LEADER 01875nam  2200433z- 450 
001 9910347051803321
005 20210211
035   $a(CKB)4920000000101998
035   $a(oapen)https://directory.doabooks.org/handle/20.500.12854/56869
035   $a(oapen)doab56869
035   $a(EXLCZ)994920000000101998
100   $a20202102d2014      |y         0
101 0 $aeng
135   $aurmn|---annan
181   $ctxt$2rdacontent
182   $cc$2rdamedia
183   $acr$2rdacarrier
200 00$aPrecipitation statistics from regional climate model at resolutions relevant for soil erosion
210   $cKIT Scientific Publishing$d2014
215   $a1 online resource (XX, 177 p. p.)
225 1 $aWissenschaftliche Berichte des Instituts für Meteorologie und Klimaforschung des Karlsruher Instituts für Technologie
311 08$a3-7315-0227-5 
330   $aA major source of uncertainty in regional climate model simulations arises from the convection parameterisation. Increasing spatial resolution to the so-called convection-permitting scale allows switching off most of the convective parameterisations. Several studies prove the benefits of this spatial scale, but none of them is based on climatological time-scale (i.e. 30 years) as this research.
606   $aPhysics$2bicssc
610   $aatmospha?rische Prozesse
610   $aatmospheric processes
610   $aclimate change signal
610   $aconvection
610   $aconvection-permitting scale
610   $aKlimawandel-Signal
610   $aKonvektion
610   $aregional climate model
610   $aRegionale Klimamodelle
615  7$aPhysics
700   $aFosser$b Giorgia$4auth$01307611
906   $aBOOK
912   $a9910347051803321
996   $aPrecipitation statistics from regional climate model at resolutions relevant for soil erosion$93028852
997   $aUNINA