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Vodní Útvary Povrchových Vod Podle ORP Stránka 1/22 Název ORP Kód
Tabulka 1 - Vodní útvary povrchových vod podle ORP Stránka 1/22 rizikový vodní název ORP kód ORP ID VÚ název VÚ kategorie VÚ dílčí povodí útvar Blansko 6201 DYJ_0430 Lubě od pramene po ústí do toku Svratka řeka DYJ ano DYJ_0460 Kuřimka od pramene po vzdutí nádrže Brno řeka DYJ ano DYJ_0580 Býkovka od pramene po ústí do toku Svitava řeka DYJ ano DYJ_0590 Svitava od toku Křetínka po tok Punkva řeka DYJ ano DYJ_0600 Punkva od pramene po ponor řeka DYJ ano DYJ_0610 Bílá voda od pramene po Marianínský potok včetně řeka DYJ ano DYJ_0620 Punkva od ponoru po ústí do toku Svitava řeka DYJ ano DYJ_0630 Šebrovka od pramene po ústí do toku Svitava řeka DYJ ano DYJ_0640 Křtinský potok od pramene po ústí do toku Svitava řeka DYJ ano DYJ_0650 Svitava od toku Punkva po ústí do toku Svratka řeka DYJ ano DYJ_0710 Rakovec od pramene po Vážanský potok včetně řeka DYJ ano DYJ_0740 Říčka (Zlatý potok) od pramene po tok Roketnice řeka DYJ ano MOV_0970 Malá Haná od pramene po vzdutí nádrže Opatovice řeka MOV ano Boskovice 6202 DYJ_0360 Hodonínka od pramene po ústí do toku Svratka řeka DYJ ano DYJ_0380 Svratka od hráze nádrže Vír I. po tok Bobrůvka (Loučka) řeka DYJ ano DYJ_0420 Besének od pramene po ústí do toku Svratka řeka DYJ ano DYJ_0500 Svitava od pramene po tok Křetínka řeka DYJ ano DYJ_0510 Křetínka od pramene po vzdutí nádrže Letovice řeka DYJ ano DYJ_0525_J Nádrž Letovice na toku Křetínka jezero DYJ ano DYJ_0530 Křetínka od hráze nádrže Letovice po ústí do toku Svitava řeka DYJ ano DYJ_0540 Bělá od pramene po vzdutí nádrže Boskovice řeka DYJ ano DYJ_0550 Okrouhlý p. -
Causes and Consequences of a Flood Wave on the Lower Reach of the Dyje River Near Břeclav
Soil & Water Res., 5, 2010 (4): 121–127 Causes and Consequences of a Flood Wave on the Lower Reach of the Dyje River Near Břeclav Milan PALÁT 1, Alois PRAX1, Milan PALÁT jr.1 and Jaroslav ROžNOVSKÝ 2 1Mendel University in Brno, Brno, Czech Republic; 2Czech Hydrometeorological Institute, Brno, Czech Republic Abstract: The settlements situated on broad flat floodplains of rivers are threatened by floods during increased water flows in the rivers. The floodplain of the Dyje river situated in the area between the Nové Mlýny water reservoir and Břeclav has been protected from former annual floods since the 70s of the last century due to the water-management measures. The realised measures including the construction of the new floodway protect the town of Břeclav as well. A long-term research into the soil water regime of the floodplain forest is underway in the region. The results obtained document its historical evolution and current status. Only in the early April of 2006 (i.e. after 34 years), an unexpected “flash flood” occurred again due to a specific climatic situation. The combination of the high snow cover in higher parts of the basin and a rapid warming up caused an intensive runoff. The so-called dry polder (floodplain forests, meadows and fields) above Břeclav protected the town and its infrastructure from potential catastrophic consequences. Keywords: basin; climatic characteristics; dry polder; floodplain forest; floods; sewerage; soil water regime Urban agglomerations including the costly infra- example, spring floods in 1941 had catastrophic structures situated in the broad floodplain valleys consequences (Figure 1). of rivers are often threatened by increased water The data of the National Water Management flows. -
Tourmalinites in the Metamorphic Complex of the Svratka Unit (Bohemian Massif): a Study of Compositional Growth of Tourmaline and Genetic Relations
Journal of Geosciences, 54 (2009), 221–243 DOI: 10.3190/jgeosci.048 Original paper Tourmalinites in the metamorphic complex of the Svratka Unit (Bohemian Massif): a study of compositional growth of tourmaline and genetic relations Renata ČOpJakOvá1,2*, David BuRIánek1, Radek ŠkODa1,2, Stanislav HOuzaR3 1 Czech Geological Survey, Leitnerova 23, 658 59 Brno, Czech Republic; [email protected] 2 Institute of Geological Sciences, Masaryk University, Kotlářská 2, 611 37 Brno, Czech Republic 3 Department of Mineralogy and Petrography, Moravian Museum, Zelný trh 6, 659 37 Brno, Czech Republic * Corresponding author Tourmalinites (rocks with an association Tu + Qtz + Ms ± Grt ± Bt ± Ky ± Sil ± Pl ± Kfs) from the Svratka Unit form stratiform layers hosted in mica schists. The chemical composition of tourmaline from tourmalinites varies from Al- rich schorl to dravite. The tourmaline usually exhibits three compositional domains, which are, from centre to the rim: a chemically inhomogeneous brecciated core (zone I), a volumetrically minor internal rim zone II, and a dominant outermost zone III. X Y W X Y W The compositional variability of tourmaline in all the zones is controlled by the ( Al OH) ( Na Mg F)-1 and Y Y Fe Mg-1 substitutions. The tourmaline of the zone I corresponds to highly vacanced X-site, Al-rich schorl with lower F (up to 0.43 apfu), which is interpreted as an older, low-temperature hydrothermal tourmaline. Tourmaline of the zone II corresponds to dravite rich in F (reaching up to 0.66 apfu) crystallizing during the prograde metamorphism. Lastly, the Al-rich schorl–dravite of the zone III grew most likely during retrograde metamorphism. -
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. -
TD 4.1C Obce S Navrženou Protipovodňovou Ochranou V Rámci
Tabelární přílohy Plán oblasti povodí Dyje D. Ochrana před povodněmi a vodní režim krajiny TD 4.1c Obce s navrženou protipovodňovou ochranou v rámci krajských studií protipovodňových opatření Pracovní Obec s rozšířenou Správce číslo Obec, lokalita Kraj Vodní tok Název vodního útvaru působností toku vodního útvaru Obce na tocích Povodí Moravy, s. p. Dačice JHC Dačice Moravská Dyje PM D006 Moravská Dyje po státní hranici Staré Město pod Landštejnem JHC Jindřichův Hradec Pstruhovec PM D007 Pstruhovec po státní hranici Adamov JHM Blansko Svitava PM D061 Svitava po ústí do toku Svratka Bílovice nad Svitavou JHM Šlapanice Svitava PM D061 Svitava po ústí do toku Svratka Blansko JHM Blansko Svitava PM D055 Svitava po soutok s tokem Punkva Blížkovice JHM Znojmo Jevišovka PM D020 Jevišovka po soutok s tokem Ctidružický potok Borač JHM Tišnov Svratka PM D037 Svratka po soutok s tokem Bobrůvka Boskovštejn JHM Znojmo Jevišovka PM D026 Jevišovka po ústí do toku Dyje Brankovice JHM Bučovice Litava (Cézava) PM D067 Litava po soutok s tokem Rakovec Brno JHM Brno Svratka PM D047 Svratka po soutok s tokem Svitava Brno JHM Brno Svitava PM D061 Svitava po ústí do toku Svratka Brno-Řečkovice JHM Brno Ponávka PM D046 Ponávka po ústí do toku Svratka Brno-Židenice JHM Brno Svitava PM D061 Svitava po ústí do toku Svratka Břeclav JHM Břeclav Dyje PM D124 Dyje po soutok s tokem odlehčovací rameno -061/2 Bučovice JHM Bučovice Litava (Cézava) PM D067 Litava po soutok s tokem Rakovec Černvír JHM Tišnov Svratka PM D037 Svratka po soutok s tokem Bobrůvka Doubravice nad -
Bullard Eva 2013 MA.Pdf
Marcomannia in the making. by Eva Bullard BA, University of Victoria, 2008 A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of MASTER OF ARTS in the Department of Greek and Roman Studies Eva Bullard 2013 University of Victoria All rights reserved. This thesis may not be reproduced in whole or in part, by photocopy or other means, without the permission of the author. ii Supervisory Committee Marcomannia in the making by Eva Bullard BA, University of Victoria, 2008 Supervisory Committee Dr. John P. Oleson, Department of Greek and Roman Studies Supervisor Dr. Gregory D. Rowe, Department of Greek and Roman Studies Departmental Member iii Abstract Supervisory Committee John P. Oleson, Department of Greek and Roman Studies Supervisor Dr. Gregory D. Rowe, Department of Greek and Roman Studies Departmental Member During the last stages of the Marcommani Wars in the late second century A.D., Roman literary sources recorded that the Roman emperor Marcus Aurelius was planning to annex the Germanic territory of the Marcomannic and Quadic tribes. This work will propose that Marcus Aurelius was going to create a province called Marcomannia. The thesis will be supported by archaeological data originating from excavations in the Roman installation at Mušov, Moravia, Czech Republic. The investigation will examine the history of the non-Roman region beyond the northern Danubian frontier, the character of Roman occupation and creation of other Roman provinces on the Danube, and consult primary sources and modern research on the topic of Roman expansion and empire building during the principate. iv Table of Contents Supervisory Committee ..................................................................................................... -
EU Strategy for the Danube Region
EU Strategy for the Danube Region Consolidated Input Document of the Danube Countries for the Revision of the EUSDR Action Plan FINAL VERSION 5th July 2019, handed over to the European Commission / DG Regio on 5th July 2019 1/103 Table of Contents PRELUDE ........................................................................................................................................... 3 PART A: ............................................................................................................................................. 4 1. Scope of the Revision Process of the EUSDR Action Plan ...................................................... 4 1.1. EUSDR History ................................................................................................................... 4 1.2. The Reasons for revising the Action Plan ........................................................................ 5 1.3. The scope of the revision ................................................................................................. 8 2. Description of the Revision Process of the EUSDR Action Plan ............................................. 8 3. Results and recommendations from the evaluation ........................................................... 10 4. Proposals for drafting a Narrative for the Danube Region .................................................. 14 5. Strategic Objectives for increasing the Quality of Living in the Danube Region ................ 15 5.1. Spatial Trends in the Danube Region ........................................................................... -
Water Developments and Their Impact on Runoff in the Upper Tisa Catchment
Water developments and their impact on runoff in the Upper Tisa catchment Károly Konecsny The 157 200 km2 large catchment of the River Tisa1 is situated in the eastern part of the Carpathian Basin, also known as the Central Danube Basin. The upper catchment down to the village Záhony is 32 782, that down to Tokaj 49 449 km2 large. The origin of the name Tisa is still unclear, some linguists trace it back to an Indo European root supposed to mean muddy, or silty. In Roman documents the river is mentioned under the names Parsiou, Pthirus, Tigas and Tisianus, while in the mediaeval Latin chronicles in the forms Tisia and Tysia. Keywords: hydrology, Upper Tisa, Carpathian Basin The Upper Tisa and her tributaries in the Ukraine The headwaters of the Tisa are in the Maramuresh Alpine Mountains, the name Tisa is used downstream of the confluence of the Chorna Tisa and Bila Tisa. Of her 962 km total length, the mountain section is only 200 km long. From the confluence of the Chorna Tisa and the Bila Tisa down to the mouth of the Vi§eu the average slope of the valley floor is very steep, 6.33 m/km, between the Vi§eu and the Tereblja 2.28 m/km, flattening down to Tiszabecs to less than l m/km. Over the mountain section the valley is narrow, the river having carved her up to 50 m wide bed between steep banks. The normal depth is a few decimetres. Beyond her emergence into the plains at Hust the Tisa becomes a typically lowland river meandering in a spreading valley. -
Harmonirib River Basin Data Documentation Chapter 2 - Svratka River Basin November 2006
Povodi Moravy, (Morava River Basin Administration), Brno, Czech Republic HarmoniRiB River Basin Data Documentation Chapter 2 - Svratka River Basin November 2006 Harmonised techniques and representative river basin data for assessment and use of uncertainty information in integrated water management Contract EVK1-CT-2002-00109 Author Pavel Biza, Povodi Moravy, (Morava River Basin Administration), Brno, Czech Republic HarmoniRiB River Basin Data Documentation Chapter 2 - Svratka River Basin November 2006 Harmonised techniques and representative river basin data for assessment and use of uncertainty information in integrated water management Contract EVK1-CT-2002-00109 This report is Chapter 2 of a publicly accessible deliverable D6.3 of the HarmoniRiB project. This R&D project is partly financed within the European Commission´s “Energy, Environment and Sustainable Development” programme, Key Action 1 “ Sustainable Management and Quality of Water”, 1.1 Integrated management and sustainable use of water resources at catchment river basin or sub-basin scale, 1.1.1 Strategic planning and integrated management methodologies and tools at catchment / river scale under contract EVK1-CT 2002-00109. This report may be downloaded from the internet and copied, provided that it is not changed and provided that proper reference to it is made: Pavel Biza. Chapter 2 - Svratka River Basin. Povodi Moravy, (Morava River Basin Administration), Brno, Czech Republic, November 2006 (www.harmonirib.com) or (http://workplace.wur.nl/QuickPlace/harmonirib/Main.nsf/h_Toc/38da1522d3c0e520c12571 -
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. -
Materials and Methods
1 Phylogeography and population genetics of the European mudminnow 2 (Umbra krameri) with a time-calibrated phylogeny for the family Umbridae 3 4 Saša Marić1, David Stanković2,3, Josef Wanzenböck4, Radek Šanda5, Tibor Erős6, Péter 5 Takács6, András Specziár6, Nenad Sekulić7, Doru Bănăduc8, Marko Ćaleta9, Ilya Trombitsky10, 6 Laslo Galambos11, Sandor Sipos12, Aleš Snoj2* 7 8 1 Institute of Zoology, Faculty of Biology, University of Belgrade, Studentski trg 16, 11001 9 Belgrade, Serbia 10 2 Department of Animal Science, Biotechnical Faculty, University of Ljubljana, Groblje 3, SI- 11 1230 Domžale, Slovenia 12 3 Department of Life Sciences, University of Trieste, Via Licio Giorgieri 5, 34127 Trieste, Italy 13 4 Research Institute for Limnology, University of Innsbruck, Mondseestraße 9, 5310 Mondsee, 14 Austria 15 5 National Museum, Department of Zoology, Václavské náměstí 68, 115 79 Prague 1, Czech 16 Republic; 17 6 Balaton Limnological Institute, MTA Centre for Ecological Research, Klebelsberg Kuno u. 18 3, H-8237 Tihany, Hungary 19 7 Institute for Nature Conservation of Serbia, Dr Ivana Ribara 91, 11070 Novi Beograd, Serbia 20 8 Faculty of Sciences, Lucian Blaga University of Sibiu, Dr. Ion Raţiu 5-7, RO-550012, Sibiu, 21 Romania 22 9 Faculty of Teacher Education, University of Zagreb, Savska cesta 77, 10000 Zagreb, Croatia 1 23 10 Eco-TIRAS International Association of Dniester River Keepers, Teatrala 11A, Chisinau 24 2012, Moldova 25 11 Institute for Nature Conservation of Vojvodina, Radnička 20a, 21000 Novi Sad, Serbia 26 12 Department of Biology and Ecology, Faculty of Science, University of Novi Sad, Trg D. 27 Obradovića 2, Novi Sad, Serbia 28 29 30 * Corresponding author: Aleš Snoj 31 Telephone number: 00 386 1 3203 912 32 Fax number: 00 386 1 3203 888 33 E-mail: [email protected] 34 35 36 37 38 39 40 41 42 43 Abstract 2 44 The genetic structure of European mudminnow populations throughout the species range was examined using 45 mitochondrial DNA and seven microsatellite loci. -
EU Strategy for the Danube Region
EU Strategy for the Danube Region Consolidated Input Document of the Danube Countries for the Revision of the EUSDR Action Plan FINAL VERSION 11th July 2019 (V1) endorsed by EUSDR NCs handed over to the European Commission / DG Regio on 11th July 2019 1/103 Table of Contents PRELUDE ....................................................................................................................................... 3 PART A: Strategic and operational framework ........................................................................... 4 1. Scope of the Revision Process of the EUSDR Action Plan ...................................................... 4 1.1. EUSDR History ....................................................................................................................... 4 1.2. The Reasons for revising the Action Plan ............................................................................ 5 1.3. The scope of the revision ..................................................................................................... 8 2. Description of the Revision Process of the EUSDR Action Plan ............................................. 8 3. Results and recommendations from the evaluation ........................................................... 10 4. Proposals for drafting a Narrative for the Danube Region .................................................. 14 5. Strategic Objectives for increasing the Quality of Living in the Danube Region ................ 15 5.1. Spatial Trends in the Danube Region ...............................................................................