{ "items" : [
    { "id" : "http://dbpedia.org/resource/Siberian_High"
      "properties" : {
        "http://www.w3.org/2000/01/rdf-schema#comment" : [ "The Siberian High (also Siberian Anticyclone) is a massive collection of cold or very cold dry air that accumulates on the northeastern part of Eurasian terrain for the cold part of the year, roughly from September till April. Usually, it is centered on Lake Baikal. It reaches its greatest size and strength in the winter, when the air temperature near the center of the high-pressure cell or anticyclone is often lower than −40 °C (−40 °F)."] } } }
