Directorate-General for Agriculture and Rural Development of the European Commission. Short-term outlook for EU arable crops, dairy and meat markets in 20. Prace Geograficzne 128:123–134ĭaňhelka J and Šercl P (2011) Floods in the Czech Republic in 2010, Meteorologicke Zpravy 64(1), 4–9. Przegląd Geofizyczny 3-4:175–188Ĭebulska M, Twardosz R (2012) Temporal variability of maximum monthly precipitation totals in the Polish Western Carpathian Mts during the period 1951–2005. Pol J Agron 34:52–61Ĭebulska M, Twardosz R (2010) Temporal variability of the lowest monthly precipitation in the upper Vistula river (1901-2000). Theor Appl Climatol 97(3–4):297–315Ĭebulska M (2018) Periods without precipitation and with low precipitation in the Polish Carpathians in the years of 1984–2013. Weather 66(6:147–153īrázdil R, Trnka M, Dobrovolný P, Chromá K, Hlavinka P, Žalud Z (2009) Variability of droughts in the Czech Republic, 1881–2006. Routledge, London, New Yorkīissolli P, Friedrich K, Rapp J, Ziese M (2011) Flooding in eastern central Europe in May 2010 – reasons, evolution and climatological assessment. J Climatol 6:661–675īarry RG, Carleton AM (2001) Synoptic and dynamic climatology. The study confirms an influence of the direction of air mass advection and (anti)cyclonicity of flow on P max and P min.Īlexandersson H (1986) A homogeneity test applied to precipitation data. Both P max and P min are characterised by irregular fluctuations in precipitation totals, with no statistically significant trend in their changes, which reflects the absence of a trend as regards overall precipitation volumes in this area. P max demonstrates a more noticeable annual frequency pattern, with a predominance in summer months, while P min shows smaller variations in individual months. On account of the variation in their relief, the Polish Carpathians are an area with a very great temporal and spatial variability in precipitation, ranging from complete absence to 500 mm per month.
Ca precipitation totals series#
To achieve the above, use is made of 14 secular series (1881–2018) of precipitation from the Polish Carpathians and the calendar of circulation types over southern Poland prepared by T. This study aims to characterise the annual and long-term variability of the highest ( P max) and lowest ( P min) monthly precipitation totals and their relationship with atmospheric circulation. They are a consequence of weather anomalies and have many dangerous effects such as floods and droughts. Extreme climatic phenomena include prolonged heavy precipitation as well as long-lasting absence thereof.
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