DEPOSITION OF DP SOFT RIME (DANGEROUS PHENOMENA) ON THE TERRITORY OF UKRAINE DURING THE PERIOD OF THE STANDARD CLIMATOLOGICAL NORM OF 1961-1990 AND FOR ITS SEPARATE DECADES

Author(s):  
S.I. Pyasetska

To clarify the features of the spatio-temporal distribution of soft rime deposits of the category DP (dangerous phenomena) over the course of the standard climatological norm of 1961-1990 materials of observations of such sediments were analyzed on a standard ice machine at all meteorological stations in Ukraine. The spatial-temporal character of the distribution of such sediments in the territory of Ukraine for each of the studied months of the cold and individual months of the transitional seasons of the year was obtained. Similar work was carried out for each separate decade during the total thirty-year study period. The years and months when such types of ice-rime deposits were the most were revealed, the contribution of each year and month to their total number was calculated. The places and regions of the greatest manifestation of DP category soft rime deposits on the territory of Ukraine during the standard climatological norm of 1961-1990 were established. A number of conclusions were obtained regarding the state of spatio-temporal distribution and the number of deposits of soft rime DP category during 1961-1990 on the territory of Ukraine, namely: – From 1961-1990, the largest number of cases of soft rime deposits of the DP category was observed in January, February and December of the study period. – In most cases, the vast majority of cases of frost deposition of the DP category were observed in the Transcarpathian region on the Play and in the Autonomous Republic of Crimea on the Ai-Petri . – Mostly the number of cases of such deposits at stations was isolated, but in some years and months at a number of stations there was a much larger number of such cases. January-December stands out the most, and among the Play and Ai-Petri stations. – The largest number of cases of soft rime deposits of the DP category was observed in the winter months, especially in January and December. During 1971-1980 and 1981-1990, a significant increase in such cases was observed in November, especially in 1971-1980. In the first decade of the standard climatological norm, this was not observed, the number of cases in March was equal to their number in November. – There is a tendency to increase the number of cases of DP soft rime deposits in December during 1971-1980 and 1981-1990, in contrast to 1961-1970, when the largest number was observed in January. – It is established that most cases of soft rime deposits of the DP category were observed during 1971-1980. – During 1961-1970, in January, cases of soft rime deposits of the DP category were quite common in Ukraine and were observed in 15 regions. The greatest spread of such deposits was observed in January 1964. Subsequently, the area of their distribution was reduced to several areas, of which they were most often observed in Transcarpathia in the Autonomous Republic of Crimea. Such deposits were quite common in December 1961-1970 and 1981-1990, when they were observed in 5-6 regions.

Author(s):  
Monika Mika ◽  
Monika Siejka ◽  
Przemysław Len

This article presents the results of analysis of the influence of selected economic, legal and environmental factors on the level of transaction prices of unbuilt land properties, in two randomly selected districts of the southern Poland. The results of the research allowed extraction of a group of factors influencing the spatial distribution of the average prices of the surveyed properties. They gave also the answer to the question about the extent to which the unit prices are confirmed by the state of properties management in the region. An analysis of the existing state in the selected region based on the analysis of the local market was performed. Furthermore, the conformity of local plans for the studied areas was examined, as well as an analysis of spatio-temporal distribution of transaction prices of real estate was performed. The research has shown that the level of transaction prices on the local real estate markets is related to the real estate management of the surveyed areas. The state of the economy is affected by many factors, most important of which seems to be the location in relation to urban areas and the condition of the access roads. The undertaken tests correspond with the directions of the world research.


As part of the research topic “Forecasting the variability of climate-vulnerable areas in Ukraine in the coming decades” (state registration number 0118U000554) a study of spatio-temporal distribution of ice category (dangerous) and SHP (spontaneous) was conducted in Ukraine at the present stage of climate change. The purpose of this article is to study the distribution of ice deposits of large diameters, namely dangerous (DHP) and spontaneous (SHP) in Ukraine during the current stage of climate change. It was also necessary to summarize the information on the identifi ed losses and their nature from ice deposits of the spontaneous (SHP) category, registered in some regions of Ukraine during this time. Main material. Dangerous ice deposits of the category are quite common in Ukraine and are observed almost every year. They are most common in the winter months (December-February) and in late autumn in November, when they are found in at least half of the regions. During 2011-2019, they were territorially observed in most oblasts, especially in the western, central and eastern regions. In the south, such deposits were mostly observed in Odesa, Mykolaiv, Kherson oblasts and the Autonomous Republic of Crimea. In April, such deposits were observed only in the Carpathian region of Transcarpathia in Playa. During October 2011-2019, dangerous ice deposits were found only in the Carpathian region (Zakarpatska and Ivano-Frankivsk regions), in some places in the center (Kirovohrad and Dnipropetrovsk regions) and in the south (Odessa, Mykolaiv, Kherson regions). Spontaneous ice deposition is observed in the territory not every month and year, but more o???? en in the cold period. The areas where they occur most o???? en are highlighted, namely in Transcarpathia at the Play weather station. However, there are places where such deposits also occurred quite often in the study period - in Lviv region (Kamyanka-Buzka, Rava-Ruska), Zhytomyr region (Olevsk, Zhytomyr), Mykolayiv region (Mykolayiv, Ochakiv), Donetsk region (Amvrosiyivka, Mariupol), Zaporizhzhia region (Zaporizhzhia, Huliaipole), the Autonomous Republic of Crimea (Chornomorske, Opasne, Simferopol). Damage from ice deposits of the SHP category was observed in 4 years out of 9 studied at the facilities of the industrial complex, transport and utilities. The largest number of losses was recorded in 2014. Conclusions. It was found that the most common dangerous ice deposits during 2011-2019 were in January, February, December, where they were observed in 10 to 14 regions, and especially in March in 21 region. They were most common in the western, central and eastern regions, and in the south in Odessa, Mykolaiv, Kherson regions and the Autonomous Republic of Crimea. Ice deposits of a spontaneous nature were mostly observed in the Zakarpatia region in Playa, as well as at some meteorological stations in Lviv, Zhytomyr, Mykolaiv, Donetsk, and Zaporizhzhia regions.


Author(s):  
S.I. Pyasetska

The article is devoted to the study of spatio-temporal distribution of DP (dangerous phenomena) frost deposits on the territory of Ukraine during the last 30 years, which characterize the current state and dynamics of the climate system in Ukraine and its individual elements. The aim of the study was to establish the features of spatio-temporal distribution of such sediments in the regions of Ukraine for individual decades of the study period and to outline the trend in their distribution. some increase in the incidence of such deposits in some months of the transition seasons. For the last decade, there has been an increase in such cases in January and December compared to previous decades. However, during the last 2 years the number of cases of frost deposits of the DP (dangerous phenomena) category has slightly decreased. It is proved that the vast majority of such cases were observed in Transcarpathia at the meteorological station Play, which is associated with a higher frequency of favorable conditions for its formation. Given the results of the study, we can say that in 1991-2000 the largest number of cases of frost deposits of the category of DP in Ukraine was observed in January, February and December, with January accounting for the vast majority of cases. During January, frost deposits of the DP category were quite widely represented on the territory of Ukraine in 9 oblasts. During February and March, they were observed only in mountainous areas – in Transcarpathia and in the Autonomous Republic of Crimea. In April, October and November, such deposits were observed only in Transcarpathia at the Play meteorological station. In December, their range expanded and they were observed not only in the mountains, but also in the north, northeast and east of the country in 5 regions. The largest number of such cases during 1991-2000 was observed in Transcarpathia (Play) and in the Autonomous Republic of Crimea (Ai-Petri). In the period 2001-2010, the main number of cases of frost deposition of the DP (dangerous phenomena) category falls on the months of the cold period of the year, especially January and December. In contrast to the period 1991-2000, the number of cases increased in March and November, and the number of such deposits increased slightly in April. The vast majority of cases of frost deposits of the DP (dangerous phenomena) category during 2001-2010, as well as in the previous decade, were observed in Transcarpathia at the Play weather station. During 2011-2020, there was an increase in the number of cases of DP frost deposits in January and February compared to 2001-2010 and a slight decrease in these deposits in November and December. Also for this period, a greater localization of such sediments in Transcarpathia was established in all the studied months compared to the previous study periods, when especially in January and December such sediments were quite widespread in Ukraine.


2016 ◽  
Vol 11 (2) ◽  
pp. 24-30
Author(s):  
Emilio Prado da Fonseca ◽  
Suelen Garcia Oliveira da Fonseca

In Brazil, there is a regional variation in and mortality by cancer of the mouth. Differences in the distribution of the rate of this type of mortality are attributed to the consumption of cigarettes and alcohol, socioeconomic conditions, diet or genetic characteristics. Aim: To compare the spatial distribution of deaths by cancer of the mouth between the macro-regions of health of the state of Minas Gerais between 2006 and 2013 and identify the formation of agglomerates of deaths by cancer of the mouth. Methodology: This is an ecological study that used the data made available by the System of Information on Mortality (SIM) and based on Chapter 2 of ICD-10. The geographic pattern was built through thematic maps of the distributions of rates mortality, as the macro-regions of health and year. Results: In the period studied 2.263 deaths occurred for cancer of the mouth in Minas Gerais, being, 1751(77,38%) men and 512 (22.62%) women. There was a trend of growth in the rate of mortality from cancer of the mouth in Minas Gerais, mainly for the male gender. You can say that deaths occurred for cancer of the mouth in all macro-regions of the state and that the geographic distribution of these deaths occurred in a heterogeneous way. Conclusion: The highest rate of deaths in men suggest the need of developing programs directed to this population in Minas Gerais Brazilian state.


2013 ◽  
Vol 38 (7) ◽  
pp. 1286-1294 ◽  
Author(s):  
Zong-Xin LI ◽  
Yuan-Quan CHEN ◽  
Qing-Cheng WANG ◽  
Kai-Chang LIU ◽  
Wang-Sheng GAO ◽  
...  

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