SELECT ?property ?value WHERE { BIND (?? AS ?s) ?s ?property ?value . FILTER (isLiteral(?value)) } LIMIT 1000

Attributes

Strahlungskonvektionsmodell
radiative-convective model
modèle radiatif-convectif
modello radiativo-convettivo
Numerische Darstellung der Temperatur der Erdoberfläche als Resultierende der solaren Einstrahlung und der terrestrischen Ausstrahlung unter Einbezug der Konvektion.
Numerical representation of the surface temperature as a function of the solar energy absorbed from the Sun and the thermal radiation emitted to space by the Earth, resolving the temperature vertically.
2023-05-31T09:17:43.3595610Z
71507
https://www.termdat.bk.admin.ch/entry/71507
H. Schmidt et al., Globale Sicht des Klimawandels, 2017, S. 8, Kap. 2.1 ([Internet, 2022-12-21](https://pure.mpg.de/rest/items/item_2366061_4/component/file_3327202/content))
American Meteorological Society, Glossary, 2000, p. 618
ENS, M. Ghil, La Dynamique non-linéaire du climat, 2008
M. Giuliacci / P. Corazzon, Manuale di meteorologia, 2008
Dans un modèle Radiatif-Convectif, ou Modèle à 1 dimension, on représente la totalité de l'atmosphère d'une planète par une unique colonne composée d'un nombre discret de couches atmosphériques.
EXP: "RCM" ist die Abkürzung des englischen Namens "Radiative-Convective Model"; das Modell versucht neben der Wärmeleitung auch den Vorgang der vertikalen Durchmischung zwischen verschiedenen Schichten der Atmosphäre (Konvektion) zu erfassen
EXP: resolves many layers in the atmosphere and seeks to compute atmospheric and surface temperatures
EXP: "RCM" est l'abréviation de l'anglais "radiative-convective model"; le modèle est utilisé p.ex. pour étudier le rôle des constituants atmosphériques
EXP: simula il trasferimento di energia attraverso l'intera atmosfera, includendo le trasformazioni che avvengono durante l'assorbimento, l'emissione e la diffusione dell'energia, e il ruolo della convezione e dei moti verticali nel mantenere l'equilibrio
Laboratoire de Météorologie Dynamique, Equilibre radiatif-convectif, 2009
after K. McGuffie/Kendal, A Climate Modelling Primer, 2005, p. 121
nach Chr.-D. Schönwiese, Klimatologie, 2003, S. 243 und H. Von Storch / S. Güss, Das Klimasystem und seine Modellierung, 1999, S. 16
secondo M. Giuliacci / P. Corazzon, Manuale di meteorologia, 2008
nach Chr.-D. Schönwiese, Klimatologie, 2003, S. 243
after K. McGuffie/Kendal, A Climate Modelling Primer, 2005, p. 121
SELECT ?property ?object WHERE { BIND (?? AS ?s) ?s ?property ?object . FILTER (isIRI(?object)) FILTER (?property != rdf:type) FILTER (?property != rdfs:subClassOf) } LIMIT 1000
SELECT ?property ?subject WHERE { BIND (?? AS ?o) ?subject ?property ?o . FILTER (?property != rdf:type) FILTER (?property != rdfs:subClassOf) } LIMIT 1000
Incoming Relationships: No results found.
SELECT ?instance ?description WHERE { BIND (?? AS ?class) ?instance (rdf:type|owl:type) ?class . OPTIONAL { ?instance schema:description ?description . } } LIMIT 5000
Instances of this Class: No results found.
SELECT ?superclass ?description WHERE { ?? rdfs:subClassOf ?superclass . OPTIONAL { ?superclass (rdfs:comment|schema:description) ?description . } } LIMIT 5000
Superclasses of this Class: No results found.
SELECT ?subclass ?description WHERE { ?subclass rdfs:subClassOf ?? . OPTIONAL { ?subclass (rdfs:comment|schema:description) ?description . } } LIMIT 5000
Subclasses of this Class: No results found.