Physical Geography and Geomorphology最新文献

{"title":"Landscape differentiation of negative physical-geographical processes in the subalpine and alpine highlands of Сhornogora (“Sheshul-Petros” section)","authors":"M. Karabiniuk","doi":"10.17721/phgg.2019.3.01","DOIUrl":"https://doi.org/10.17721/phgg.2019.3.01","url":null,"abstract":"","PeriodicalId":191415,"journal":{"name":"Physical Geography and Geomorphology","volume":"33 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"117083565","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Duration of the growth phase in cases of ice deposits of category SHP (spontaneous) in the territory of Ukraine in the months of the cold period of the year during 1991–2016","authors":"S. Pyasetska","doi":"10.17721/phgg.2019.4-6.05","DOIUrl":"https://doi.org/10.17721/phgg.2019.4-6.05","url":null,"abstract":"The data on the duration of the growth phase of cases of ice storms of the category of SHР in the territory of Ukraine for certain periods of time during 1991–2016 in the month of the cold period of the year and the separate months of the transitional seasons are considered. It has been established that the duration of the growth phase varies from a few hours to several dozen and sometimes hundreds of hours in a row. It was found that, for the most part, slight duration of the growth phase of icing of the category of SHP is predominant. They are usually calculated several dozens of hours, but there are longer ones. The most prolonged were the growth phases in the cases of ice deposits in the category of SHP in the winter months. You can make a number of conclusions from the conducted research, such as: – The duration of the growth phase of ice-oily deposits in the category of SHP is within a fairly wide time range from several hours to tens or hundreds of hours, depending on the current conditions. – It has been established that for the most part, the duration of the growth phase of ice deposits is insignificant and lasts from several hours to several dozens of hours, regardless of the place where the sediment was formed. - Most often, longer phases of growth are observed in the months of the winter season, especially in January and December, as well as in November. This refers to the 1991–2000 and 2001–2010 periods. - The most prolonged phases of the accumulation of ice deposits of the CSF category, which exceeded 48 hours in a row, were observed during 1991-2000 in February 1995 at MS Play, November 1991 and 2000 in Lyubashivka, 1999 in Mariupol, November 2000, in Razdelna and Nova Ushytsia, December 1992 in Lyubashitsa, December 1997 in Pomechna, Kryvyi Rih and Loshkarovka. During 2001–2010, the longest phases of the increase in ice deposits of the CSF category were observed in January and December 2007 at MS Play, December 2007 in Debaltseve, 2008 in Ovruch, Vinnytsia. During 2011-2016, cases of ice deposition with such prolonged phases of an increase in ice of the SНР category were observed in Poltava in January 2013. – For cases where the duration of the growth phase of ice deposits was negligible, it would have a long duration of the preservation and destruction phase. Because due to the considerable duration of this phase, the danger of emergency situations in the ice-and-frost deposits depending on the sectors of the economy will increase.","PeriodicalId":191415,"journal":{"name":"Physical Geography and Geomorphology","volume":"351 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"123229497","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Perspective geotourist products in protected areas of the Transcarpathia region","authors":"L. Dubis, N. Habchak","doi":"10.17721/phgg.2019.1.04","DOIUrl":"https://doi.org/10.17721/phgg.2019.1.04","url":null,"abstract":"","PeriodicalId":191415,"journal":{"name":"Physical Geography and Geomorphology","volume":"23 2","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"131923364","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Retrospective-geographical analysis of the formation and change of the state of ponds of the Volyn Region in the XIX-XXI centuries","authors":"I. Grytsiuk, E. Ivanov, I. Kovalchuk","doi":"10.17721/phgg.2019.4-6.01","DOIUrl":"https://doi.org/10.17721/phgg.2019.4-6.01","url":null,"abstract":"The main retrospective-geographical (historical) stages of ponds formation in the Volyn Region are considered – initial, early (manufactory), industrial and modern (agrarian, post-industrial). In order to analyse conditions and functioning of the region’s pond farms we used topographic maps for four historical periods: Commonwealth of Poland historical atlas (scale 1 : 300,000, early ХІХ century), Russian Empire (scale 1 : 126,000, 1875), Polish (scale 1 : 100,000, 1924-1933) and Soviet maps (scale 1 : 100,000, 1977-1992). They reflect the trend of changes in the parameters and functioning of the existing ponds in the Volyn Region over the last 220 years. Landscape-hydrological systems were selected for geospatial analysis of location features of the ponds and water mills within the Volyn Region. Overall, 19 individual landscape-hydrological systems were established. An exponential increase in the number of ponds in early and industrial stages was identified, considering some decreases in particular historical periods. The number of ponds in the region varied from 76 (in the 1970s) to 625 units (1970-80s). A clear, almost linear, increase in ponds total area was observed. During the studied historical period, the area of ponds increased from 1,553.7 to 4,242.4 ha. The highest concentration of pond farms is specific to the landscape-hydrological systems of the Volyn Highland, especially to the Stir-III sub-basins (29.9 % of the total count in the region), Luga-III and Goryn-III. At the same time, a gradual decrease in the average area of a pond – from 20.44 (in the 70s of the XIX century) to 6.28 ha (70-80 years of the XX century) was shown. The considerable number of ponds in the rural areas of the Volyn Region is an important factor in the creation of new work places, recreation areas, diversification of agricultural products and feed base.","PeriodicalId":191415,"journal":{"name":"Physical Geography and Geomorphology","volume":"82 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"134278410","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"The research of deflation processes on the Ukrainian Roztochya using the semi-stationary methods","authors":"V. Brusak","doi":"10.17721/phgg.2019.2.04","DOIUrl":"https://doi.org/10.17721/phgg.2019.2.04","url":null,"abstract":"","PeriodicalId":191415,"journal":{"name":"Physical Geography and Geomorphology","volume":"50 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"124157318","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Terrain morphometric characteristics as indicators of Ukrainian Roztochia springs localization","authors":"Bogdan Ivanovych","doi":"10.17721/phgg.2019.2.02","DOIUrl":"https://doi.org/10.17721/phgg.2019.2.02","url":null,"abstract":"The opening of aquifers with erosional downcut is one of the main factors in springs occurrence, therefore, morphometric analysis of the territory where springs are localized is necessary to understand conditions of their formation. Maps of vertical and horizontal relief dissection and steepness of land surface were created using GIS and the data about terrain morphometric characteristics in the places of springs localization were obtained, as well as for the territory of the Ukrainian Roztochia landscapes. More than 75% of the Ukrainian Roztochia springs, confined (maximum steepness of slopes within a radius of 250 m) to steep and very steep slopes and high vertical dissection of more than 60 m/km, are attributed to 38.32% of spring localization spots. The link between springs localization and terrain morphometric indicators has been confirmed. It involves the similarities between landscape areas and springs localization spots morphometrics in general and on the each landscape particularly, direct matching between terrain morphometric parameters and springs quantity in landscapes, certain springs associations with steep and very steep slopes and places with high values of vertical dissection. Moreover, the abovementioned shows inequivalence of various morphometric characteristics as indicators of springs distribution. In general, terrain morphometrics and springs localization correlated unevenly. Morphometric characteristics of the relief, as the springs localization indicators best illustrate the situation in the Dubrovytskyi landscape (it has the higher values of dissection deepness, density and the steepness of land surface), also it explains non-availability of springs in the Domazhyrskyi landscape. Morphometric values are significantly lower than in other landscapes, what is low favourable for springs formation. This evidences that the particularly well-defined influence of terrain morphometrics on springs distribution occurs in conditions of more homogeneous strongly or slightly dissected nature of the terrain.","PeriodicalId":191415,"journal":{"name":"Physical Geography and Geomorphology","volume":"1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"114897867","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Features of anthropogenic landforms of the mining complex in Polonsky district, Khmelnitskyi Region","authors":"Y. Filonenko, Mykhailo Snitsarenko","doi":"10.17721/phgg.2019.1.01","DOIUrl":"https://doi.org/10.17721/phgg.2019.1.01","url":null,"abstract":"","PeriodicalId":191415,"journal":{"name":"Physical Geography and Geomorphology","volume":"11 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"126154836","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Analysis of the seasonal variability of the hydrochemical composition of the waters of the Kosivska River for the period 2017-2018","authors":"V. Leta, O. Pylypovych","doi":"10.17721/phgg.2019.3.03","DOIUrl":"https://doi.org/10.17721/phgg.2019.3.03","url":null,"abstract":"","PeriodicalId":191415,"journal":{"name":"Physical Geography and Geomorphology","volume":"1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"129779366","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Statistical analysis of aridity in Ukraine","authors":"V. Zatula, N. Zatula","doi":"10.17721/phgg.2019.1.03","DOIUrl":"https://doi.org/10.17721/phgg.2019.1.03","url":null,"abstract":"","PeriodicalId":191415,"journal":{"name":"Physical Geography and Geomorphology","volume":"1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"129009717","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Monitoring for the areas of illegal extraction of amber using remote sensing (on the territory of Zhytomyr Polissya)","authors":"V. Atamanchuk","doi":"10.17721/phgg.2019.1.02","DOIUrl":"https://doi.org/10.17721/phgg.2019.1.02","url":null,"abstract":"","PeriodicalId":191415,"journal":{"name":"Physical Geography and Geomorphology","volume":"71 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"1900-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"130755973","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}