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Tendencies in climate changes in Poland and Ukraine during the last centuries and their causes

100%
Boryczka J., Stopa-Boryczka M., Mucha B., Miłaszewska M.
Miscellanea Geographica. Regional Studies on Development
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2008
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vol. 13
77-88
EN
The paper describes tendencies in changes of air temperature in Poland and Ukraine on the basis of a long series of measurements made in Warsaw (1779-2000), Cracow (1826-2000), Lviv (1824-2002) and Kiev (1812-2002). Air temperature in these cities in the years 1825-2002 is positively correlated with the North Atlantic Oscillation (NAO) Index. Values of the r correlation coefficient are much higher in winter months than during the summer and they decrease with distance from the Atlantic Ocean. Of interest are air temperature changes in Warsaw, Cracow, Lviv and Kiev in the XIXth -XXth centuries together with forecasts until the year 2100. Significant dependence of the climate of Poland and Ukraine on the NAO index stems from similar temperature cycles and the eight-year, eleven-year and one-hundred-year NAO index. Forecast credibility results from the similar periodicity of air temperature, the NAO index and solar activity. The forecast mean annual temperature values for 2001-2100 were obtained from the interference of statistically important temperature cycles, determined by the sinusoidal regression method.
2
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Warming and cooling of the Earth's climate and their causes

100%
Boryczka J., Szmajda D.
Miscellanea Geographica. Regional Studies on Development
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2006
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vol. 12
31-41
EN
The progressing wanning of the Earth's climate is mainly caused by natural factors, that is, the increasing solar activity and the decreasing volcanic activity on the Earth. The aspects which testify to the predominance o f natural factors include: synchronous changes in the average air temperature in the Northern Hemisphere in the years 1856-2002, the average consecutive 11-year Wolf numbers and the location of the mass centres o f the four largest planets. Natural causes o f the climate warming are corroborated by the synchronicity o f changes in the carbon dioxide concentration and paleotemperature in the last 450,000 years, revealed on the basis o f an analysis o f the ice core in Antarctica. Periods o f climate warming occur every 100,000 years and are caused by an increased solar radiation in high latitudes, resulting from changes in the Earth's orbit and the inclination of the Earth axis (according to the popular Milanković theory).
3
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The influence of the North Atlantic Oscillations (NAO) on the climate of Warsaw and Lviv

100%
Boryczka J., Mucha B., Stopa-Boryczka M., Wawer J.
Miscellanea Geographica. Regional Studies on Development
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2006
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vol. 12
75-80
EN
The objective of the work is to determine the periodicity and trends of change in air temperature in Warsaw and in Lviv during the 18th-20thcenturies, together with the forecast for the years 2000-2100. There are interesting diagrams of temporal changes of the North Atlantic Oscillation (NAO) indicator and air temperature, with the forecast reaching the year 2100. The forecasts were obtained on the basis of interpretations of the Sun activity and the NAO indicator cycles, determined with the method of ”regression sinusoids”. The fluctuations of air temperature and North Atlantic Oscillation during winter in Warsaw and in Lviv are closely correlated.
4
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Heat and Cold Waves in an Annual Cycle Air Temperatures in Warsaw (1951-2010)

100%
Stopa-Boryczka M., Boryczka J., Kossowska-Cezak U., Wawer J.
Miscellanea Geographica. Regional Studies on Development
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2011
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vol. 15
103-114
EN
Heat and cold waves in Warsaw (the Okęcie district) have been determined determined basing on daily average air temperature values in Warsaw (the Okęcie district), measured for 60 years between 1951 and 2010. Air temperature cycles, i.e. periods, amplitudes and phases have been determined by means of a sinusoidal regression method. Especially worth noting are 15 to 18-day long cycles of air temperature in given months (e.g. 16-day long cycles during 6 months: March, April, May, August, September, and October). Heat and cold waves result from interferences of cycles whose duration ranges from several to teen days of daily temperature values, and long-term cycles of average annual temperature.
5
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Wykorzystanie transformaty Fouriera oraz transformaty falkowej do analizy przebiegów odkształconych

84%
Bartman J., Sobczyński D.
Acta Scientifica Academiae Ostroviensis. Sectio A, Nauki Humanistyczne, Społeczne i Techniczne
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2017
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issue 10(2)/2017
124-135
PL
Praca poświęcona jest zagadnieniu analizy elektrycznych przebiegów odkształconych. Przedstawiono w niej podstawy analiz częstotliwościowych bazujących na Dyskretnej Transformacie Fouriera (DFT) oraz analiz czasowo-częstotliwściowych realizowanych z wykorzystaniem Dyskretnej Transformaty Falkowej (DWT). W końcowej części pracy pokazano wykorzystanie obu metod do analizy prądu odkształconego pobieranego przez obrabiarkę numeryczną.
EN
The work is devoted to the problem of analysis of electric waveforms distortion. It presents the basis for frequency-based analysis using on Discrete Fourier Transform (DFT) and time-frequency analysis using Discrete Wavelet Transform (DWT).The final part of the paper presents the use of both methods for the analysis of current distortion by a machine CNC.
6
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Cyclic changes of climate in Europe during the last millenium according to dendrological data

84%
Boryczka J., Stopa-Boryczka M., Bijak S., Miłaszewska M.
Miscellanea Geographica. Regional Studies on Development
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2008
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vol. 13
57-66
EN
The paper discusses periodic climate changes in Europe determined on the basis of dendrochronological data dating back one thousand years. In tree-ring width sequences of trees growing in Poland there are approximately 8-, 11-, 100- and 180- year periods. The tree-ring widths of oaks growing in Poland for the last centuries are characterised, without any significant amplitude, by 8- and 11-year periods (Tab. 1). In turn, chronologies of pine, spruce, larch, oak and fir growing in Europe are characterised by 100- and 180-year periods (Tab. 2). Cycles of dendrochronological variables approximate cycles of air temperature and North Atlantic Oscillation NAO as well as those of solar activity. The forecast of annual growth (ring width) for 2001-2100 was calculated by interference of the tree-ring width cycles determined by the sinusoidal regression method. Because of much longer empirical sequences of specific periods, the credibility of forecasts for treering widths is greater than that for air temperature.
7
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Nile Red - barwnik kontrastujący cyjanoakrylan

84%
Rogoża E., Drzewiecka K.
Problemy Kryminalistyki
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2015
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issue 290
58-64, 115-120
PL
Ślady linii papilarnych ujawniane metodą cyjanoakrylową na podłożach niechłonnych w celu poprawy czytelności wymagają dodatkowego kontrastowania barwnikami fluorescencyjnymi. Nile Red zaliczany jest do jednych z nich. Skuteczność jego działania sprawdzono w warunkach zbliżonych do codziennej praktyki laboratoryjnej. Najwyższa fluorescencja Nile Red wystąpiła przy wzbudzeniu światłem niebieskozielonym w długości fali 505 nm. Analiza widm spektralnych wykazała, że emisja światła oscyluje w zakresie długości fali około 630 nm. W celu odcięcia światła wzbudzającego fluorescencję można użyć filtrów krawędziowych długofalowych barw: żółtej, pomarańczowej lub czerwonej. Wybór filtra uzależniony jest od charakterystyki podłoża i można dobrać go doświadczalnie. Fluorescencja Nile Red nie ulega zmianie w dłuższym przedziale czasowym, co pozwala na wykonanie rejestracji śladów w terminie dogodnym dla wykonującego badania, bez obawy o utratę ich jakości. Nile Red może być alternatywą dla innych barwników fluorescencyjnych wykorzystywanych w wizualizacyjnych badaniach daktyloskopijnych.
EN
Fingerprints disclosed by cyanoacrylate on non-absorbent substrates, in order to improve readability, require additional contrasting fluorescent dyes. Nile Red is one of them. Its effectiveness was tested under conditions similar to those of daily laboratory practice. The highest Nile Red fluorescence occurred in an excitation light of blue-green and a wavelength of 505nm. Spectral analysis showed that the emission of light oscillates in the wavelength of about 630nm. In order to cut off the light, longpass edge filters of the colours yellow, orange or red can be used. Filter selection depends on the characteristics of the substrate and can be chosen empirically. Nile Red fluorescence does not change over a longer period of time, which allows for the registration of fingerprints to be performed within a time convenient for the testing, without fear of losing their ąuality. Nile Red may be an alternative to other fluorescent dyes used for visualization in fingerprint testing.
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