9.Zeljko Incorporating Existing Modeling Along the Sava River

Total Page:16

File Type:pdf, Size:1020Kb

9.Zeljko Incorporating Existing Modeling Along the Sava River Sava River Flood Mapping Workshop Incorporating Existing Modeling along the Sava River Dragan Zeljko Deputy Secretary for RBM and water planning Contents • Brief history of cooperation • Overview of collected data from the countries • Data processing by the ISRBC • Final results • Tips & tricks • Lessons learned • What next? 2 Brief history of cooperation • June 2008 - Dr. Kathleen D. White (USACE) participated on the PEG FP meeting • the PEG FP is willing to develop a single hydraulic model of the Sava River and its major tributaries for the purpose of developing a comprehensive systems approach to flood risk management in the Sava River Basin; • Overbank mapping of the Sava River and its major tributaries with sufficient resolution to generate flood-inundation and flood-risk maps with a reasonable level of uncertainty ; • Ability to provide flood forecasts; • GIS methodology to support model development, especially Geo-RAS, with automated procedures for updating either independently or by the Commission as new information becomes available 3 Brief history of cooperation • September 2009 – USACE prepared ToR and Scope and Needs documents – First approximate Sava River hydraulic model • December 2009 – ISRBC requested data from national institutions • January – April 2010 – data submitting • February – July 2010 – ISRBC processing data • All the time – numerous teleconferences USACE – ISRBC • ftp site created for exchanging data 4 Overview of data collected from the countries • What has been collected? – Hydrologic data; – Hydraulic models; – Geometry in various formats; – Bathymetry data; – Descriptions of the system... Everything usable and available 5 Overview of data collected from the countries 6 Geometry, models & other data - HR SAVA • HEC-RAS (km 213- 458) > 1200 XS – 01jamena_zupanja.g01 – 02zupanja_samac.g01 – 03samac_brod.g02 – 04brod_mackovac.g01 • MIKE 11 (km 458-728) > 900 XS – Mackovac – Jesenice (HR) 7 Geometry, models & other data - HR Tributaries (and channels) • HEC2 – Sutla 0-24 km – Krapina 0-58 km – Bosut 0-130 km • MIKE 11 – Odra 0-33 km – Lonja -Strug 0-8 km; 0-5 km – Una 0-42 km – Kupa 0-80 km 8 Geometry, models & other data - HR SAVA (ACAD stream centerline & XS cutlines) 9 Geometry, models & other data - RS SAVA • HEC-RAS model (km 0-209) > 200 XS – Beograd-Jamena.g01 10 Geometry, models & other data - RS SAVA • (ACAD stream centerline & XS cutlines) 11 Geometry, models & other data - BA • HEC-RAS models of: – Vrbas (km 0-35) and Tinja (km 0-44) • Various usable data for Brka and Bosnia 12 Geometry, models & other data – RS and BA • Bathymetric data (2004 and 2009) 13 Geometry, models & other data – SRTM 90 m DEM – ASTER 30m GDEM – GIS data prepared in Secretariat (banks, levee placements etc...) – Sava River waterway centerline (agreed) 14 Data processing by the ISRBC • Challenging effort because of: – Huge amount of collected data – Different formats (HEC2; HEC-RAS;MIKE 11...) – Need for use of various applications (ArcGIS, Mike 11, HEC- RAS, Google Earth...) – No single model-geometry collected was truly georeferenced • Final aim: – To provide georeferenced (in UTM34 zone) HEC-RAS geometry to the USACE for further model set up 15 Final results Georeferenced model of the: -Sava River (BG- Jesenice-HR) -Sutla, Krapina, Bosut,Una, Vrbas, Tinja -Lonja-Strug, Odra > 3000 XS 16 Tips & tricks • Georeferencing –ACAD file available dwg – coordinates in GK7 projection Dwg shp georef GeoRAS RAS 17 Tips & tricks • Georeferencing –ACAD file NOT available Krapina River example kml shp georef GeoRAS RAS 18 Tips & tricks Krapina – before processing Krapina – after processing 19 Tips & tricks • Georeferencing –preparation and import of stream centerline 20 Tips & tricks • Mike 11 to HEC-RAS 21 Tips & tricks • Mike 11 to HEC-RAS 22 Tips & tricks • HEC RAS to Mike 11 • Additional tools required 23 Lessons learned • Each data usable • Start modeling from available data • Georeferencing is very important for mapping • High importance of cooperation in the Sava RB • Find mechanisms for faster response in data collection 24 What next? • Tributaries- precise georeferencing needed • Levees – updata&upgrade missing information • Update geometry with new bathymetric data • Incorporate SI data in the model • Decision on further rights in use of the model • New hydrologic study needed 25.
Recommended publications
  • Vegetation FORESTS
    CROATIA Climate and vegetation Geographic position of Croatia- Central European-mediterranean country Basic information about Croatia The land area 56594 km2 The teriritorial waters 31.067 km2 Lenght of coast 1777 km Number of islands, islets and reefs 1185 The highest point above the sea level 1831 m Number of countys 21 Number of cities and municiplalities 127 - 429 Population 4.290.612 Population on km2 78,1 Number of inhabited islands 48 Language Croatian Script Latin Political system Parliamentary democracy GDP per capita in 2012 10203 Breaking up Croatia into Counties Natural-geographic areas of Croatia Panonian-peripanonian region(includes 55% of the territory and 66% of the population) Mediterranean or Croatian coastal region(includes 31% of the territory and 31% of the population) Mountainous or Dinaric region (includes 14% of the territory and 3% of the population) Climate Climactic characteristics of Croatia are a result of its location in the mid-latitude, the influence of the Mediterranean and Atlantic seas as well as the shape and relief (mountains along the coast and Panonian plain). - moderate continental climate - Mediterranean climate - mountainous climate Vegetation FORESTS (climazonal vegetation) Mediterannean region covers approximately 40% of Croatia’s surface, here we find 17 forest communities; Eurosiberian-North American region covers about 60% of Croatia’s surface, where there are 45 forest communities. NON-FOREST VEGETATION Created by human activity – lawns, meadows, pastures, underbrush Spatial distribution
    [Show full text]
  • 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.
    [Show full text]
  • Final Report Land Use Analyses
    The relevance of farming and farmland for maintaining the landscape and biodiversity of the Sava floodplains Final report of Task C of the Life 3 rd countries project Protection of Biodiversity of the Sava River Basin Floodplains Wageningen International December 2009 WageningenInternational The relevance of farming and farmland for maintaining the landscape and biodiversity of the Sava floodplains Final report of Task C of the Life 3 rd Countries Program Protection of Biodiversity of the Sava River Basin Floodplain (LIFE06 TCY INT 246 ) The following report is based on the reports of the Land Use Working Group The editors of the three country reports are: Croatia- Ivana Ilijas, Jasna Jeremic, Andreja Ribaric State Institute for Nature Protection of Croatia Serbia- Alen Kis, Laslo Galambos, Dejan Bakovic, Klara Szabados and Milos Vukelic; Institute for Nature Conservation Serbia Bosnia and Herzegovia- Tihomir Predic- Agricultural Institute Banja Luka ABSTRACT Author(s) Zingstra, Henk ( final edit), Alen Kis, Andreja Ribaric, Dejan Bakovic, Ivana Ilijas, Jasna Jeremic, Laslo Galambos, Klara Szabados, Milos Vukelic, Tihomir Predic ; The relevance of farmland and farming for the protection of the landscape and biodiversity of the Sava Floodplains, Final Report of Task C of the EU-LIFE06 TCY INT 246 Project. Photos: Institute for Nature Conservation of Croatia, Agricultural Institute Banja Luka. Keywords: Land use, agriculture, agri environment, flood protection, nature conservation. © 2009 Wageningen International P.O. Box 88; 6700 AB Wageningen; The Netherlands No part of this publication may be reproduced or published in any form or by any means, or stored in a database or retrieval system without the written permission of Wageningen International.
    [Show full text]
  • Sava River Position Paper Prepared by Euronatur Supported by Croatian Society for Bird and Nature Protection (HDZPP) and Birdlife Slovenia (DOPPS)
    Sava River Position Paper Prepared by EuroNatur Supported by Croatian Society for Bird and Nature Protection (HDZPP) and BirdLife Slovenia (DOPPS) Introduction EuroNatur has been dedicated to nature conservation and the sustainable use of natural resources in the Sava River Basin for the last 25 years. In our role as an official observer of the Sava Commission EuroNatur has been following the processes of the Commission and the ongoing development of the Sava River Basin Management Plan with attention. Hereby we would like to comment on some questions related to further infrastructural development and regulation of the Sava River, which are urgent and alarming from our point of view. Moreover, we are offering recommendations and suggestions regarding these issues. Comments on the focus of the Sava Commission (ISRBC) The International Sava River Basin Commission (ISRBC) has been established for the purpose of realization of the following goals: I. Establishment of an international regime of navigation on the Sava River II. Establishment of sustainable water management III. Undertaking of measures to prevent or limit hazards Although the second goal includes the availability of “water in sufficient quantity and of appropriate quality for the preservation, protection and improvement of aquatic eco-systems (including flora and fauna and eco-systems of natural ponds and wetlands)” no working group was implemented that is adequately dealing with such issues as the monitoring and protection of the Sava River and connected aquatic ecosystems. Most publications that were elaborated by the ISRBC so far miss a clear reference to biodiversity and nature conservation topics, but deal with navigation and water management issues.
    [Show full text]
  • 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
    [Show full text]
  • 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.
    [Show full text]
  • Flood Risk Management Plan for the Danube River Basin District Is Based on Information Received from the ICPDR Contracting Parties by 10 November 2015
    / / / / / / / / / / / / / н ϊ ρ κ Y Flood Risk / / / / a v o Management Plan d l uj //// Crna o pб Gor M // C a //// / // Ro // a mân я / in ia //// ρu for the Danube River Basin District Бълѕѕ v o g e c r e H i a n nd //// Ös s schla terreic o ut h //// B e Č / D esk // // á r / / ep a // ub / lik k / a / s / /// t / a / Sl v / ov r / en / sk H / o / / / /// / M // agyar ija н ors n ϊ zág //// Slove ρ κ Y / / / / a v o d l o M / / / / я u ρ ѕ л ъ Б / / / / a i n â m o R / / / / a r o G a n agyarorsz r /// M ág //// C / S ko lov / s en / n ija / e //// / ov H Sl rva j // tska u // //// б ka Bosn Cp bli a i H //// pu ercegovina re ská / Če h /// rreic / Öste land /// ////// eutsch D Disclaimer This Flood Risk Management Plan for the Danube River Basin District is based on information received from the ICPDR Contracting Parties by 10 November 2015. Sources other than the competent authorities have been clearly identified in the Plan. A more detailed level of information is presented in the national Flood Risk Management Plans. Hence, the Flood Risk Management Plan for the Danube River Basin District should be read and interpreted in conjunction with the national Flood Risk Management Plans. The data in this report has been dealt with, and is presented, to the best of our knowledge. Nevertheless inconsistencies cannot be ruled out.
    [Show full text]
  • Neolithisation of Sava-Drava-Danube Interfluve at the End of the 6600–6000 BC Period of Rapid Climate Change> a New Solutio
    Documenta Praehistorica XLIII (2016) Neolithisation of Sava-Drava-Danube interfluve at the end of the 6600–6000 BC period of Rapid Climate Change> a new solution to an old problem Katarina Botic´ Institute of Archaeology, Zagreb, CR [email protected] ABSTRACT – The idea of the Neolithisation of the Sava-Drava-Danube interfluve has undergone very little change since S. Dimitrijevi≤'s time. Despite their many shortcomings, new archaeological exca- vations and radiocarbon dates of Early Neolithic sites have provided us with new insight into the process of Neolihisation of this region. Using the recently published work by B. Weninger and L. Clare (Clare, Weninger 2010; Weninger et al. 2009; Weninger et al. 2014) as a starting point, the available radiocarbon and archaeological data are used to build up a time frame comparable to the wider region of Southeast Europe and climate conditions for specific period. The results fit the model of Neolithisation well (Weninger et al. 2014.9, Fig. 4), filling in the geographical gaps. IZVLE∞EK – Premise o neolitizaciji v medre≠ju Save, Drave in Donave se od ≠asa S. Dimitrijevi≤a niso veliko spremenile. Nova arheolo∏ka izkopavanja in radiokarbonski datumi zgodnjega neolitika so, kljub mnogim pomanjkljivostim, prinesli nove vpoglede v proces neolitizacije na tem obmo≠ju. Za os- novo pri interpretaciji smo uporabili nedavno objavljena dela B. Weningerja in L. Clarea (Clare, We- ninger 2010; Weninger et al. 2009; Weninger et al. 2014), dosegljive radiokarbonske datume in arheo- lo∏ke podatke pa smo uporabili za izdelavo ≠asovnega okvirja, ki je primerljiv s ∏ir∏im obmo≠jem ju- govzhodne Evrope in s klimatskimi pogoji za posamezna obdobja.
    [Show full text]
  • Download This Article in PDF Format
    Knowl. Manag. Aquat. Ecosyst. 2021, 422, 13 Knowledge & © L. Raguž et al., Published by EDP Sciences 2021 Management of Aquatic https://doi.org/10.1051/kmae/2021011 Ecosystems Journal fully supported by Office www.kmae-journal.org français de la biodiversité RESEARCH PAPER First look into the evolutionary history, phylogeographic and population genetic structure of the Danube barbel in Croatia Lucija Raguž1,*, Ivana Buj1, Zoran Marčić1, Vatroslav Veble1, Lucija Ivić1, Davor Zanella1, Sven Horvatić1, Perica Mustafić1, Marko Ćaleta2 and Marija Sabolić3 1 Department of Biology, Faculty of Science, University of Zagreb, Rooseveltov trg 6, Zagreb 10000, Croatia 2 Faculty of Teacher Education, University of Zagreb, Savska cesta 77, Zagreb 10000, Croatia 3 Institute for Environment and Nature, Ministry of Economy and Sustainable Development, Radnička cesta 80, Zagreb 10000, Croatia Received: 19 November 2020 / Accepted: 17 February 2021 Abstract – The Danube barbel, Barbus balcanicus is small rheophilic freshwater fish, belonging to the genus Barbus which includes 23 species native to Europe. In Croatian watercourses, three members of the genus Barbus are found, B. balcanicus, B. barbus and B. plebejus, each occupying a specific ecological niche. This study examined cytochrome b (cyt b), a common genetic marker used to describe the structure and origin of fish populations to perform a phylogenetic reconstruction of the Danube barbel. Two methods of phylogenetic inference were used: maximum parsimony (MP) and maximum likelihood (ML), which yielded well supported trees of similar topology. The Median joining network (MJ) was generated and corroborated to show the divergence of three lineages of Barbus balcanicus on the Balkan Peninsula: Croatian, Serbian and Macedonian lineages that separated at the beginning of the Pleistocene.
    [Show full text]
  • 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.
    [Show full text]
  • World Bank Document
    work in progress for public discussion Public Disclosure Authorized Water Resources Management in South Eastern Public Disclosure Authorized Europe Volume II Country Water Notes and Public Disclosure Authorized Water Fact Sheets Environmentally and Socially Public Disclosure Authorized Sustainable Development Department Europe and Central Asia Region 2003 The International Bank for Reconstruction and Development / The World Bank 1818 H Street, N.W., Washington, DC 20433, USA Manufactured in the United States of America First Printing April 2003 This publication is in two volumes: (a) Volume 1—Water Resources Management in South Eastern Europe: Issues and Directions; and (b) the present Volume 2— Country Water Notes and Water Fact Sheets. The Environmentally and Socially Sustainable Development (ECSSD) Department is distributing this report to disseminate findings of work-in-progress and to encourage debate, feedback and exchange of ideas on important issues in the South Eastern Europe region. The report carries the names of the authors and should be used and cited accordingly. The findings, interpretations and conclusions are the authors’ own and should not be attributed to the World Bank, its Board of Directors, its management, or any member countries. For submission of comments and suggestions, and additional information, including copies of this report, please contact Ms. Rita Cestti at: 1818 H Street N.W. Washington, DC 20433, USA Email: [email protected] Tel: (1-202) 473-3473 Fax: (1-202) 614-0698 Printed on Recycled Paper Contents
    [Show full text]
  • 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.
    [Show full text]