Articles | Volume 22, issue 5
https://doi.org/10.5194/cp-22-957-2026
https://doi.org/10.5194/cp-22-957-2026
Research article
 | 
08 May 2026
Research article |  | 08 May 2026

Newly recovered series of meteorological measurements in SW Greenland (Nuuk) in the period 1806–1813

Rajmund Przybylak, Andrzej Araźny, Przemysław Wyszyński, Garima Singh, and Konrad Chmist

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Cited articles

Aguilar, E., Auer, I., Brunet, N., Peterson, T. C., and Wieringa, J.: Guidelines on climate metadata and homogenization, WMO/TD No. 1186, pp. 50, 2003. 
Axford, Y., Losee, S., Briner, J. P., Francis, D. R., Langdon, P. G., and Walker, I. R.: Holocene temperature history at the western Greenland Ice Sheet margin reconstructed from lake sediments, Quat. Sci. Rev., 59, 87–100, https://doi.org/10.1016/j.quascirev.2012.10.024, 2013. 
Baranowski, S.: Thermals of the periglacial tundra SW Spitsbergen, Acta Univ. Wratislaviensis, 68, Studia Geograficzne X, Wrocław, Poland, 1968 (in Polish). 
Borm, J., Kodzik, J., and Charbit, S.: Producing and communicating natural history in the long 18th century: Moravian observations concerning Greenland's climate in unpublished sources, Polar Rec., 57, 1–10, https://doi.org/10.1017/S0032247421000218, 2021. 
Box, J. E.: Survey of Greenland instrumental temperature records: 1873–2001, Int. J. Climatol., 22, 1829–1847, https://doi.org/10.1002/joc.852, 2002. 
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Short summary
This study presents and analyses a newly discovered unique series of meteorological measurements from Greenland, covering the period 1806–1813. This record, the longest instrumental dataset from the Arctic before 1840, provides valuable information for improving knowledge about the climate of that period. The analysis shows that it was one of the coldest intervals in the past two millennia. Intense volcanic activity and low solar activity are proposed as the main reasons for this cold period.
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