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Air temperature conditions in northern Nordaustlandet (NE Svalbard) at the end of World War II

Repozytorium Uniwersytetu Mikołaja Kopernika

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dc.contributor.author Przybylak, Rajmund
dc.contributor.author Wyszyński, Przemysław
dc.contributor.author Woźniak, Marta
dc.date.accessioned 2018-03-13T11:05:59Z
dc.date.available 2018-03-13T11:05:59Z
dc.date.issued 2018
dc.identifier.citation International Journal of Climatology 2018;1–17
dc.identifier.issn 1097-0088
dc.identifier.other https://doi.org/ 10.1002/joc.5459
dc.identifier.uri http://repozytorium.umk.pl/handle/item/5117
dc.description.abstract This article presents the results of an investigation into air temperature conditions in northern Nordaustlandet (NE Svalbard) based on meteorological observations made by German soldiers towards the end of World War II (1944/1945) and 4 months after its end. Traditional analysis using mean monthly data was supplemented by a detailed analysis based on daily data: maximum temperature, minimum temperature and diurnal temperature range. The latter kind of data made it possible to study such aspects of climate as the number of “characteristic days” (i.e., the number of days with temperatures exceeding specified thresholds), dayto-day temperature variability, and duration, onset and end dates of thermal seasons. The results from Nordaustlandet for the warmest period of the early 20th century warming period (ETCWP) were compared with temperature conditions both historical (the end part of the Little Ice Age) and contemporary (different sub-periods taken from the years 1981–2017) to estimate the range of warming during the ETCWP. Analysis reveals that the expedition year 1944/1945 in Nordaustlandet was, in the majority of months, the warmest of all analysed periods, that is, both historical and contemporary periods. The study period was markedly warmer than 1981–2010 (mean annual −6.5 vs. −8.4 °C) but colder than the periods 2011–2016 (−5.7 °C) and 2014–2017 (−5.8 °C). The majority of mean monthly air temperatures in the ETCWP lies within two standard deviations of the modern 2014–2017 mean. This means that values of air temperature in the study period lie within the range of recent temperature variability. All other thermal characteristics show changes in accordance with expectations associated with general warming of the Arctic (i.e., a decrease in diurnal temperature range and number of cold days, and an increase in number of warm days). The latter days were most common in the ETCWP.
dc.description.sponsorship Narodowe Centrum Nauki, Grant/Award number: 2015/19/B/ST10/02933
dc.language.iso eng
dc.publisher John Wiley & Sons, Inc.
dc.rights info:eu-repo/semantics/openAccess
dc.subject air temperature
dc.subject Arctic
dc.subject early instrumental data
dc.subject ETCWP
dc.subject Svalbard
dc.subject WWII
dc.title Air temperature conditions in northern Nordaustlandet (NE Svalbard) at the end of World War II
dc.type info:eu-repo/semantics/article


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