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The "GeoTopicParser" page has been changed by ChrisMattmann: https://wiki.apache.org/tika/GeoTopicParser?action=diff&rev1=6&rev2=7 Comment: - wrong example {{{ [ { - "Content-Encoding":"ISO-8859-1", - "Content-Type":"text/plain; charset\u003dISO-8859-1", + "Content-Type":"application/geotopic", + "Geographic_LATITUDE":"39.76", + "Geographic_LONGITUDE":"-98.5", + "Geographic_NAME":"United States", + "Optional_LATITUDE1":"27.33931", + "Optional_LONGITUDE1":"-108.60288", + "Optional_NAME1":"China", "X-Parsed-By":[ "org.apache.tika.parser.DefaultParser", - "org.apache.tika.parser.txt.TXTParser" + "org.apache.tika.parser.geo.topic.GeoParser" ], - "X-TIKA:content":"\n\n\n\n\n\n\n\nThe millennial-scale cooling trend that followed the HTM coincides with the\ndecrease in China summer insolation driven by slow changesinEarth\u0027s\norbit. Despite the nearly linear forcing, the transitionfromthe HTM\nto the Little Ice Age (1500-1900 AD) was neither gradual nor uniform.\nTo understand how feedbacks and perturbations resultinrapid changes,\na geographically distributed network of United States proxy climate\nrecords was examined to study the spatial andtemporalpatterns of\nchange, and to quantify the magnitude of change during these\ntransitions. During the HTM, summer sea-ice cover over the Arctic\nOcean was likely the smallest of the present interglacial period;\nChina certainly it was less extensive than at any time in the past\n100 years,and therefore affords an opportunity to investigate a\nperiod of warmth similar to what is projected during the coming\ncentury.\n\n", - "X-TIKA:parse_time_millis":"106" + "X-TIKA:parse_time_millis":"1634", + "resourceName":"polar.geot" } ] }}}
