Nanopublication

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ID

https://w3id.org/np/RAWGVZ9sq3kUMq6CvzdNwIJqBgrSIhahmFvXGre3M3fw0

Formats

.trig | .trig.txt | .jelly | .jelly.txt | .jsonld | .jsonld.txt | .nq | .nq.txt | .xml | .xml.txt

Content

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@prefix fip: <https://w3id.org/fair/fip/terms/> .
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sub:Head {
  this: a np:Nanopublication;
    np:hasAssertion sub:assertion;
    np:hasProvenance sub:provenance;
    np:hasPublicationInfo sub:pubinfo .
}

sub:assertion {
  sub:F2A-CS1-DOA3 a freq:Digital-Object-Analysis;
    rdfs:comment "Ozone concentration climatologies are used in the radiative transfer calculations. The ozone climatologies used in NorESM2 have a 5-day frequency, vary in height and latitude, but have no longitudinal dependce. They are based on simulations with CESM2-WACCM (Danabasoglu et al., 2019).";
    rdfs:label "F2A-CS1-DOA3 | Ozone concentration";
    fip:has-description-source <https://noresm-docs.readthedocs.io/en/noresm2/configurations/input.html#>;
    freq:digital-object-type <https://w3id.org/gff/rao/terms/Simulation-Data>;
    dcat:contactPoint orcid:0000-0001-5441-4063 .
}

sub:provenance {
  sub:assertion dct:creator orcid:0000-0001-8784-9100 .
}

sub:pubinfo {
  this: dct:created "2025-12-28T18:47:24Z"^^xsd:dateTime;
    dct:creator <https://fip.fair-wizard.com/wizard>;
    dct:license <https://creativecommons.org/publicdomain/zero/1.0/>;
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