@prefix this: . @prefix sub: . @prefix schema: . @prefix np: . @prefix dct: . @prefix npx: . @prefix freq: . @prefix xsd: . @prefix orcid: . @prefix rdfs: . @prefix dcat: . @prefix fip: . @prefix prov: . sub:Head { this: np:hasAssertion sub:assertion; np:hasProvenance sub:provenance; np:hasPublicationInfo sub:pubinfo; a np:Nanopublication . } sub:assertion { a freq:Digital-Object-Analysis; rdfs:comment "OH, ozone, NO3-radical, HO2** The oxidant concentrations are used in the description of secondary aerosol formation (sulfate and SOA). OH, ozone, NO3 and H2O2 (formed by HO2) are relevant for the oxidation of DMS, SO2, isoprene, and monoterpenes. 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-DOA7 | Oxidant concentration"; schema:identifier ; fip:has-description-source ; freq:digital-object-type ; dcat:contactPoint orcid:0000-0001-5441-4063 . } sub:provenance { sub:assertion dct:creator orcid:0000-0001-8784-9100 . } sub:pubinfo { this: dct:created "2025-12-28T21:04:09Z"^^xsd:dateTime; dct:creator ; dct:license ; npx:introduces ; npx:supersedes ; prov:wasDerivedFrom . sub:sig npx:hasAlgorithm "RSA"; npx:hasPublicKey "MIGfMA0GCSqGSIb3DQEBAQUAA4GNADCBiQKBgQCoKFb7LKlXyBB7BUvjFF9bDJNk0WxH3Xerr4H3v/VCiRVshEDl3BZVekbMMmdRe+TOPyc8AOLd9IAL2VfVVD/T0rmCHk7Pw7DQjI96mwyeXhE7f4g0WG5UT5Pxxm0Rzy7IrYnEaaVDs7dkZUt952M6qWlHfTwCQDcXJhZfLiXoMwIDAQAB"; npx:hasSignature "dipMqQKbdBtektG5waRBiobXx8lQNu47Riwb8w1v6BoVH319RPvW8cj9T4cO89gmLgAMw+5S9aUkw+pgJTBy6zRXOyznXDIUy8sBvd1X7OF01re565iK4nCu/b/naI0iQo/75fHBNCtBfI1X7ESuypqgBXrhhTGnyyX1CU1GlyQ="; npx:hasSignatureTarget this: . }