This paper describes the third full release of the Rossby Centre Regional Climate model (RCA3),
with an emphasis on changes compared to earlier versions, in particular the …

… bases less than 100 m (darkest), 100–300 m, 300–600 m, and 600–1000 m. Values 1000–3000
m are indicated with dense diagonal lines and values above 3000 m with coarser lines. …

… for an analysis of a number of surface‐related parameters: 2 m temperature, minimum and
maximum daily temperatures, 10 m wind, and daily precipitation. The analysis is done on a …

… extreme values of 2 m temperature and 24 h accumulated precipitation. However, no added
value in the HIRLAM reanalysis could be quantified for the wind speed at 10 m over land. …

… 𝑀/𝑠 Reaction rates describing transports between the compartments in the model. … is divided
into a number of M groups and the calibration is then done M times where each time one of …

Molecules exchange between the nucleus and the cytosol occurs through nuclear pore
complexes(NPCs), which are 66 MDa complexes embedded in the nuclear envelope. The yeast …

… The invagination into the postsynaptic dendrite of some HRP-stained boutons of the present
study, as well as of M boutons following rhizotomys and of M boutons into intracellularly …

… of the deep layer is 1.0m in mountainous areas and 2.2m elsewhere. There is no relaxation
of soil moisture, thus runoff from the deep layer can be used as input to a routing scheme. …

… m) and to the value of z0m for small values on z0m (< 0.1 m). The presently relatively thick (90
m… been forced to assume z0h = z0m = 0.2 m for snow free open land. Thus the Zilitinkevich …

This report describes the physical processes as part of the surface scheme in the Rossby
Centre Regional Atmospheric Climate Model (RCA4). Or more strictly for the version used for …