Geothermics of the Pannonian Basin and Its Bearing on the Neotectonics
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Analysis of Sub-Daily Precipitation for the Pannex Region
atmosphere Article Analysis of Sub-Daily Precipitation for the PannEx Region Monika Lakatos 1,*, Olivér Szentes 1, Ksenija Cindri´cKalin 2, Irena Nimac 2, Katja Kozjek 3, Sorin Cheval 4 , 4 4 5,6 5 7 7 Alexandru Dumitrescu , Adrian Iras, oc , Petr Stepanek , Aleš Farda , Peter Kajaba , Katarína Mikulová , Dragan Mihic 8, Predrag Petrovic 8, Barbara Chimani 9 and David Pritchard 10 1 Hungarian Meteorological Service, 1024 Budapest, Hungary; [email protected] 2 Croatian Meteorological and Hydrological Service, 10000 Zagreb, Croatia; [email protected] (K.C.K.); [email protected] (I.N.) 3 Slovenian Environment Agency, 1000 Ljubljana, Slovenia; [email protected] 4 National Meteorological Administration, 013686 Bucharest, Romania; [email protected] (S.C.); [email protected] (A.D.); [email protected] (A.I.) 5 Global Change Research Institute, Czech Academy of Sciences, 603 00 Brno, Czech Republic; [email protected] (P.S.); [email protected] (A.F.) 6 Czech Hydrometeorological Institute, 616 67 Brno, Czech Republic 7 Slovak Hydrometeorological Institute, 833 15 Bratislava, Slovakia; [email protected] (P.K.); [email protected] (K.M.) 8 Republic Hydrometeorological Service of Serbia, 11030 Beograd, Serbia; [email protected] (D.M.); [email protected] (P.P.) 9 Zentralanstalt für Meteorologie und Geodynamik, 1190 Wien, Austria; [email protected] 10 School of Engineering, Newcastle University, Newcastle upon Tyne NE1 7RU, UK; [email protected] * Correspondence: [email protected]; Tel.: +36-1-346-4725 Citation: Lakatos, M.; Szentes, O.; Abstract: The PannEx is a GEWEX-initiated, community driven research network in the Pannonian Cindri´cKalin, K.; Nimac, I.; Kozjek, Basin. -
Arsenic- Water in Vojvodina 2010..Pdf
This article appeared in a journal published by Elsevier. The attached copy is furnished to the author for internal non-commercial research and education use, including for instruction at the authors institution and sharing with colleagues. Other uses, including reproduction and distribution, or selling or licensing copies, or posting to personal, institutional or third party websites are prohibited. In most cases authors are permitted to post their version of the article (e.g. in Word or Tex form) to their personal website or institutional repository. Authors requiring further information regarding Elsevier’s archiving and manuscript policies are encouraged to visit: http://www.elsevier.com/copyright Author's personal copy Environmental Research 111 (2011) 315–318 Contents lists available at ScienceDirect Environmental Research journal homepage: www.elsevier.com/locate/envres Reports from the Field Arsenic occurrence in drinking water supply systems in ten municipalities in Vojvodina Region, Serbia$ Dragana Jovanovic a,n, Branko Jakovljevic´ b, Zorica Rasicˇ ´-Milutinovic´ c, Katarina Paunovic´ b, Gordana Pekovic´ c, Tanja Knezevic´ a a Institute of Public Health of Serbia ‘‘Dr Milan Jovanovic Batut’’, Dr Subotica 5, Belgrade, Serbia b Institute of Hygiene and Medical Ecology, School of Medicine, Belgrade, Serbia c Department of Endocrinology, University Hospital Zemun, Belgrade, Serbia article info abstract Article history: Vojvodina, a northern region of Serbia, belongs to the Pannonian Basin, whose aquifers contain high Received 9 August 2010 concentrations of arsenic. This study represents arsenic levels in drinking water in ten municipalities in Received in revised form Serbia. Around 63% of all water samples exceeded Serbian and European standards for arsenic in drinking 15 November 2010 water. -
Evolution of the Pannonian Basin and Its Geothermal Resources
Geothermics 53 (2015) 328–352 Contents lists available at ScienceDirect Geothermics jo urnal homepage: www.elsevier.com/locate/geothermics Invited Review Evolution of the Pannonian basin and its geothermal resources a,b a,∗ b,f d e c a F. Horváth , B. Musitz , A. Balázs , A. Végh , A. Uhrin , A. Nádor , B. Koroknai , d a a N. Pap , T. Tóth , G. Wórum a Geomega Ltd., Mester u. 4, H-1095 Budapest, Hungary b Department of Geophysics and Space Sciences, Eötvös Loránd University, Pázmány Péter st. 1/c, H-1117 Budapest, Hungary c Geological and Geophysical Institute of Hungary, Stefánia út 14, H-1442 Budapest, Hungary d Department of Political Geography and Regional Development, University of Pécs, Vasvári Pál u. 4., H-7622 Pécs, Hungary e Eriksfiord AS, Prof. Olav Hanssens vei 7A, Ipark, N-4021 Stavanger, Norway f Utrecht University, Faculty of Geosciences, Utrecht, The Netherlands a r t i c l e i n f o a b s t r a c t Article history: The Pannonian basin is an integral part of the convergence zone between the Eurasian and Nubian plates Received 25 March 2013 characterized by active subductions of oceanic and continental plates, and formation of backarc basins. Accepted 18 July 2014 The first part of this paper presents an overview of the evolution of the Alpine-Mediterranean region in order to understand the large scale crustal and upper mantle processes in and around the Pannonian basin, Keywords: resulting a collage of terranes of Alpine and Adriatic origin. It will be followed by a summary of the history Pannonian basin of sedimentation, volcanism and tectonic activity. -
Urban Climate Monitoring System Suitability for Intra-Urban Thermal Comfort Observations in Novi Sad (Serbia) – with 2014 Ex
ICUC9 - 9th International Conference on Urban Climate jointly with 12th Symposium on the Urban Environment Urban climate monitoring system suitability for intra-urban thermal comfort observations in Novi Sad (Serbia) – with 2014 examples Dragan D. Milošević Dragan D. Milošević1, Stevan M. Savić1, János Unger2, Tamás Gál2 1 Climatology and Hydrology Research Centre, Faculty of Science, University of Novi Sad, Trg Dositeja Obradovića 3, 21000 Novi Sad, Serbia, [email protected], [email protected] 2 Department of Climatology and Landscape Ecology, University of Szeged, P.O. Box 653, 6701 Szeged, Hungary, [email protected], [email protected] dated: 12 June 2015 Abstract In 2014, urban climate monitoring systems were established in two neighboring European cities (Novi Sad, Serbia; Szeged, Hungary) based on Local Climate Zones (LCZ) classification system, GIS model calculations and fieldwork. Seven built LCZ types in the built-up area of Novi Sad (112 km2) and two LCZ land cover types in nonurban environment in the vicinity of the city were delineated. Urban climate monitoring system in Novi Sad consists of 27 stations equipped with air temperature and relative humidity sensors distributed across all LCZs. This system provided 10-minute measured air temperature and relative humidity data since June 2014. Human comfort observations in different LCZs of the city and its surroundings were investigated for warmest (tropical) and coldest (icy) day in 2014 in Novi Sad. Thermal comfort was assessed with the application of the Physiologically Equivalent Temperature (PET) thermal index. Differences in PET index amongst LCZs can be as high as 10-12 ºC during nocturnal hours when comparing built-up areas of the city (e. -
Evaluation of Wetlands and Floodplain Areas in the Danube River Basin Final Report May 1999
DANUBE POLLUTION REDUCTION PROGRAMME EVALUATION OF WETLANDS AND FLOODPLAIN AREAS IN THE DANUBE RIVER BASIN FINAL REPORT MAY 1999 Programme Coordination Unit UNDP/GEF Assistance prepared by WWF Danube-Carpathian-Programme and WWF-Auen-Institut (Germany) DANUBE POLLUTION REDUCTION PROGRAMME EVALUATION OF WETLANDS AND FLOODPLAIN AREAS IN THE DANUBE RIVER BASIN FINAL REPORT MAY 1999 Programme Coordination Unit UNDP/GEF Assistance prepared by WWF Danube-Carpathian-Programme and WWF-Auen-Institut (Germany) Preface The "Evaluation of Wetlands and Flkoodplain Areas in the Danube River Basin" study was prepared in the frame of the Danube Pollution Reduction Programme (PRP). The Study has been undertaken to define priority wetland and floodplain rehabilitation sites as a component of the Pollution reduction Programme. The present report addresses the identification of former floodplains and wetlands in the Danube River Basin, as well as the description of the current status and evaluation of the ecological importance of the potential for rehabilitation. Based on this evaluation, 17 wetland/floodplain sites have been identified for rehabilitation considering their ecological importance, their nutrient removal capacity and their role in flood protection. Most of the identified wetlands will require transboundary cooperation and represent an important first step in retoring the ecological balance in the Danube River Basin. The results are presented in the form of thematic maps that can be found in Annex I of the study. The study was prepared by the WWF-Danube-Carpathian-Programme and the WWF-Auen-Institut (Institute for Floodplains Ecology, WWF-Germany), under the guidance of the UNDP/GEF team of experts of the Danube Programme Coordination Unit (DPCU) in Vienna, Austria. -
Pannex, a GEWEX Regional Hydroclimate Project (RHP) Over the Pannonian Basin
PannEx, A GEWEX Regional Hydroclimate project (RHP) over the Pannonian Basin White Book J anuary 2019 WCRP Publication No.: 03/2019 Bibliographic information This report should be cited as: PannEx White Book, A GEWEX Regional Hydroclimate Project (RHP) over the Pannonian Basin (2019). WCRP Report 3/2019, World Climate Research Programme (WCRP): Geneva, Switzerland, 108 pp. Contact information All enquiries regarding this report should be directed to [email protected] or: World Climate Research Programme c/o World Meteorological Organization 7 bis, Avenue de la Paix Case Postale 2300 CH-1211 Geneva 2 Switzerland Cover image credit Cover page image courtesy of Katarina Stefanović Copyright notice This report is published by the World Climate Research Programme (WCRP) under a Creative Commons Attribution 3.0 IGO License (CC BY 3.0 IGO, www.creativecommons.org/licenses/by/3.0/igo) and thereunder made available for reuse for any purpose, subject to the license’s terms, including proper attribution. Authorship and publisher’s notice PannEx (the Pannonian Basin Experiment) is a Regional Hydroclimate Project (RHP) of the Global Energy and Water Exchanges project (GEWEX) Hydroclimatology Panel (GHP) which aims to achieve a better understanding of the Earth system components and their interactions in the Pannonian Basin. The international efforts in PannEx provide scientific support and involve the international research community in an integrated approach towards identifying and increasing adaptation capacity in the face of climate change in the Pannonian Basin. The WCRP Core Project on Global Energy and Water Exchanges (GEWEX) is an integrated program of research, observations, and science activities that focuses on the atmospheric, terrestrial, radiative, hydrological, coupled processes, and interactions that determine the global and regional hydrological cycle, radiation and energy transitions and their involvement in global changes. -
Potentials of Renewable Energy Sources in the Republic of Serbia
POTENTIALS OF RENEWABLE ENERGY SOURCES IN THE REPUBLIC OF SERBIA WITH A DETAILED REVIEW OF THE EXPLOITATION OF GEOTHERMAL RESOURCES IN THE AUTONOMOUS PROVINCE OF VOJVODINA Zoran Stipi ć City of Subotica Urban Planning Institute, Trg Republike 16, Subotica, Serbia [email protected] Slobodan Vidovi ć Tehnoproing , Gogoljeva 13,Novi Sad, Serbia, [email protected] Mom čilo Spasojevi ć Faculty of Technical Sciences, Trg D.Obradovi ća 6, Novi Sad, Serbia, [email protected] Abstract: Energy supply is one of the basic issues in the contemporary world’s sustainable development. By adopting the Kyoto Protocol and implementing its mechanisms, it is expected that the use of conventional energy sources shall stabilise and decrease on global level. The European Union’s legal framework, through its appropriate directives, sets very clear objectives for the use of renewable energy sources for member states. Serbia is a country with significant potentials in renewable energy sources, which are, regretfully, underused. Renewable energy source potentials are featured by very favourable indicators in matters of both capacity and distribution. The status is especially favourable in the field of geothermal energy potentials in the Autonomous Province of Vojvodina, situated in the Pannonian Basin, where there are significant sources of this fuel. The paper presents the basic forms and characteristics of renewable energy sources in Serbia and provides an overview of the possibilities for their use. Key words: Renewable energy sources, potentials, capacities, resources, geothermal energy, Serbia, Vojvodina. 1. INTRODUCTION Solving global energy problems implies an interdisciplinary approach and considering the issues from different perspectives. Decreasing overall energy consumption, increasing energy efficiency, modernising the installation, using alternative energy sources and adopting and implementing a number of legal regulations and international covenants are the points of departure in solving this exceptionally complex issue. -
Seismic Stratigraphy Based Chronostratigraphy (SSBC) of the Serbian Banat Region of the Pannonian Basin
Cent. Eur. J. Geosci. • 2(4) • 2010 • 481-500 DOI: 10.2478/v10085-010-0027-2 Central European Journal of Geosciences Seismic Stratigraphy Based Chronostratigraphy (SSBC) of the Serbian Banat Region of the Pannonian Basin Research Article John D. Pigott∗1, Dejan Radivojeviㆠ2 1 University of Oklahoma, ConocoPhillips School of Geology and Geophysics, 100 East Boyd, Norman, Oklahoma 73019 USA 2 NIS Naftagas, Narodnog fronta 12, 21000 Novi Sad, Serbia Received 17 May 2010; accepted 29 August 2010 Abstract: Seismic stratigraphy based chronostratigraphic (SSBC) analysis of the Serbian Banat region allows the delin- eation of the spatial and stratigraphic relationships of the generally regressive and shallowing upward Neogene depositional fill of a tectonically unstable central portion of the Pannonian Basin. When geometrically restored in time and space, the sediment dispersal directions, sediment source directions, types of sedimentation breaks and the tectonic events influencing basin evolution can be delineated. For such an analysis the time- transgressive lithostratigraphic units used in the neighbouring Hungarian part of the Pannonian Basin are conveniently introduced based upon their characteristic seismic facies and constrained borehole log records as mappable seismic stratigraphic sequence units, termed ”seismic operational sequences”. The respective Neogene stage and operational sequence equivalents (Hungarian lithostratigraphic units or formations) are the Middle Miocene (Badenian, Sarmatian), Upper Miocene-Lower Pliocene (Pannonian-Endrod and Szolnok Formations; Pontian- Algyo and Ujfalu Formations and Lower Pliocene- Zagyva Formation) and Upper Pliocene- Quaternary (Nagyalfold Formation). SSBC analysis greatly assists in the geological constraint or ”geovalidation” of interpreted seismic stratigraphic relationships and provides potentially critical insight into stratigraphic and structural problems of non-unique interpretations. -
Analysis of the Transdanubian Region of Hungary According to Plant Species Diversity and Floristic Geoelement Categories
FOLIA OECOLOGICA – vol. 44, no. 1 (2017), doi: 10.1515/foecol-2017-0001 Review article Analysis of the Transdanubian region of Hungary according to plant species diversity and floristic geoelement categories Dénes Bartha1*†, Viktor Tiborcz1* *Authors with equal contribution 1Department of Botany and Nature Conservation, Faculty of Forestry, University of West Hungary, H-9400 Sopron, Bajcsy-Zsilinszky 4, Hungary Abstract Bartha, D., Tiborcz, V., 2017. Analysis of the Transdanubian region of Hungary according to plant species diversity and floristic geoelement categories.Folia Oecologica, 44: 1–10. The aim of this study was to describe the proportion of floristic geoelements and plant biodiversity in the macroregions of Transdanubia. The core data source used for the analysis was the database of the Hungar- ian Flora Mapping Programme. The analysed data were summarized in tables and distribution maps. The percentage of continental elements was higher in dry areas, whereas the proportion of circumboreal elements was higher in humid and rainy parts of Transdanubia. According to the climatic zones, the highest value of continental geoelement group occurred in the forest-steppe zone. The plant species diversity and geoele- ments were analysed also on a lower scale, with Transdanubia specified into five macroregions. The highest diversity values were found in the Transdanubian Mountain and West-Transdanubian regions because of the climatic, topographic, and habitat diversity. Keywords Borhidi’s climatic zones, climatic variables, floristic geoelement categories, macroregion, species diversity, Transdanubia Introduction Hungary is influenced by many different environmental In some European countries, floristic assessments conditions which are also reflected in the floristic diver- have already been made based on published flora at- sity. -
Research Article
kj8 z Available online at http://www.journalcra.com INTERNATIONAL JOURNAL OF CURRENT RESEARCH International Journal of Current Research Vol. 11, Issue, 05, pp.3546-3552, May, 2019 DOI: https://doi.org/10.24941/ijcr.34579.05.2019 ISSN: 0975-833X RESEARCH ARTICLE THE CAVE OPENING TYPES OF THE BAKONY REGION (TRANSDANUBIAN MOUNTAINS, HUNGARY) *Márton Veress and Szilárd Vetési-Foith Department of Physical and Geography, University of Pécs, Pécs, Hungary ARTICLE INFO ABSTRACT Article History: The genetic classification of the cave openings in the Bakony Region is described. The applied Received 09th February, 2019 methods are the following: studying the relation between the distribution of phreatic caves and the Received in revised form quality of the host rock and in case of antecedent valley sections, making theoretical geological 12th March, 2019 longitudinal profiles. The phreatic caves developed at the margins of the buried karst terrains of the th Accepted 15 April, 2019 mountains. The streams of these terrains created epigenetic valleys, while their seeping waters created th Published online 30 May, 2019 karst water storeys over the local impermeable beds. Cavity formation took place in the karst water storeys. Phreatic cavities also developed in the main karst water of the mountains. The caves are Key Words: primarily of valley side position, but they may occur on the roof or in the side of blocks. The cavities Gorge, Phreatic Cave, of valley side position were opened up by the streams downcutting the carboniferous rocks (these are Development of Cave openings. the present caves of the gorges). While cavities of block roof position developed at the karst water storey at the mound of the block. -
Background and Introduction
Chapter One: Background and Introduction Chapter One Background and Introduction title chapter page 17 © Libor Vojtíšek, Ján Lacika, Jan W. Jongepier, Florentina Pop CHAPTER?INDD Chapter One: Background and Introduction he Carpathian Mountains encompass Their total length of 1,500 km is greater than that many unique landscapes, and natural and of the Alps at 1,000 km, the Dinaric Alps at 800 Tcultural sites, in an expression of both km and the Pyrenees at 500 km (Dragomirescu geographical diversity and a distinctive regional 1987). The Carpathians’ average altitude, how- evolution of human-environment relations over ever, of approximately 850 m. is lower compared time. In this KEO Report, the “Carpathian to 1,350 m. in the Alps. The northwestern and Region” is defined as the Carpathian Mountains southern parts, with heights over 2,000 m., are and their surrounding areas. The box below the highest and most massive, reaching their offers a full explanation of the different delimi- greatest elevation at Slovakia’s Gerlachovsky tations or boundaries of the Carpathian Mountain Peak (2,655 m.). region and how the chain itself and surrounding areas relate to each other. Stretching like an arc across Central Europe, they span seven countries starting from the The Carpathian Mountains are the largest, Czech Republic in the northwest, then running longest and most twisted and fragmented moun- east and southwards through Slovakia, Poland, tain chain in Europe. Their total surface area is Hungary, Ukraine and Romania, and finally 161,805 sq km1, far greater than that of the Alps Serbia in the Carpathians’ extreme southern at 140,000 sq km. -
Miocene Depositional Systems and Sequence Stratigraphy of the Vienna Basin
Cour. Forsch.-Inst. Senckenberg 246 187–212 13 Figs, 1 Tab. Frankfurt a. M., 07. 04. 2004 Miocene depositional systems and sequence stratigraphy of the Vienna Basin With 13 fi gs, 1 tab. Michal KOVÁČ, Ivan BARÁTH, Mathias HARZHAUSER, Ivan HLAVATÝ & Natália HUDÁČKOVÁ Abstract The Vienna Basin, depositional systems of alluvial plains, deltas, littoral and neritic areas have been characterized to recognize the development of aquatic and terrestrial environments during the paleogeo- graphic evolution of the basin. Their mutual interrelationship was discussed to be triggered by sea-level changes. Based on evaluation of the sedimentary environments, the possibilities of creating an accommoda- tion space by tectonic subsidence, as well as the basin fi ll by increased input of clastics by deltas it can be stated that only partial comparison between global and regional sea-level changes is possible in the Miocene. Nine third-order cycles of relative sea-level changes are proposed for the Miocene of the Vienna Basin. These cycles, termed VB1 to VB 9, resulted from combination of eustatic global sea-level changes, tectonic evolution of the basin and sediment supply mostly by deltas in this area. Some of these cycles correspond fairly to regional chronostratigraphic stages, whilst others, such as VB 5–7 cycles, follow other criteria. Key words: Vienna Basin, Miocene, depositional systems, sequence stratigraphy Zusammenfassung Die paläogeographische Entwicklung des Wiener Beckens bedingte die Bildung einer großen Vielfalt aquatischer und terrestrischer Lebensräume. Diese spiegeln sich in den miozänen Ablagerungssyste- men wider, die von Flusslandschaften und Deltas über Küstenbereiche bis zu offen marinen, neritischen Becken bedingungen reichen.