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    <AnnotationProperty rdf:about="http://purl.obolibrary.org/obo/IAO_0000115"/>
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    <!-- http://purl.obolibrary.org/obo/ENVO_01001345 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/ENVO_01001345">
        <rdfs:label xml:lang="en">floating ice mass</rdfs:label>
    </Class>
    


    <!-- http://purl.obolibrary.org/obo/ENVO_01001517 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/ENVO_01001517">
        <rdfs:label xml:lang="en">drift ice mass</rdfs:label>
        <rdfs:subClassOf rdf:resource="http://purl.obolibrary.org/obo/ENVO_01001345"/>
        <oboInOwl:creation_date rdf:datatype="http://www.w3.org/2001/XMLSchema#dateTime">2019-01-14T19:46:20Z</oboInOwl:creation_date>
        <oboInOwl:hasDbXref>http://sweetontology.net/realmCryo/DriftIce</oboInOwl:hasDbXref>
        <oboInOwl:hasBroadSynonym>drift ice</oboInOwl:hasBroadSynonym>
        <rdfs:comment>Prior to approximately 2014, drift ice was synonymous with the various grades of pack ice, described as very open (with an ice concentration of 1/10 to 3/10), open (4/10 to 6/10, with many leads and polynyas and the floes generally not in contact with one another), close (7/10 to 8/10, composed of floes mostly in contact), very close (9/10 to less than 10/10), and compact (10/10, with no water visible, called consolidated pack ice if the floes are frozen together). This is deprecated, with pack ice now referring to drift ice with a concentration equal to or above 7/10; however, other usages are still common.</rdfs:comment>
        <ns3:IAO_0000115>A floating mass of ice which is 1) unattached to land or land-fast ice and 2) moved by the action of winds or currents.</ns3:IAO_0000115>
        <oboInOwl:created_by rdf:resource="https://orcid.org/0000-0002-4366-3088"/>
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