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<md:lastName>Anwandter</md:lastName>
<md:firstName>Carlos</md:firstName>
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<md:year>1859</md:year>
<md:title>Temperature measurements in Valdivia, Chile from September 1851- December 1854, digitized version</md:title>
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<md:lastName>Dove</md:lastName>
<md:firstName>HW</md:firstName>
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<md:year>1859</md:year>
<md:title>Über die nicht periodischen Veränderungen der Temperatur-Vertheilung auf der Oberfläche der Erde</md:title>
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<md:pages>428 pp</md:pages>
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<md:westBoundLongitude>-73.24</md:westBoundLongitude>
<md:eastBoundLongitude>-73.24</md:eastBoundLongitude>
<md:southBoundLatitude>-39.811</md:southBoundLatitude>
<md:northBoundLatitude>-39.811</md:northBoundLatitude>
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<md:label>CHIVLD1</md:label>
<md:latitude>-39.811</md:latitude>
<md:longitude>-73.24</md:longitude>
<md:elevation>9.0</md:elevation>
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<md:name>Chile</md:name>
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<md:name>Weather station/meteorological observation</md:name>
<md:optionalName>WST</md:optionalName>
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<md:size unit="data points">48</md:size>
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<md:name>Creative Commons Attribution 3.0 Unported</md:name>
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<md:comment>He had a thermometer divided in 80º in Reaumur scale. The instrument was suspended 20 foot above the sea level.
---
The data of this dataset might have been revised during the review process. This might therefore be an old version. To be sure, please check the respective dataset at doi:10.1594/PANGAEA.871480</md:comment>
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<md:comment>in Reamur, mean, series 1</md:comment>
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