A Basis for Wise Development Decisions Croatia
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The Possible Negative Consequences of Underground
EGU Journal Logos (RGB) Open Access Open Access Open Access Advances in Annales Nonlinear Processes Geosciences Geophysicae in Geophysics Open Access Open Access Nat. Hazards Earth Syst. Sci., 13, 2041–2052, 2013 Natural Hazards Natural Hazards www.nat-hazards-earth-syst-sci.net/13/2041/2013/ doi:10.5194/nhess-13-2041-2013 and Earth System and Earth System © Author(s) 2013. CC Attribution 3.0 License. Sciences Sciences Discussions Open Access Open Access Atmospheric Atmospheric Chemistry Chemistry and Physics and Physics The possible negative consequences of underground dam and Discussions Open Access Open Access reservoir construction and operation in coastal karstAtmospheric areas: Atmospheric Measurement Measurement an example of the hydro-electric power plant (HEPP)Techniques Ombla near Techniques Dubrovnik (Croatia) Discussions Open Access Open Access T. Roje-Bonacci and O. Bonacci Biogeosciences Biogeosciences Faculty of Civil Engineering, Architecture and Geodesy, Split University, 21000 Split, Matice hrvatske 15, Croatia Discussions Correspondence to: O. Bonacci ([email protected]) Open Access Received: 5 April 2013 – Published in Nat. Hazards Earth Syst. Sci. Discuss.: 19 April 2013 Open Access Revised: 8 July 2013 – Accepted: 9 July 2013 – Published: 15 August 2013 Climate Climate of the Past of the Past Discussions Abstract. The Ombla Spring represents a typical abundant (7) conflict regarding internationally shared karst aquifers; coastal karst spring located in the vicinity of the town of (8) intensification of karst flash floods; (9) sea water intru- Open Access Dubrovnik (Croatia). Its outlet is at an altitude of 2.5 m sion in coastal karst aquifer; etc. Open Access above sea level (m a.s.l.) and the water from it immediately Earth System Earth System flows into the Adriatic Sea. -
Riviera Paklenica
MTB 04* Velebit 3 Road 02* Paklenica 1 This attractive trail through the peaks and slopes of the southern Velebit moun- This bike route is intended for riders who prefer a long, constant but not too tain will be especially appealing to the MTB and trekking riders in better physi- steep ascent. In addition, you will get the chance to see Velebit mountain cal condition for whom long ascents do not represent a greater problem. From range both from the southern and from the northern side. After the start in the sea level start on almost 1000 m hights, beautiful panoramic views of the Starigrad, the route will first take you to the Adriatic road (Jadranska magis- Velebit canal and the Zadar archipelago will help you master a long ascent with- trala) right on the coast until you reach Rovenska and then you will start to out shades. Reaching the highest peak brings the reward of temperature differ- slightly ascent the Zrmanja Canyon up to the highest point (765 m), followed ence and awe of Tulove grede towers. Long serpentine descent to the Zrmanja by 11 km of well-deserved descent towards Gračac and Ričice lake. canyon will surely put a smile on your face. Given that there are no springs nor Start/Finish Starigrad Length 52.5 km gastronomic facilities on the trail, make sure to bring enough liquids. * Via Jasenice - Zaton Physical Difficulty 2/3 Route to be marked by Start/Finish Rovanjska Length 51 km Obrovački - Elevation 831 m Discover MTB, ROAD or FAMILY the end of Via Libinjska kosa - Physical Difficulty 3/3 Gračac - Štikada 2020. -
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. -
Projekt Frisco1
PROJEKT FRISCO1 PREKOGRANIČNO USKLAĐENO SLOVENSKO-HRVATSKO SMANJENJE RIZIKA OD POPLAVA – NEGRAĐEVINSKE MJERE ČEZMEJNO USKLAJENO SLOVENSKO-HRVAŠKO ZMANJŠEVANJE POPLAVNE OGROŽENOSTI – NEGRADBENI UKREPI MURA DRAVA SOTLA/SUTLA KOLPA/KUPA BREGANA DRAGONJA 4 O projektu (ENG, HR, SI) 9 Rezultati projekta Unaprijeđene baze podataka za upravljanje rizicima od poplava 10 Izboljšane baze podatkov za obvladovanje poplavne ogroženosti Zajedničke prekogranične studije integriranog upravljanja rizicima od poplava 12 Skupne čezmejno usklajene študije celovitega obvladovanja poplavne ogroženosti Unaprijeđeni hidraulički modeli 14 Izboljšani hidravlični modeli Unaprijeđeni modeli za prognoziranje poplava 16 Izboljšani modeli za napovedovanje poplav Unaprijeđene i prekogranično usklađene karte opasnosti od poplava i 18 karte rizika od poplava Izboljšane in čezmejno usklajene karte poplavne nevarnost in poplavne ogroženosti Zajednički projekti provedbe građevinskih mjera (Priprema projektne i druge tehničke dokumentacije) 20 Skupni projekti za izvedbo gradbenih ukrepov (priprava projektne in ostale tehnične dokumentacije) Sustavi ranog upozoravanja 22 Sistemi zgodnjega opozarjanja Podizanje svijesti javnosti o rizicima od poplava 24 Ozaveščanje o poplavni ogroženosti in krepitev zmogljivosti 26 Opis porečij in prikaz možnih gradbenih ukrepov 28 Sliv Kupe / Porečje Kolpe 34 Sliv Sutle / Porečje Sotle 40 Sliv Mure / Porečje Mure 46 Sliv Drave / Porečje Drave 51 Sliv Dragonje / Porečje Dragonje 56 Sliv Bregane / Porečje Bregane Kazalo About the project ENG In -
Aquatic Molluscs of the Mrežnica River
NAT. CROAT. VOL. 28 No 1 99-106 ZAGREB June 30, 2019 original scientific paper / izvorni znanstveni rad DOI 10.20302/NC.2019.28.9 AQUATIC MOLLUSCS OF THE MREŽNICA RIVER Luboš Beran Nature Conservation Agency of the Czech Republic, Regional Office Kokořínsko – Máchův kraj Protected Landscape Area Administration, Česká 149, CZ–276 01 Mělník, Czech Republic (e-mail: [email protected]) Beran, L.: Aquatic molluscs of the Mrežnica River. Nat. Croat. Vol. 28, No. 1., 99-106, Zagreb, 2019. Results of a malacological survey of the Mrežnica River are presented. The molluscan assemblages of this river between the boundary of the Eugen Kvarternik military area and the inflow to the Korana River near Karlovac were studied from 2013 to 2018. Altogether 29 aquatic molluscs (19 gastropods, 10 bivalves) were found at 9 sites. Theodoxus danubialis, Esperiana esperi, Microcolpia daudebartii and Holandriana holandrii were dominant at most of the sites. The molluscan assemblages were very similar to assemblages documented during previous research into the Korana River. The populations of the endangered bivalves Unio crassus and Pseudanodonta complanata were recorded. An extensive population of another endangered gastropod Anisus vorticulus was found at one site. Physa acuta is the only non-native species confirmed in the Mrežnica River. Key words: Mollusca, Unio crassus, Anisus vorticulus, Mrežnica, faunistic, Croatia Beran, L.: Vodeni mekušci rijeke Mrežnice. Nat. Croat. Vol. 28, No. 1., 99-106, Zagreb, 2019. U radu su predstavljeni rezultati malakološkog istraživanja rijeke Mrežnice. Sastav mekušaca ove rijeke proučavan je na području od Vojnog poligona Eugen Kvarternik do njenog utoka u Koranu blizu Karlovca, u razdoblju 2013. -
TO SLOVENIA First Time Cultivating Wine in Protestant Literature
Compiled by FACTS Neža Lukančič & VINARIUM TOWER Benjamin Wolf The Pannonian Eiffel Tower is the SLOVENIA highest observation tower in Slovenia POPULATION: and allows a view in four countries: 2,067,000 Slovenia, Croatia, Hungary and Austria. CAPITAL CITY: LJUBLJANA (288,250) ŽIČE CHARTERHOUSE The ruins of this 12th century GDP: €43 BILLION monastery complex, overgrown with GDP PER CAPITA: ivy and moss, are a magical place. €21,000 MEŽICA MINE CROATIA ZAGREB POPULATION: The underground of Slovenia also offers hidden treasures. Sit in a small train and descend to a mine The history of Croatia’s capital dates back 4,167,000 universe that has been active for over 350 years. to the Romans. Today, the area houses a CAPITAL CITY: quarter of the country's population. ZAGREB (806,920) Zagreb’s old town boasts buildings from the 13th to the 19th century. GDP: €49 BILLION GDP PER CAPITA: OTOČEC €11,700 PREDJAMA CASTLE The only water castle in Slovenia was build on a small Source: Eurostat (2017). This Renaissance castle is built within a cave, island on Krka River. It is a favorite wedding venue, pressed next to a cliff under the original while the nearby leisure park offers fun times. Medieval fortification. METAL DAYS (SOČA) LJUBLJANA Every July, the peaceful Soča River is Slovenia’s capital stands at the middle the setting for one of the biggest heavy of a trade route between the northern metal music festivals in Europe with Adriatic Sea and the Danube region. the fitting motto: “Hell over Paradise.” Among the sights of this green city are Tivoli Park and Ljubljana Castle. -
Article N° 09 Conf. CM², Split, Croatie, 2017
Conférence Méditerranéenne Côtière et Maritime EDITION 4, SPLIT, CROATIA (2017) Coastal and Maritime Mediterranean Conference Disponible en ligne – http://www.paralia.fr – Available online Adriatic karstic estuaries, their characteristics and evolution Mladen JURAČIĆ 1 1. University of Zagreb, Faculty of Science, Department of Geology, Horvatovac 102a, 10 000 Zagreb, Croatia. [email protected] Abstract: The coastal area of the eastern Adriatic is characterized with a prevalence of carbonate rocks and well-developed karst. Present freshwater input into the Adriatic is quite large, mostly through coastal and submarine springs. However, there are also a number of rivers debouching in the Adriatic from the eastern coast. Most of them have canyon like fluviokarstic valleys that were carved dominantly during Pleistocene and were drowned during post-LGM sea-level rise forming estuaries. These estuaries are filled to a different extent during Holocene highstand (last 7.500 years). The intraestuarine delta progradation is rather different in those estuaries depending on the quantity of the river- borne material. Human impact on progradation rate in some of the estuaries has been shown. Keywords: Estuaries, Sedimentation, Intraestuarine delta, Progradation, Allogenic river, Anthopo- genic influence. https://dx.doi.org/10.5150/cmcm.2017.009 45 Mediterranean rocky coasts: Features, processes, evolution and problems 1. Introduction Eastern Adriatic coastal area is formed predominantly in Mesozoic carbonate rocks with well-developed karst (PIKELJ & JURAČIĆ, 2013). Due to prevalent humid climatic conditions and karst maturation present freshwater input into the Adriatic is large, mostly through coastal and submarine springs (vruljas). However, there are also a number of rivers debouching into the Adriatic. -
Sustainable Hydropower
Sustainable Hydropower Skadar Lake, Montenegro. © Wi in the Dinaric Arc UPDATE L Issue 4 / May 2013 d Wonder 2013 S of e urope Mi L an r adi S ic S / WW f Fresh water This newsletter provides information on the latest developments of the Dinaric Arc Sustainable Hydropower Initiative (DASHI) as well as further news on freshwater and hydropower in the region. DASHI, launched by WWF in 2011, aims to reduce the adverse impacts of hydropower development in the Western Balkans and to promote good practices in the region. The Initiative focuses on the protection of the region’s most precious freshwater ecosystems, in particular Ramsar wetlands such as Livanjsko Polje and Hutovo Blato in Bosnia and Herzegovina and Lake Skadar shared by Albania and Montenegro. HYDROPOWER NEWS FROM THE REGION WWF reveals the undiscovered world of Dinarides Through the Dinaric Arc Parks project (www.discoverdinarides.com) WWF urges the region and the world to discover the “undiscovered world of Dinarides.” The largest canyon in the world after the canyon of the Colorado River; the oldest and largest rainforest in Europe; meadows with more orchid species than there are in the whole UK; the largest and longest gorge in Europe ... all this is hiding in the Dinaric Arc region! Inspired by all these amazing facts, the creative agency Leo Burnett in Croatia designed a media campaign to promote the brand “Parks Dinarides” which can be seen from April in numerous newspapers, internet portals and on many TV stations throughout the region. www.discoverdinarides.com Energy Strategy for the “The current energy strategy for the Balkans is not in line with European Western Balkans environmental standards” (Jelko Kacin, EP MP) In February, the Committee on Foreign Affairs of the European Parliament (AFET) held a public debate on the energy strategy of the European Energy Community for the countries of the western Balkans, chaired by MP Jelko Kacin. -
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.