The Kupa River in Antiquity: a Preliminary Reconstruction of a Fluvial Landscape and Its Navigation Practices Anton Divić, Giulia Boetto, Krunoslav Zubčić
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FEEFHS Journal Volume VII No. 1-2 1999
FEEFHS Quarterly A Journal of Central & Bast European Genealogical Studies FEEFHS Quarterly Volume 7, nos. 1-2 FEEFHS Quarterly Who, What and Why is FEEFHS? Tue Federation of East European Family History Societies Editor: Thomas K. Ecllund. [email protected] (FEEFHS) was founded in June 1992 by a small dedicated group Managing Editor: Joseph B. Everett. [email protected] of American and Canadian genealogists with diverse ethnic, reli- Contributing Editors: Shon Edwards gious, and national backgrounds. By the end of that year, eleven Daniel Schlyter societies bad accepted its concept as founding members. Each year Emily Schulz since then FEEFHS has doubled in size. FEEFHS nows represents nearly two hundred organizations as members from twenty-four FEEFHS Executive Council: states, five Canadian provinces, and fourteen countries. lt contin- 1998-1999 FEEFHS officers: ues to grow. President: John D. Movius, c/o FEEFHS (address listed below). About half of these are genealogy societies, others are multi-pur- [email protected] pose societies, surname associations, book or periodical publish- 1st Vice-president: Duncan Gardiner, C.G., 12961 Lake Ave., ers, archives, libraries, family history centers, on-line services, in- Lakewood, OH 44107-1533. [email protected] stitutions, e-mail genealogy list-servers, heraldry societies, and 2nd Vice-president: Laura Hanowski, c/o Saskatchewan Genealogi- other ethnic, religious, and national groups. FEEFHS includes or- cal Society, P.0. Box 1894, Regina, SK, Canada S4P 3EI ganizations representing all East or Central European groups that [email protected] have existing genealogy societies in North America and a growing 3rd Vice-president: Blanche Krbechek, 2041 Orkla Drive, group of worldwide organizations and individual members, from Minneapolis, MN 55427-3429. -
Primjena Indeksa Kvalitete Vode U Ocjeni Kakvoće Vode Krških Jezera
D. tomas et al. PrimjenA inDeksa kvAlitete voDe u ocjeni kAkvoće voDe kRških Jezera Stručni članak Professional paper UDk 556.55:556.114/.115>(497.5 Cres) primljeno (Received): 10. 7. 2013.; prihvaćeno (Accepted): 27. 11. 2013. primjena inDeKsa Kvalitete voDe u oCjeni KaKvoće voDe KršKih jezera U radu je prikazana kakvoća vode jezera primjenom indeksa Damir tomas, dipl. ing. kvalitete vode (eng. Water Quality Index, WQI) i njihov kemijski Hrvatske vode, Glavni vodnogospodarski laboratorij sastav Piperovim dijagramom. Ispitivana su jezera: Vrana na otoku Ulica Grada Vukovara 220, 10000 Zagreb Cresu, Vransko jezero kod Biograda na Moru, Baćinsko jezero [email protected] Crniševo i akumulacija Butoniga u razdoblju 2010.-2012. godine. Krešimir maldini, dipl. ing. U izračunu WQI korišteni su sljedeći pokazatelji: pH vrijednost, Hrvatske vode, Glavni vodnogospodarski laboratorij ukupna otopljena tvar (TDS), hidrogenkarbonati, ukupna tvrdoća, Ulica Grada Vukovara 220, 10000 Zagreb kloridi, sulfati, nitrati, fluoridi, kalcij, magnezij, željezo i mangan. Za izračun WQI korištene su preporuke vode za piće Svjetske natalija matić, dipl. ing. Hrvatske vode, EU jedinica zdravstvene organizacije (eng. World Health Organization, WHO) Ulica Grada Vukovara 220, 10000 Zagreb te dobiveni WQI predstavlja prikladnost voda za uporabu u vodoopskrbi. mr. sc. marija marijanović rajčić, dipl. ing. Istraživanjem je utvrđeno da je kakvoća vode na Vranskom jezeru Hrvatske vode, Glavni vodnogospodarski laboratorij kod Biograda n/m bila najlošije kvalitete u 2012. godini (WQI=870), Ulica Grada Vukovara 220, 10000 Zagreb dok je najbolja kakvoća vode zabilježena na jezeru Vrana na otoku Cresu u 2012. godini (WQI=31,2). Prema Piperovom dijagramu ispitivana jezera se po kemijskom sastavu razlikuju ovisno o hidrološkom dobu, dok je Vransko jezero na Cresu ujednačene kakvoće. -
STRATEGIC ENVIRONMENTAL ASSESSMENT of the COOPERATION PROGRAMME SLOVENIA – CROATIA 2014-2020 APPENDIX 1: APPROPRIATE ASSESSMENT
Dvokut ECRO d.o.o. ZaVita, svetovanje, d.o.o. Integra Consulting s.r.o. Trnjanska 37 Tominškova 40 Pobrezni 18/16, 186 00 HR -10000 Zagreb, Hrvaška 1000 Ljubljana , Slovenija Pragu 8 , Republika Češka STRATEGIC ENVIRONMENTAL ASSESSMENT of the COOPERATION PROGRAMME SLOVENIA – CROATIA 2014-2020 APPENDIX 1: APPROPRIATE ASSESSMENT SEA REPORT Ljubljana, March 2015 This project is funded by the European Union Strategic Environmental Assessment of the Cooperation Programme INTERREG V-A Slovenia-Croatia 2014-2020 Appendix: Appropriate Assessment Strategic environmental assessment of the Cooperation Programme Slovenia – Croatia 2014-2020 Appendix 1: Appropriate Assessment SEA REPORT Contracting Authority : Republic of Slovenia Government Office for Development and European Cohesion Policy Kotnikova 5 SI-1000 Ljubljana, Slovenia Drafting of the PHIN Consulting & Training d.o.o. Cooperation Programme: Lanište 11c/1 HR-10000 Zagreb, Croatia K&Z, Development Consulting ltd. Kranjska cesta 4, 4240 Radovljica, Slovenia Drafting of the ZaVita, svetovanje, d.o.o. Environmental Report: Tominškova 40 SI-1000 Ljubljana, Slovenia Responsible person: Matjaž Harmel, Director Dvokut –ECRO d.o.o. Trnjanska 37 HR-10000 Zagreb, Croatia Responsible person: Marta Brkić, Director Integra C onsulting s.r.o. Pobrezni 18/16, 186 00 Pragu 8, Czech Republic Responsible person: Jiří Dusík, Director Project team leader: Matjaž Harmel, B. Sc. Forestry Project team deputy team leader: Klemen Strmšnik, B. Sc. Geography Project team members: Aleksandra Krajnc, B. Sc. Geography Marta Brkić, MA Landscape art and Architecture Jiří Dusík, M. Sc. Engeneering Jelena Fressl, B.Sc. Biology Ivana Šarić, B.Sc. Biology, Daniela Klaić Jančijev, B.Sc. Biology, Konrad Kiš, MSc Forestry Katarina Bulešić, Master of Geography Tomislav Hriberšek, B.Sc. -
Groundwater Bodies at Risk
Results of initial characterization of the groundwater bodies in Croatian karst Zeljka Brkic Croatian Geological Survey Department for Hydrogeology and Engineering Geology, Zagreb, Croatia Contractor: Croatian Geological Survey, Department for Hydrogeology and Engineering Geology Team leader: dr Zeljka Brkic Co-authors: dr Ranko Biondic (Kupa river basin – karst area, Istria, Hrvatsko Primorje) dr Janislav Kapelj (Una river basin – karst area) dr Ante Pavicic (Lika region, northern and middle Dalmacija) dr Ivan Sliskovic (southern Dalmacija) Other associates: dr Sanja Kapelj dr Josip Terzic dr Tamara Markovic Andrej Stroj { On 23 October 2000, the "Directive 2000/60/EC of the European Parliament and of the Council establishing a framework for the Community action in the field of water policy" or, in short, the EU Water Framework Directive (or even shorter the WFD) was finally adopted. { The purpose of WFD is to establish a framework for the protection of inland surface waters, transitional waters, coastal waters and groundwater (protection of aquatic and terrestrial ecosystems, reduction in pollution groundwater, protection of territorial and marine waters, sustainable water use, …) { WFD is one of the main documents of the European water policy today, with the main objective of achieving “good status” for all waters within a 15-year period What is the groundwater body ? { “groundwater body” means a distinct volume of groundwater within an aquifer or aquifers { Member States shall identify, within each river basin district: z all bodies of water used for the abstraction of water intended for human consumption providing more than 10 m3 per day as an average or serving more than 50 persons, and z those bodies of water intended for such future use. -
ACTIVE FLOOD DEFENCE in CROATIA: Regulatory Framework, Roles & Responsibilities
Workshop on Flood Risk Management measures & links to EU WFD November 11-12, 2015, Zagreb, Croatia ACTIVE FLOOD DEFENCE IN CROATIA: regulatory framework, roles & responsibilities Zoran Đurokovi ć, M.Sc.C.E. Croatian Waters Main Flood Protection Centre Head of Main Centre ∗ Climate change has intensified in recent years worldwide, including Croatia ∗ Extremely dry and wet periods have been alternating frequently in the last approximately 15 years ∗ Damage from extreme hydrological events is increasing ∗ “Average” or “normal” years are becoming increasingly rarer ∗ The frequency of high water waves and extreme water levels including floods is increasing ∗ There are almost no longer any rules concerning the occurrence of high water waves ∗ Forecasting climate models indicate increasingly frequent extreme climate events, both globally and locally ∗ Only in the last 15 years or so, the major part of the Croatian territory has experienced frequent extreme hydrological events which caused droughts in the years 2000, 2003, 2011 and 2012, but also floods in the years 2002, 2004, 2005, 2006, 2009, 2010, 2012, 2013, 2014 and 2015 ∗ Heavy damage is recorded, primarily in agriculture, but settlements, infrastructure and industrial facilities are also at risk ∗ Still, unlike in many other countries, major fatalities and disastrous damage in the urban areas have been avoided in Croatia ∗ Floods are natural phenomena which cannot be completely prevented. However, flood risks can be reduced to an acceptable level through constant development of flood -
DIKTAS Country Report
Protection and Sustainable Use of the Dinaric Karst Transboundary Aquifer System Country Report (Regional Aspect) - Croatia http://diktas.iwlearn.org Protection and Sustainable Use of the Dinaric Karst Transboundary Aquifer System Contents HYDROGEOLOGICAL OVERVIEW 1. Introduction 1.1. Project task and role of WG1 1.2. General on karst – term, distribution. Importance 1.3. Histrical review of karst researches 2. Physiography and climate 2.1. Geographic position and boundaries 2.2. Vegetation and land cover 2.3. Rainfall regime 2.4. Air temperature 2.5. Other climate elements 3. Hydrology 3.1. Hydrographic network 3.2. Stream-flow regime 3.3. Controlling streamflow – dams and reservoirs 4. Geological pattern 4.1. Paleogeography of Dinaric region 4.2. Dinaric Carbonate Platform (External Dinarides) - litostratigraphic units 4.3. Tectonic 5. Geomorphology and karstification 5.1. Karstification process 5.2. Karstic features 5.2.1. Surface karstic features 5.2.2. Potholes and caves 6. Aquifer systems 6.1. Aquifers classification and distribution 7. Groundwater basins 7.1. Regional groundwater direction 7.2. Grounwater bodies ENVIRONMENT AND SOCIO-ECONOMIC OVERVIEW 1. Administrative boundaries 2. Population and demography 3. Tourism 4. Land use 5. Sources of income 6. Agriculture 7. Roads 8. Industries 9. Mining sites 10. Solid waste disposal 11. Wastewater treatment Protection and Sustainable Use of the Dinaric Karst Transboundary Aquifer System 12. Dams and Hydropower Plants 13. Protected areas 14. Karstic caves 15. Groundwater dependent ecosystems 16. Water use 17. Surface water quality LEGAL AND INSTITUTIONAL FRAMEWORK AND POLICY 1. Introduction 2. Updated report on legal, institutional and policy framework in Croatia 3. -
Case Study of Kupa River Watershed in Croatia
J. Hydrol. Hydromech., 67, 2019, 4, 305–313 DOI: 10.2478/johh-2019-0019 Long term variations of river temperature and the influence of air temperature and river discharge: case study of Kupa River watershed in Croatia Senlin Zhu1, Ognjen Bonacci2, Dijana Oskoruš3, Marijana Hadzima-Nyarko4*, Shiqiang Wu1 1 State Key Laboratory of Hydrology-Water resources and Hydraulic Engineering, Nanjing Hydraulic Research Institute, Nanjing 210029, China. 2 Faculty of Civil Engineering and Architecture, University of Split, Matice hrvatske 15, 21000 Split, Croatia. 3 Meteorological and Hydrological Service, Gric 3, 10000 Zagreb, Croatia. 4 Josip Juraj Strossmayer University of Osijek, Faculty of Civil Engineering and Architecture Osijek, Vladimira Preloga 3, 31000 Osijek, Croatia. * Corresponding author. E-mail: [email protected] Abstract: The bio-chemical and physical characteristics of a river are directly affected by water temperature, which therefore affects the overall health of aquatic ecosystems. In this study, long term variations of river water temperatures (RWT) in Kupa River watershed, Croatia were investigated. It is shown that the RWT in the studied river stations in- creased about 0.0232–0.0796ºC per year, which are comparable with long term observations reported for rivers in other regions, indicating an apparent warming trend. RWT rises during the past 20 years have not been constant for different periods of the year, and the contrasts between stations regarding RWT increases vary seasonally. Additionally, multi- layer perceptron neural network models (MLPNN) and adaptive neuro-fuzzy inference systems (ANFIS) models were implemented to simulate daily RWT, using air temperature (Ta), flow discharge (Q) and the day of year (DOY) as predic- tors. -
Navigational Characteristics of Lower Sava – Determining Draught and Carring Capacity of Ships
I. ŠKILJAICA et al. NAVIGATIONAL CHARACTERISTICS OF LOWER SAVA... Navigational Characteristics of Lower Sava – Determining Draught and Carring Capacity of Ships IVAN V. ŠKILJAICA, University of Novi Sad, Original scientific paper Faculty of Technical Sciences, Novi Sad UDC: 656.628.1:629.546 Department of Traffic Engineering DOI: 10.5937/tehnika1805677S VLADIMIR S. ŠKILJAICA, University of Novi Sad, Faculty of Technical Sciences, Department of Traffic Engineering, Novi Sad This paper presents the procedure for calculation of possible values of draught of ships or barges in pushed convoy while navigating through certain sections of Lower Sava which have characteristic shapes and dimensions. The goals of the paper is to, based on known calculation procedures, determine the value of possible draughts of ships or pushed convoys through this section with restrictions in navigating conditions, or to determine periods of the year when ships or pushed convoys can achieve best results during exploitation. Key words: ship; barge; navigation, water levels; limited depths; limited draughts 1. INTRODUCTION ces significantly as it enters Pannonian Plain. The Danube, besides that it connects Serbia and Between the mouth of river Kupa all the way to its Croatia, at the same time connects the whole region not mouth Sava river’s slope has gradient of 42 mm/km, only to other countries on the Danube, but to the which makes it become a low land river which me- countries of the Middle East as well. This waterway nders a lot. Due to such low gradient of the slope Sava carries significant part of international trade of the river is not capable of transporting alluvium brought countries in the region. -
Research Article
Ecologica Montenegrina 44: 69-95 (2021) This journal is available online at: www.biotaxa.org/em http://dx.doi.org/10.37828/em.2021.44.10 Biodiversity, DNA barcoding data and ecological traits of caddisflies (Insecta, Trichoptera) in the catchment area of the Mediterranean karst River Cetina (Croatia) IVAN VUČKOVIĆ1*, MLADEN KUČINIĆ2**, ANĐELA ĆUKUŠIĆ3, MARIJANA VUKOVIĆ4, RENATA ĆUK5, SVJETLANA STANIĆ-KOŠTROMAN6, DARKO CERJANEC7 & MLADEN PLANTAK1 1Elektroprojekt d.d., Civil and Architectural Engineering Department, Section of Ecology, Alexandera von Humboldta 4, 10 000 Zagreb, Croatia. E-mails:[email protected]; [email protected] 2Department of Biology (Laboratory for Entomology), Faculty of Science, University of Zagreb, Rooseveltov trg 6, 10 000 Zagreb, Croatia. E-mail: [email protected] 3Ministry of Economy and Sustainable Development, Radnička cesta 80/7, 10000 Zagreb, Croatia. E-mail: [email protected] 4Croatian Natural History Museum, Demetrova 1, 10 000 Zagreb, Croatia. E-mail: [email protected] 5Hrvatske vode, Central Water Management Laboratory, Ulica grada Vukovara 220, 10 000 Zagreb, Croatia. E-mail:[email protected] 6Faculty of Science and Education, University of Mostar, Matice hrvatske bb, 88000 Mostar, Bosnia and Herzegovina. E-mail: [email protected] 7Primary School Barilović, Barilović 96, 47252 Barilović and Primary School Netretić, Netretić 1, 47271 E-mail: [email protected] *Corresponding author: [email protected] **Equally contributing author Received 2 June 2021 │ Accepted by V. Pešić: 19 July 2021 │ Published online 2 August 2021. Abstract The environmental and faunistic research conducted included defining the composition and distribution of caddisflies collected using ultraviolet (UV) light trap at 11 stations along the Cetina River, from the spring to the mouth, and also along its tributaries the Ruda River and the Grab River with two sampling stations each, and the Rumin River with one station. -
Commercial Inland Fishing in Member Countries of the European Inland Fisheries Advisory Commission (EIFAC)
Commercial inland fishing in member countries of the European Inland Fisheries Advisory Commission (EIFAC): Operational environments, property rights regimes and socio-economic indicators Country Profiles May 2010 Mitchell, M., Vanberg, J. & Sipponen, M. EIFAC Ad Hoc Working Party on Socio-Economic Aspects of Inland Fisheries The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO in preference to others of a similar nature that are not mentioned. The views expressed in this information product are those of the author(s) and do not necessarily reflect the views of FAO. All rights reserved. FAO encourages the reproduction and dissemination of material in this information product. Non-commercial uses will be authorized free of charge, upon request. Reproduction for resale or other commercial purposes, including educational purposes, may incur fees. Applications for permission to reproduce or disseminate FAO copyright materials, and all queries concerning rights and licences, should be addressed by e-mail to [email protected] or to the Chief, Publishing Policy and Support Branch, Office of Knowledge Exchange, Research and Extension, FAO, Viale delle Terme di Caracalla, 00153 Rome, Italy. © FAO 2012 All papers have been reproduced as submitted. -
Impact of Climate Variability and Change on the Kupa River
Impact of Climate Variability and Change on the Kupa River Dušan Trninić, Tomislava Bošnjak Meteorological and Hydrological Service Zagreb, CROATIA Abstract The latest studies on climate variability and changes in South and East Europe, including Croatia, the continued air temperature increase trend is expected to be accompanied by further decrease in precipitation and, consequently, number of days with snow and snow cover, decrease in runoff, land humidity and availability of water resource. The results of studies on climate variability and changes (WMO, UNEP, 2008) indicate 23-36 % decrease in annual runoff in South and East Europe for time thresholds set at 2020, 2050 and 2070. The Kupa River annual runoff analysis for the locations near Hrvatsko and Kamanje (period: 1957-2008) shows a decreasing trend. An outcome of such, less than optimistic, forecast is a need for demanding water resources management. The observations and forecasts of climate variability and changes should be continued, focusing in particular on the near future. Also, it is necessary to continue with observation of meteorological and hydrological values for the region and take into consideration the anthropological impact on climate variability and changes. Keyword: climate variability and changes, runoff, Kupa River Introduction Significant meteorological, hydrological, morphological, sediment and other changes have recently been observed in the Kupa River catchment area. Some results of the annual precipitation amount and annual runoff analyses are presented in this paper. The increasing presence of scientifically verified climate variability and changes should be highlighted as well as intensified anthropological impact on hydrological regime. The increasing climate variability and changes, and presence of anthropological impacts, complicate the water-related problems at the entire Croatian territory, including the Kupa River catchment area. -
High Flows from Gornja Dobra Basin
45 The Mining-Geology-Petroleum Engineering Bulletin High ƪ ows from Gornja Dobra basin UDC: 556.5 DOI: 10.17794/rgn.2018.3.5 Professional paper Krešimir Pavli©1; Daniel Jakobovi©2 1 University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Pierottijeva 6, p.p. 390, 10000 Zagreb 2 HIS d.o.o. Donja Višnjica 61D, 42255 Donja Višnjica Abstract This paper presents basic hydrological indicators based on data from the four existing hydrological stations in the Gorn- ja Dobra basin. The frequency and ƪ ow-duration curves of mean daily ƪ ow in the Turkovi©i proƤ le are also deƤ ned and presented. The dependence of the mean maximum annual speciƤ c ƪ ows on the size of the inƪ uential basin to the con- sidered hydrological proƤ les was considered. A review of the most recent high water event in 2017 was given. Keywords Gornja Dobra, frequency and ƪ ow-duration curve, maximum speciƤ c ƪ ow, stage-discharge curve, big water wave. 1. Introduction The main objective of this paper is to determine the dependence of mean maximum annual speci¿ c dis- The Dobra River can be divided into three character- charge qժ M on the size of the inÀ uential basin, to de¿ ne istic areas of À ow. The ¿ rst, known as the Gornja (Up- the frequency and À ow-duration curves of mean daily per) or Ogulinska Dobra, is 51.2 km long, stretches from À ows and to analyse the most recent À ood event that oc- the spring on the north-eastern slopes of the Mlada Gora curred in Ogulin in September 2017.