Formation Factors and Criteria of the Allocation of High-Altitude Landscape Stage in Chornogora (Ukrainian Carpathians)

Melnyk, Anatoliy; Karabiniuk, Mykola

doi:10.30970/gpc.2018.08.2012

Cited by 6 publications

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“…There are comprehensive works on tectonics and stratigraphy for the territory of the entire Ukrainian Carpathians such as Bondarchuk (1959), V. Hlushko (1968), I. Gofstein (1995 and others. In the 21st century, many articles have been published on the geomorphology of the Svydovets massif (Krawczuk 2008, Kłapyta et al 2020 and Chornohora (Melnyk 2018). O.…”

Section: Fig 1 Map Of the Chorna Tisza Catchment Area With Boundaries...mentioning

confidence: 99%

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Physical Geography and Geomorphology publishes original research papers, review articles and short contributions in all areas of physical geography and geomorphology, namely: theoretical and methodological research in physical geography and geomorphology, landscape studies, geoecology, palaeoecology, Quaternary palaeogeography, soil science, meteorology, climatology, hydrology, structural, dynamic, ecological and palaeogeomorphology, application of GIS in natural geographic research, and geographical education.The journal is published since 1970. Published bi-monthly. Articles are published in Ukrainian and English.

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Section: Fig 1 Map Of the Chorna Tisza Catchment Area With Boundaries...mentioning

confidence: 99%

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“…Gofstein (1995) and others. In the 21st century, many articles have been published on the geomorphology of the Svydovets massif (Krawczuk 2008, Kłapyta et al 2020 and Chornohora (Melnyk 2018). O. Obodowski (2005) and Yu.…”

Section: Fig 1 Map Of the Chorna Tisza Catchment Area With Boundaries...mentioning

confidence: 99%

Features of the structure of selected segments of the Chorna Tisza river

Derii

2022

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The paper presents an analysis of the structure of the Chorna Tisza river based on the fieldwork done in the summer of 2020. In this paper, the results of the riverbed classification by Krzemień (2012) are presented. During the typological classification of the river, 34 segments were identified, which were grouped into 7 typological segments according to processes prevailing in each. The classification takes a variety of factors into account, including: the difference in elevation per kilometer of channel run, the presence of channel forms, the area of the forms, the height of the banks, the bank depth of channel incision, the lithological and tectonic factors as well as factors indicating anthropogenic influence on the channel. A total of 16 factors were identified. It was revealed that Chorna Tisza’s riverbed has a tendency to bed erosion mostly in all typological plots, which may be a problem for residents in the future. An attempt was made to predict the evolution of the riverbed based on the collected data and assessment of the human impact on the structure of the riverbed.

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“…Чорногора є найвищим гірським ландшафтом Українських Карпат та характеризується своєрідною історією розвитку і високим ландшафтним різноманіттям (Miller, 1963(Miller, , 1974Melnyk, 1999Melnyk, , 2009Melnyk et al, 2018;Melnyk, Karabiniuk, 2018c, 2018dKarabiniuk, , 2020. У розвитку природних територіальних комплексів (ПТК) та ландшафтної структури масиву важливу роль відіграють ерозійні процеси, які тісно пов'язані із розвитком сучасної річкової системи та гідрологічним режимом річок.…”

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Modern dynamics of water levels and their flood rises in the upper reaches of the Prut River within the Chornohora Landscape (Ukrainian Carpathian)

Карабінюк¹,

Гнатяк²,

Буряник³

et al. 2021

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This article presents the results of the analysis of modern water levels of the upper reaches of the largest river named Prut in the mountain landscape of Chornohora for the period from 2010 to 2019, based on data from own long-term hydro-meteorological observations on the basis of Landscape Monitoring Laboratory of Ivan Franko National University. The studied river is characterized by a dense river network, a peculiar hydrological regime and periodic formation of heavy floods, as well as the presence in its basin of valuable landscape complexes and environmental facilities, high landscape diversity and recreational and tourist potential, which determines the relevance of this study. As a result of the study, the peculiarities of the formation and modern features of the hydro network of the Prut river basin were established, its heterogeneity in the mid-mountain and high-mountain landscape tiers was characterized. It is established that during the period 2010-2019 in the upper reaches of the Prut River there was an increase in river water levels, as well as identified the main factors and their impact on current changes in the hydrological regime of the river. The annual changes in the water level in the upper reaches of the Prut River for the period 2010-2019 were also analyzed and it was found that its mountainous nature causes high dynamics of river water levels at different times of the year and in certain months. It was important to identify the relationships between their indicators and the characteristics of the annual distribution of precipitation and snowmelt during studying the annual cycles of water level fluctuations. Particular attention is paid to the study of the formation and spread of floods as the most dangerous hydrological phenomenon of the upper reaches of the Prut River, characterized by a sharp rise in water levels, high erosion capacity, etc. The study found that more than 75 % of floods occur during the spring snowmelt in April and May where the average daily river water levels usually do not exceed 60-70 cm. The analysis of flood rises in terms of years and months shows that the most severe catastrophic floods are formed in November-December due to heavy rains, which cause the formation of powerful destructive water flows and catastrophic growth of river water levels over 90-100 cm. The total annual number of flood rises in the Prut River was also analyzed according to certain categories of indicators (over 60 cm, 70 cm, etc.) and it was found that the total number of floods in the upper reaches of the river is increasing.

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Formation Factors and Criteria of the Allocation of High-Altitude Landscape Stage in Chornogora (Ukrainian Carpathians)

Cited by 6 publications

References 0 publications

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Features of the structure of selected segments of the Chorna Tisza river

Modern dynamics of water levels and their flood rises in the upper reaches of the Prut River within the Chornohora Landscape (Ukrainian Carpathian)

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