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@prefix sub: <https://w3id.org/np/RAD1b59koA6QMH4DJCwH2qQNM74jP8ys5w8OGilgFFclI/> .
@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 {
  sub:F2A-CS1-DOA5 a freq:Digital-Object-Analysis;
    rdfs:comment "Production of H2O from methane oxidation is prescribed using a climatologies based on simulations with CESM2-WACCM. This source is especially relevant in the stratosphere. These climatologies have a monthly frequency, and a 3-dimensional spatial distribution. They are based on simulations with CESM2-WACCM (Danabasoglu et al., 2019).";
    rdfs:label "F2A-CS1-DOA5 | Water vapour emissions";
    schema:url <https://ns16001b.web.sigma2.no/datalake/inputdata/>;
    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 "2025-12-28T21:35:18Z"^^xsd:dateTime;
    dct:creator <https://fip.fair-wizard.com/wizard>;
    dct:license <https://creativecommons.org/publicdomain/zero/1.0/>;
    npx:introduces sub:F2A-CS1-DOA5;
    prov:wasDerivedFrom <https://w3id.org/fip/wizard/57fd4ae7-c55b-4e90-b3dd-eef6baeb1254> .
  
  sub:sig npx:hasAlgorithm "RSA";
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    npx:hasSignatureTarget this: .
}