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@prefix sub: <https://w3id.org/np/RALvRULnlkX6EvWmpO-1zqLa6j9_2ce0LPBw4KLt9SDj4/> .
@prefix schema: <https://schema.org/> .
@prefix np: <http://www.nanopub.org/nschema#> .
@prefix dct: <http://purl.org/dc/terms/> .
@prefix npx: <http://purl.org/nanopub/x/> .
@prefix freq: <https://w3id.org/fff/req/> .
@prefix xsd: <http://www.w3.org/2001/XMLSchema#> .
@prefix orcid: <https://orcid.org/> .
@prefix rdfs: <http://www.w3.org/2000/01/rdf-schema#> .
@prefix dcat: <https://www.w3.org/ns/dcat#> .
@prefix fip: <https://w3id.org/fair/fip/terms/> .
@prefix prov: <http://www.w3.org/ns/prov#> .

sub:Head {
  this: np:hasAssertion sub:assertion;
    np:hasProvenance sub:provenance;
    np:hasPublicationInfo sub:pubinfo;
    a np:Nanopublication .
}

sub:assertion {
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      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";
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    fip:has-description-source <https://noresm-docs.readthedocs.io/en/noresm2/configurations/input.html#>;
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}

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

sub:pubinfo {
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    dct:creator <https://fip.fair-wizard.com/wizard>;
    dct:license <https://creativecommons.org/publicdomain/zero/1.0/>;
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    npx:hasSignatureTarget this: .
}