<?xml version="1.0"?>
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    <AnnotationProperty rdf:about="http://purl.obolibrary.org/obo/IAO_0000115"/>
    


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    <!-- http://purl.obolibrary.org/obo/ENVO_00000097 -->

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        <rdfs:label rdf:datatype="http://www.w3.org/2001/XMLSchema#string">desert</rdfs:label>
    </Class>
    


    <!-- http://purl.obolibrary.org/obo/ENVO_01000382 -->

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        <rdfs:label>cold desert</rdfs:label>
        <rdfs:subClassOf rdf:resource="http://purl.obolibrary.org/obo/ENVO_00000097"/>
        <ns2:IAO_0000115 rdf:datatype="http://www.w3.org/2001/XMLSchema#string">A cold desert is a desert which has hot summers and cold, dry winters with temperatures below 0 degrees Celsius</ns2:IAO_0000115>
        <rdfs:comment rdf:datatype="http://www.w3.org/2001/XMLSchema#string">This variant of the desert climate is somewhat rare outside of Asia. A cold desert climate is typically found in temperate zones, almost always in the rain shadow of high mountains which restrict precipitation from the westerly winds, or in the case of Central Asia, from the monsoon. The Gobi desert in Mongolia is a classic example of a region with a cold desert climate. Though hot in summer, it shares the very cold winters of the rest of Central Asia. The Kyzyl Kum and Taklamakan deserts of Central Asia and the drier portions of the Great Basin Desert of the western United States are other major examples of BWk climates. The Ladakh region, lying in the Great Himalayas in India also has a cold desert climate.</rdfs:comment>
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