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    <!-- 
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    <AnnotationProperty rdf:about="http://purl.obolibrary.org/obo/IAO_0000115"/>
    <AnnotationProperty rdf:about="http://www.geneontology.org/formats/oboInOwl#hasDbXref"/>
    


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    <!-- http://purl.obolibrary.org/obo/RO_0000057 -->

    <ObjectProperty rdf:about="http://purl.obolibrary.org/obo/RO_0000057">
        <rdfs:label xml:lang="en">has participant</rdfs:label>
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    <!-- http://purl.obolibrary.org/obo/RO_0000086 -->

    <ObjectProperty rdf:about="http://purl.obolibrary.org/obo/RO_0000086">
        <rdfs:label xml:lang="en">has quality</rdfs:label>
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    <!-- http://purl.obolibrary.org/obo/RO_0002234 -->

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        <rdfs:label xml:lang="en">has output</rdfs:label>
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    <!-- http://purl.obolibrary.org/obo/CHEBI_15377 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/CHEBI_15377">
        <rdfs:label>water</rdfs:label>
    </Class>
    


    <!-- http://purl.obolibrary.org/obo/ENVO_00010504 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/ENVO_00010504">
        <rdfs:label>surface layer</rdfs:label>
    </Class>
    


    <!-- http://purl.obolibrary.org/obo/ENVO_01000830 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/ENVO_01000830">
        <rdfs:label xml:lang="en">water-based rainfall</rdfs:label>
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    <!-- http://purl.obolibrary.org/obo/ENVO_01000896 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/ENVO_01000896">
        <rdfs:label xml:lang="en">freezing rainfall</rdfs:label>
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        <oboInOwl:hasDbXref>METAR:FZRA</oboInOwl:hasDbXref>
        <rdfs:comment xml:lang="en">A surface temperature inversion is usually required. In such an inversion, the surface must have a temperature below freezing, while the temperature of the atmosphere where the precipitation forms is above freezing. Alternately, if the temperature of the ground surface and glazed objects is typically near or below freezing (0C or 32F), it is necessary that the water drops be supercooled before striking. Freezing rain can sometimes occur on surfaces exposed to the air (such as tree limbs) with air temperatures slightly above freezing in strong winds. Local evaporational cooling may result in freezing. Freezing rain frequently occurs, therefore, as a transient condition between the occurrence of rain and ice pellets (sleet). When encountered by an aircraft in flight, freezing rain can cause a dangerous accretion of clear icing. In aviation weather observations, this hydrometeor is encoded ZR by NOAA.</rdfs:comment>
        <ns4:IAO_0000115 xml:lang="en">Water-based rainfall which freezes either 1) on impact with a surface to form a coating of clear ice (glaze) or 2) after percolating through surface layers.</ns4:IAO_0000115>
        <oboInOwl:hasDbXref rdf:resource="http://sweetontology.net/phenAtmoPrecipitation/FreezingRain"/>
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    <!-- http://purl.obolibrary.org/obo/PATO_0001306 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/PATO_0001306">
        <rdfs:label>decreased temperature</rdfs:label>
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    <!-- http://purl.obolibrary.org/obo/PATO_0001985 -->

    <Class rdf:about="http://purl.obolibrary.org/obo/PATO_0001985">
        <rdfs:label>frozen</rdfs:label>
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