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Titlebook: Climate Change in Poland; Past, Present, Futur Małgorzata Falarz Book 2021 Springer Nature Switzerland AG 2021 Climate Change in Poland.Tre

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https://doi.org/10.1007/3-540-07483-Xhave been held every year, bringing together representatives from almost all countries of the world and resulting in important global agreements on combating global warming (e.g. the Kyoto Protocol in 1997, Paris Agreement in 2015).
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2352-0698 umerous colored maps and charts.Presents new research and pr.This edited book provides a comprehensive overview of the past, present and future climate development in Poland. The book consists of three main parts. The first part presents the results of the study of climate change before instrumental
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William Burke,Andrew Malcolm Cole Attention was paid to long-term trends and extreme values, including the number of days with specific air temperature thresholds. All characteristics have been compiled for the period 1951–2018. Changes in the average air temperature since the beginning of their operation were assessed for three stations (Krakow, Warszawa, and Gdansk).
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Data and Methods of Investigationn Poland in the last millennium. More than 50 proxy series including documentary evidences, dendrochronological records and varved sediment records were analysed. On this basis, reconstructions of: summer and winter air temperature, winter severity, precipitation (liquid and solid) and droughts were
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Climate Change Before Instrumental Measurementsin the last millennium. Data for this period are gaining importance due to their comparability with modern instrumental data, which is possible thanks to their high temporal resolution (annual, seasonal). The authors compiled the research results of climate reconstruction based on the following avai
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Change of Atmospheric Circulationscales. The traditional manual classifications by Niedźwiedź and the well-known Grosswetterlagen were used. Simultaneously, an automatic classification was made by Ustrnul and Lityński and the NAO index was also measured for mutual comparison. All of the analyses concerned basically the main period
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Air Pressure Changehe years 1966–2018. The exceptions are the three mountain stations (Zakopane, Śnieżka and Kasprowy Wierch) for which the pressure values at the levels of these stations were used and, based on them, only the trends of changes in this meteorological element were determined. In addition, a series of m
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