation to an already existing grammar of the language as well

In addition, there is also a greater overlap with carbonaceous structures decomposition event, once (i) there is a remarkable increase in metallic particles size (Fig. 8)

Dans la catégorie moyenne ou second groupe, les 7 Bowl-Barrows avec banquette extérieure (volume moyen de 444 m³) forment, encore, le premier groupe volumétrique ;

4.2 Statistics of auroral observations and auroral oval We reconstruct the daily variation of aurora occurrence and its dependence on local time and position of the aurora on the

Anomalous emanation of radon ( 222 Rn) was ob- served preceding large earthquakes and is considered to be linked to preseismic electromagnetic phenomena (e.g. great changes

Regional climate downscaling with prior statistical correction of the global climate forcing.. Augustin Colette, Robert