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  "collectionName": "DSS Borehole tempature reconstruction",
  "context": "context.jsonld",
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  "googleSpreadSheetKey": "13zzXd8DUmBu1_qKsb2SD-0M4UKrAGWFpcBoIxAq3qqc",
  "investigators": "van Ommen, Tas Morgan, Vin Elcheikh, Alan Dahl-Jensen, Dorthe",
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          ["temperature (LPD7abab671): paleoData_mostRecentCompilations: '' has been replaced by 'Temp12k-1_0_2, HoloceneAbruptChange-0_10_0'"]
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          ["temperature (LPD7abab671): interpretation1_seasonality: 'annual' has been replaced by ''"]
        ]
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    },
    {
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          ["temperature (LPD7abab671): paleoData_proxyDetail: 'borehole' has been replaced by ''"]
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    {
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      "curator": "nick",
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      "notes": "This marks the creation of the changelog, and marks the status of this dataset as of Temp12k version 1.0.1",
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          ["Changelog created"]
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  "pub": [
    {
      "author": [
        {
          "name": "Dahl-Jensen, Dorthe; Morgan, Vin I.; Elcheikh, Alan"
        }
      ],
      "abstract": "<jats:title>Abstract<\/jats:title>\n            <jats:p>The temperature profile in the 1200 m deep Dome Summit South (DSS) borehole near the summit of Law Dome, Antarctica, was measured in 1996, 3 years after the termination of the deep drilling.<\/jats:p>\n            <jats:p>The temperature profile contains information on past surface temperature over the last 4ka. This temperature history is determined by the use of a Monte Carlo inverse method in which no constraints are placed on the unknown temperature history and no solution is assumed to be unique. The temperature history is obtained from a selection of equally well-fitting solutions by a statistical treatment.<\/jats:p>\n            <jats:p>The results show that solutions covering the last 4ka have a well-developed central value, a most likely temperature history. The temperature record has two well-developed minima at AD 1250 and 1850. From 1850 to the present, temperatures have gradually increased by 0.7 K. The reconstructed temperatures are compared with the stable oxygen isotope (<ce><b4><jats:sup>18<\/jats:sup>O) from the DSS ice core.<\/jats:p>",
      "citeKey": "BZFR72FP",
      "dataUrl": "Manually Entered",
      "journal": "Annals of Glaciology",
      "page": "145-150",
      "pages": "145   150",
      "pubDataUrl": "doi.org",
      "publisher": "Cambridge University Press (CUP)",
      "title": "Monte Carlo inverse modelling of the Law Dome (Antarctica) temperature profile",
      "type": "article-journal",
      "volume": "29",
      "year": 1999,
      "doi": null,
      "issue": null
    },
    {
      "doi": null
    }
  ],
  "geo": {
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    "latitude": -66.7697,
    "elevation": "NA",
    "geometryType": "Point",
    "pages2kRegion": "Ant",
    "siteName": "Law Dome DSS",
    "subRegion": "unassigned",
    "countryOcean": "Antarctica",
    "gcmdLocation": "Antarctica"
  },
  "@context": "context.jsonld"
}
