Floodsite Project Report D22.3
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XXIX Danube Conference
XXIX Danube Conference XXIX Conference of the Danubian Countries on Hydrological Forecasting and Hydrological Bases of Water Management September 6–8, 2021 ISBN 978-80-7653-017-1 Brno Czech Hydrometeorological Institute Czech National Committee for UNESCO Intergovernmental Hydrological Programme Danube XXIX Conference of the Danubian Countries on Hydrological Forecasting and Hydrological Bases of Water Management Conference proceedings Extended abstracts September 6–8, 2021 Brno, Czech Republic Prague 2021 Organized by Under the auspices of Czech National Committee for UNESCO Intergovernmental Hydrological Programme Danube Co-organizers Czech National Committee for Hydrology CREA Hydro & Energy Povodí Moravy Czech Scientific and Technical Water Management Company Technical University of Vienna University of Ljubljana, Faculty of Civil and Geodetic Engineering © Czech Hydrometeorological Institute ISBN 978-80-7653-020-1 2 XXIX Conference of the Danubian Countries, September 6–8, 2021, Brno, the Czech Republic Obsah Introductory word .................................................................................................................... 8 TOPIC 1 DATA: TRADITIONAL & EMERGING, MEASUREMENT, MANAGEMENT & ANALYSIS ............................................................................................ 9 Estimation of design discharges in terms of seasonality and length of time series .......... 10 Veronika Bačová MITKOVÁ Modelling snow water equivalent storage and snowmelt across Europe with a simple degree-day model ........................................................................................... -
Trails of Carpathians
OLEG YAMALOV Trails of Carpathians Hiking and Trekking in the Ukrainian Karpaty 80 Trails In memory of Oleg Yamalov 1951 – 2017 Completion and Refinement by: Svetlana Yamalova Folio Publishers Kharkiv, Ukraine 2019 CONTENTS Preface 6 Acknowledgments 10 How to Use this Guidebook 12 Marks and Abbreviations 14 Carpathian Mountains 15 Highest Summits of Carpathians by Countries of their Location 20 HIKING AND TREKKING ROUTES E1-E24 Eastern (Central) Cascade of the Ukrainian Carpathians 21 E1 Latorytsky (Nyzhni Vorota) Pass – Serednyoveretsky Pass – Torunsky (Vyshkivsky) Pass 29 E2 Train station Beskyd – Yavirnyk Mountain – Train station Lavochne 33 Train station Volovets – Pliy Mountain – Velyky Verh Mountain E3 – Shypit waterfall – Village Podobovets 39 Urban-type settlement Volovets – Pliy Mountain – Velyky Verh E4 Mountain – Stiy Mountain – Train station “1663 km” 45 E5 Village Podobovets – Shypit waterfall – Velyky Verh Mountain – Stiy Mountain – Train station Vovchy 51 Train station Vovchy – Zeneva Mountain – Stiy Mountain – Velyky E6 Verh Mountain – Urban-type settlement Volovets 57 Train station “1663 km” - Stiy Mountain – Velyky Verh Mountain – E7 Temnatyk Mountain – Urban-type settlement Volovets 63 E8 Village Bereznyky – Stiy Mountain – Train station “1663 km” 69 Village Nyzhny Bystry – Kuk Mountain – Pryslip Pass – Velyky Verh E9 Mountain – Stiy Mountain – Train station “1663 km“ 77 Torunsky Pass – Vyshkivsky Gorgan Mountain – Popadya E10 Mountain – Grofa Mountain – Village Osmoloda 85 E11 Torunsky Pass - Vyshkivsky Gorgan Mountain -
Patterns and Forecast of Long-Term Cyclical Fluctuations of the Water
Environmental Research, Engineering and Management 2017/73/1 33 EREM 73/1 Patterns and Forecast of Long-term Cyclical Fluctuations of the Water Journal of Environmental Research, Runoff of Ukrainian Carpathians Rivers Engineering and Management Vol. 73 / No. 1 / 2017 Received 2017/06 Accepted after revision 2017/07 pp. 33-47 DOI 10.5755/j01.erem.73.1.15799 © Kaunas University of Technology http://dx.doi.org/10.5755/j01.erem.73.1.15799 Patterns and Forecast of Long-term Cyclical Fluctuations of the Water Runoff of Ukrainian Carpathians Rivers Oleksandr Obodovskyi, Olga Lukianets Taras Shevchenko National University of Kyiv Glushkov prospekt, 2A, Kyiv, SMP680 Ukraine Corresponding author: [email protected] Oleksandr Obodovskyi , Taras Shevchenko National University of Kyiv Glushkov prospekt, 2A, Kyiv, SMP680 Ukraine Knowledge of the cyclicity features in the fluctuations of river runoff, duration and nature of the low-water and high-water period interchange in one or other river basins, and especially their prediction, provides invaluable as- sistance in the planning and sound management of water resources, improving the operational efficiency of hydro- power, reclamation and other water facilities. Currently, the interest in the study of long-term cyclical fluctuations in river runoff, as well as patterns of fluctuations of its underlying factor, has highly increased due to their use in long-term forecasts. Time series of annual water runoff for basins of Tisza, Dniester and Prut rivers were estimated with the use of mathematical tools, methodological framework of which is based on a statistical means of summarizing, systemi- sation of the input data, evaluation methods of time random sets of runoff characteristics, methods of analysis of the time-series variability and manifestation of their structure. -
TABLE of CONTENTS Estimation of the Long-Term Cyclical Fluctuations Of
TABLE OF CONTENTS Estimation of the long-term cyclical fluctuations of snow-rain floods in the Danube basin within Ukraine Tetiana ZABOLOTNIA, Liudmyla GORBACHOVA, Borys KHRYSTIUK 3 Multi-annual variability of global solar radiation in the agricultural area of Lower Silesia (SW Poland) and its relationship with the North Atlantic Oscillation Krystyna BRYŚ, Tadeusz BRYŚ 13 Sensitivities of the Tiedtke and Kain-Fritsch Convection Schemes for RegCM4.5 over West Africa Mojisola Oluwayemisi ADENIYI 27 Water vapor induced airborne rotational features Roman MARKS 39 Learning to cope with water variability through participatory monitoring: the case study of the mountainous region, Nepal Santosh REGMI, Jagat K. BHUSAL, Praju GURUNG, Zed ZULKAFLI, Timothy KARPOUZOGLOU, Boris Ochoa TOCACHI, Wouter BUYTAERT, Feng MAO 49 Long-term seasonal characterization and evolution of extreme drought and flooding variability in northwest Algeria Kouidri SOFIANE, Megnounif ABDESSELAM, Ghenim Abderrahmane NEKKACHE 63 Homogeneous regionalization via L-moments for Mumbai City, India Amit Sharad PARCHURE, Shirish Kumar GEDAM 73 After COP24 Conference in Katowice – the role of the Institute of Meteorology and Water Management – National Research Institute in connection of hydrological and meteorological measurements and observations with climate change adaptation actions Marta BARSZCZEWSKA, Ksawery SKĄPSKI 85 Vol. 7 Issue 2 June 2019 Estimation of the long-term cyclical fluctuations of snow-rain floods in the Danube basin within Ukraine Tetiana Zabolotnia, Liudmyla Gorbachova, Borys Khrystiuk Ukrainian Hydrometeorological Institute, Prospekt Nauki 37, 03028 Kyiv, Ukraine, e-mail: [email protected], [email protected], [email protected] Abstract. Floods are a periodic natural phenomenon, often accompanied by negative consequences for the local population and the economy as a whole. -
Geomorphologic Effects of Human Impact Across the Svydovets Massif in the Eastern Carpathians in Ukraine
PL ISSN 0081-6434 studia geomorphologica carpatho-balcanica vol. liii – liV, 2019 – 2020 : 85 – 111 1 1 1 3 PIOTR KŁapYTA , KaZimier2 Z KrZemieŃ , elŻBIETA GORCZYca , PAWeŁ KrĄŻ , lidia dubis (KraKÓW, lViV) GEOMORPHOLOGIC EFFECTS OF HUMAN IMPACT ACROSS THE SVYDOVETS MASSIF IN THE EASTERN CARPATHIANS IN UKRAINE Abstract - : contemporary changes in the natural environment in many mountain areas, espe cially those occurring above the upper tree line, are related to tourism. the svydovets massif,- located in the eastern carpathians in ukraine, is a good example of an area that is currently experiencing intense degradation. the highest, ne part of this area is crisscrossed with nu merous paths, tourist routes, and ski trails. the strong human impact the area experiences is occurring simultaneously with the activity of natural geomorphologic processes. the processes occur with the greatest intensity above the upper tree line.th the development of the discussed- area has been occurring gradually since the early 20 century. it started when the region belonged to austria-hungary, then czechoslovakia, and subsequently the ussr. now that it be longs to independent ukraine the level of tourism-related development has sharply increased. comparing it to other mountain areas, such as the tatras, the alps, or the monts dore massif in France, the svydovets massif is being reshaped much more rapidly due to the damage caused byKeywords human impact. : human impact, tourism-related deterioration of mountains, high mountains, svydovets, eastern carpathians, ukraine INTRODUCTION - man plays a huge role in the reshaping of the geographic environment and hu man activity is especially noticeable in the mountains. -
Annual Maximum Discharge Qmax Danube River
Flood regime of rivers in the Danube River basin App. I.3 APPENDIX I.3 Annual Maximum Discharge Qmax Danube River 1 Flood regime of rivers in the Danube River basin App. I.3 River: Danube Station: Berg Area: 4.047 103 km2 GE Qmax Basic statistical characteristics Qmax qmax min max cs cv Med. trend m3/s l/s/km2 m3/s m3/s m3/s 1876-2005 205 50.6 53 445 0.69 0.43 196 0.2310 Period Qmax qmax min max cs cv Period Qmax St.dev qmax cs cv 1871-1880 1886-1915 1881-1890 1901-1930 1891-1900 1916-1945 195 85 48.2 0.56 0.43 1901-1910 1931-1960 205 89 50.6 0.35 0.43 1911-1920 1946-1975 195 83 48.2 0.64 0.43 1921-1930 1961-1990 213 98 52.7 0.75 0.46 1931-1940 189 46.8 105 367 1.21 0.42 1976-2005 219 95 54.2 0.74 0.43 1941-1950 204 50.5 53 345 -0.10 0.53 1951-1960 221 54.6 117 376 0.68 0.38 ] 250 1 - 1961-1970 194 47.8 120 351 1.28 0.37 s 3 200 1971-1980 194 47.9 77 412 0.95 0.52 150 1981-1990 252 62.2 92 445 0.23 0.45 [m Q 100 1991-2000 185 45.6 120 354 1.47 0.40 1886- 1901- 1916- 1931- 1946- 1961- 1976- 2001-2006 202 49.8 116 281 -0.01 0.32 1915 1930 1945 1960 1975 1990 2005 Long term 30-year discharge. -
Human Potential of the Western Ukrainian Borderland
Journal of Geography, Politics and Society 2017, 7(2), 17–23 DOI 10.4467/24512249JG.17.011.6627 HUMAN POTENTIAL OF THE WESTERN UKRAINIAN BORDERLAND Iryna Hudzelyak (1), Iryna Vanda (2) (1) Chair of Economic and Social Geography, Faculty of Geography, Ivan Franko National University of Lviv, Doroshenka 41, 79000 Lviv, Ukraine, e-mail: [email protected] (corresponding author) (2) Chair of Economic and Social Geography, Faculty of Geography, Ivan Franko National University of Lviv, Doroshenka 41, 79000 Lviv, Ukraine, e-mail: [email protected] Citation Hudzelyak I., Vanda I., 2017, Human potential of the Western Ukrainian borderland, Journal of Geography, Politics and Society, 7(2), 17–23. Abstract This article contains the analysis made with the help of generalized quantative parameters, which shows the tendencies of hu- man potential formation of the Western Ukrainian borderland during 2001–2016. The changes of number of urban and rural population in eighteen borderland rayons in Volyn, Lviv and Zakarpattia oblasts are evaluated. The tendencies of urbanization processes and resettlement of rural population are described. Spatial differences of age structure of urban and rural population are characterized. Key words Western Ukrainian borderland, human potential, population, depopulation, aging of population. 1. Introduction during the period of closed border had more so- cial influence from the West, which formed specific Ukraine has been going through the process of model of demographic behavior and reflected in dif- depopulation for some time; it was caused with ferent features of the human potential. significant reduction in fertility and essential mi- The category of human potential was developed gration losses of reproductive cohorts that lasted in economic science and conceptually was related almost a century. -
Mapping the Mean Annual River Runoff in the Ukrainian Carpathian Region
22 Environmental Research, Engineering and Management 2020/76/2 Mapping the Mean Annual River Runoff in the EREM 76/2 Ukrainian Carpathian Region Journal of Environmental Research, Engineering and Management Vol. 76 / No. 2 / 2020 Received 2018/06 Accepted after revision 2020/06 pp. 22–33 DOI 10.5755/j01.erem.76.2.20916 http://dx.doi.org/10.5755/j01.erem.76.2.20916 Mapping the Mean Annual River Runoff in the Ukrainian Carpathian Region Oleksandr Obodovskyi, Olga Lukianets*, Oksana Konovalenko, Valeriy Mykhaylenko Taras Shevchenko National University of Kyiv, 2-A, Glushkov Prospekt, Kyiv, SMP680, Ukraine *Corresponding author: [email protected] The paper presents the spatial distribution of the mean annual river runoff in the Ukrainian Carpathians in the form of a map. The methodological approaches concerning the river runoff mapping and the technological stages of map creation by applying the geographic information system (GIS) analytical functions are considered. The accuracy assessment of the calculation of the mean annual river runoff water based on the data from the hydrometric stations for the whole observation period was performed. The mapping reliability of the mean annual runoff and their territorial variability over the main basins in the Ukrainian Carpathians are analysed. Keywords: rivers of the Ukrainian Carpathians, analytical functions of GIS, spatial distribution, mean annual river runoff, water resources. Introduction Maps of runoff give not only an idea about the space- map of the mean annual river runoff in the Ukrainian time variability of river runoff distribution over the Carpathians (the basins of Tisza, Prut and Dniester riv- studied area but also the quantitative information on ers), its generalisation for designing the stream power a spatial variability, seasonality and regularity of river hydro-energy potential of rivers, even those unstudied. -
Transcarpathian Art Institute
ЕРДЕЛІВСЬКІ ЧИТАННЯ, 2013 р. MINISTRY OF EDUCATION AND SCIENCE OF UKRAINE TRANSCARPATHIAN ART INSTITUTE №4 The NEWSLETTER of Transcarpathian Institute of Arts Bulletin of scientific and research works of International scientific‐practical conference Uzhhorod, the 13‐14th of May, 2013 Edition Hrazhda Uzhhorod, 2013 2 The Herald of Transcarpathian Art Institute. № 4 LBC 85.103(4UKR) UDC 7.03(477) N 34 The fourth issue of “The Herald of Transcarpathian Art Institute” contains the materials of international scientific and practical conference “Erdelyi’s Lec‐ tures”, held in Uzhhorod on the 14th ‐16th of May, 2013. The scientific analysis of theoretical and practical researches in the sphere of Fine and Decorative‐ Applied Arts, design and art education in Ukraine was given and the problem of interinfluence of the cultures of the European people and the introduction of art education in artistic establishments were touched upon. It is printed according to the decree of Scientific council of Transcarpathian Art Institute since the 25th of January, 2013, protocol №5 Editorial board: Ivan Nebesnyk, Phd of pedagogical sciences, professor, rector of TAI; Mykola Yakovlev, PhD of technical sciences (technical aesthetics), professor, main scientific secretary of NAAU; Mykola Mushynka, academician of NAAU, PhD of philological sciences, professor; Volodymyr Vasylyev, PhD of culturology, professor of Chuvask state university named after I.M. Ulyanov; Orest Holubets, PhD of art criticism, professor; Halyna Stelmashchuk, PhD of art criticism, professor; Mykhaylo Tyvodar, PhD of historical sciences, professor; Serhiy Fedaka, PhD of historical sciences, professor; Ivan Vovkanych, PhD of historical sciences, professor; Roman Yaciv, candidate of art criticism, associate professor, vice rector of LNAA; Odarka Dolhosh, candidate of art criticism; Attila Kopryva, candidate of art criticism, associate professor; Mykhaylo Pryimych, candidate of art criticism, associate professor; Nataliya Rebryk, candidate of philological sciences, vice rector of TAI. -
Ministry of Education and Science of Ukraine Transcarpahtian State University Institute for Transfrontier Cooperation
MINISTRY OF EDUCATION AND SCIENCE OF UKRAINE TRANSCARPAHTIAN STATE UNIVERSITY INSTITUTE FOR TRANSFRONTIER COOPERATION METHODOLOGY AND TOOLS FOR SOCIOLOGICAL ANALYSIS OF TRANSBORDER COOPERATION proceedings of international scientifi c – practical conference (Uzhgorod, Ukraine, January 24-25, 2013) Special issue Of collection of scientifi c papers GEOPOLITICS OF UKRAINE: HISTORY AND MODERN TIMES Uzhgorod • 2013 УДК 327 (477) ББК 66.011.3 (11 Англ) Г 36 The collection includes reports, speeches and scientifi c papers prepared following the international scientifi c – practical conference within “Methodology and tools for sociological analysis of transborder cooperation”, held by the project “Borders through the eyes of people” framework in Uzhgorod, Ukraine on January 24-25, 2013 within implementation of ENPI Cross border Cooperation Program the Hungary – Slovakia – Romania – Ukraine 2007 – 2013. The publication is issued with fi nancial support of the European Union. Editorial board: Ustych S.I. — PhD, Associate Professor (Editor in Chief) Artyomov I.V. — PhD, Professor (Deputy Editor in Chief) Vovkanych I.I. — PhD, Professor Korol I.F. — PhD, Professor Majboroda I.M. — PhD, Professor Pakhomov Y.M. — PhD, Professor, member of Academy of Sciences of Ukraine Rudenko O.M. — PhD, Associate Professor Editorial board of the collection: Vashchuk F.H. — PhD, Professor (Board Head) Budkin V.S. — PhD, Professor Luhovyj V.I. — PhD, Professor, Vice-President of the NAPN Ukraine Polyuzhyn M.M. — PhD, Professor Popovych V.M. — PhD, Professor Reviewers Olenski -
Spatial-Temporal Evaluation of Maximal Quantity of Precipitations for Hydrological Calculations and Forecasts
SPATIAL-TEMPORAL EVALUATION OF MAXIMAL QUANTITY OF PRECIPITATIONS FOR HYDROLOGICAL CALCULATIONS AND FORECASTS Nataliia Pryimachenko, Mykhaylo Sosedko Ukraіnіan Hydrometeorologіcal Research Institute Pr. Nauky 37, Kyіv 03028 Ukraіne [email protected]; [email protected] Abstract The score of the maximal precipitations only then have a value if it is known their repeatability or probability of approach. Such estimations can be received through statistical generalization of homogeneous data in time and space. Nevertheless in many publications and directories it is not attending appropriate attention to data which are processed. Therefore value of similar generalizations is not enough high, as data are lost on intensity of precipitations. Keywords: maximum quantities, precipitations, mountain part, homogeneous districts. 1 HETEROGENEITY OF THE MAXIMAL DAILY QUANTITIES OF PRECIPITATIONS Widespread enough characteristic of precipitations is the maximal daily quantity. This value is estimated by summation of quantities of precipitations for terms of observation during a meteorological day. Therefore separate parts of the same rain can get in P m contiguous day. Thus daily quantities of precipitations d mainly will be smaller, than maximal for 24 hours, which cover the interval of their fall which has been not attached P m to constant initial time reckoning - 24 . A ratio between these values of the maximal precipitations is defined by an inequality (Sosedko, 1980): m m m 5,0 P24 Pd P24 . (1) In table 1 are resulted comparisons of daily and 24-hours maximum quantities of precipitations for a flood in November, 1998 in the Tisza river basin. So, for the values of the maximal daily quantities of precipitations is inhere the uncertainty caused by the way of their receiving. -
Search List H
© Skoumal Krisztián V.2021.03.13 Sorszam Kod Nev Szul.* Telepules* Apa Anya Nr. Code Name Born* Town* Father Mother 1. RCE3810026340892012004 HAACK Franz 1856 Wien (A) HAACK Mathias DRAHORAT Aloysia 2. IRCK400300102000654060 HAAS Antal Andras 1941 Temesvar Timisoara (RO) 3. ZSE4000300185901024004 HAAS Eszter <1887 Temesvar Timisoara (RO) HAAS M. [Moshe] 4. ZSE4000300341896485001 HAAS Jakab <1880 Arad (RO) HAAS Benjamin 5. IRCK400300102000653049 HAAS Janos 1897 Temesvar Timisoara (RO) 6. RCE3810026340901018002 HAAS Jozsef 1876 Gyertyamos Carpinis (RO) HAAS Lajos AUGUSTIN Maria 7. ZSE4000300341894478082 HAAS Jozsef 1866 Jaszbereny (H) HAAS David SPITZER Hanni 8. ZSE4000310000889017022 HAAS Markus 1866 Kurtics Curtici (RO) HAAS Bernat N. Rozalia 9. ZSE4000300185897019079 HAAS Vilmos [Tzvi] <1881 10. ZSE4000310000890024035 HAASZ Albert 1864 Kurtics Curtici (RO) HAASZ Bernat KLOPNAR Rozalia 11. CRE3669775101919029067 HAASZ Anna 1902 Szederkeny (H) HAASZ Oszvald RITTER Emilia 12. IRCK400300102000653060 HAASZ Arpad 1901 Temesvar Timisoara (RO) 13. IRCK400300102000654009 HAASZ Edit Maria 1920 Temesvar Timisoara (RO) 14. IRCK400300102000654018 HAASZ Egon 1922 Temesvar Timisoara (RO) 15. IRCK400300102000654013 HAASZ Herman 1921 Temesvar Timisoara (RO) 16. CRE4000310501910008024 HAASZ Janos 1853 Arad Arad-Sega (RO) HAASZ Karoly VOGEL Borbala 17. ZSE4000310000894050014 HAASZ Jozsef 1866 Csernatfalu Cernatu/Sacele (RO) HAASZ Salamon 18. CRE3669775101919008011 HAASZ Krisztina 1878 Hidor (H) HAASZ Antal MORSCHHAUSER Erzsebet 19. IRCK400300102000654017 HAASZ Laszlo 1922 Temesvar Timisoara (RO) 20. CRK3669775100919014074 HAASZ Maria 1919 Olasz (H) HAASZ Jakab SCHMIED Katalin 21. ZSE4000300185894015059 HAASZ Rosa 1873 Nagy-Semlak Semlacu Mare (RO) HAASZ Miksa GRUNBAUM Veronika 22. ZSE1606016028885007003 HAAZ Fani 1863 T. Abad ??? HAAZ Jakab HERSKOVITS Rozalia 23. RCE3810026340906108058 HABA Ferenc 1877 Zombor Sombor (SRB) HABA Mihaly MIHALIK Maria 24. CRE1606003212922609039 HABAKUN Anna 1904 Kistarna Khyzha (UA) HABAKUN Ivan ONUK Marie 25.