Successful Red Deer Management in Southern Transdanubia and Its Physico-Geographical Background
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IDŐJÁRÁS Quarterly Journal of the Hungarian Meteorological Service Vol
IDŐJÁRÁS Quarterly Journal of the Hungarian Meteorological Service Vol. 117, No. 2, April – June, 2013, pp. 219–237 Projected changes in the drought hazard in Hungary due to climate change Viktória Blanka1*, Gábor Mezősi1*, and Burghard Meyer2 1University of Szeged, Egyetem u. 2-6. H-6722 Szeged, Hungary 2Universität Leipzig, Ritterstraße 26. DE-04109 Leipzig, Germany *Corresponding authors E-mails: [email protected], [email protected] (Manuscript received in final form December 18, 2012) Abstract–In the Carpathian Basin, drought is a severe natural hazard that causes extensive damage. Over the next century, drought is likely to remain one of the most serious natural hazards in the region. Motivated by this hazard, the analysis presented in this paper outlines the spatial and temporal changes of the drought hazard through the end of this century using the REMO and ALADIN regional climate model simulations. The aim of this study was to indicate the magnitude of the drought hazard and the potentially vulnerable areas for the periods 2021–2050 and 2071–2100, assuming the A1B emission scenario. The magnitude of drought hazard was calculated by aridity (De Martonne) and drought indices (Pálfai drought index, standardised anomaly index). By highlighting critical drought hazard areas, the analysis can be applied in spatial planning to create more optimal land and water management to eliminate the increasing drought hazard and the related wind erosion hazard. During the 21st century, the drought hazard is expected to increase in a spatially heterogeneous manner due to climate change. On the basis of temperature and precipitation data, the largest increase in the drought hazard by the end of the 21st century is simulated to occur in the Great Hungarian Plain. -
A Tanulni Vágyók Soha El Nem Múló Tudásszomjának Csillapítására Az Úr És Az Internet Segedelmével Összeállította: Kiss Attila
IV. BÉLA ÁLTALÁNOS ISKOLA ÉS ÓVODA 7012 ALSÓSZENTIVÁN, BÉKE ÚT 112. Tel.:(25) / 504-710; fax: (25) / 504-711;. OM: 030 149 e-mail: [email protected] Intézményünk COMENIUS 2000 alapú minőségirányítási rendszert működtet. Az év végi vizsga szóbeli témakörei FÖLDRAJZ A tanulni vágyók soha el nem múló tudásszomjának csillapítására az Úr és az Internet segedelmével összeállította: Kiss Attila Alsószentiván, 2008. 1. MAGYARORSZÁG FÖLDRAJZI HELYZETE 1. Helyünk a földgömbön a) az Egyenlítőtől északra az északi félgömb országa b) a kezdő 0. hosszúsági körtől keletre a keleti félgömbön található c) a Ráktérítő és az Északi-sarkkör között az északi mérsékelt övben fekszik d) földrészünk: Európa 2. Helyünk Európában a) Európa központi országa Közép-Európa országai közé tartozik. b) Közép-Európán belül gazdasági-társadalmi fejlettsége miatt Kelet-Közép- Európába sorolják hazánkat. c) A Kárpátok gyűrűjében terül el a Kárpát-medence országa d) a Duna középső szakasza mentén fekszik a Közép-Duna-medencében található 3. Szomszédos országok Irány Ország Főváros É Szlovákia Pozsony (Bratislava) ÉK Ukrajna Kijev (Kiev) K Románia Bukarest (Bucuresti) D Szerbia Belgrád (Beograd) D-DNY Horvátország Zágráb (Zagreb) DNY Szlovénia Ljubljana NY Ausztria Bécs (Wien) 4. Magyarország általános adatai Területe: 93 000 km2 Lakossága: 10 millió fő Fővárosa: Budapest A főváros lakossága: 1.8 millió fő Államformája: köztársaság Államnév: Magyar Köztársaság Köztársasági elnök: Miniszterelnök: Éghajlata: nedves kontinentális Évi középhőmérséklet: 10-11 C Évi csapadék: 500 – 800 mm Uralkodó szélirány: ÉNY – NY 2. MAGYARORSZÁG FÖLDTÖRTÉNETE 1. Óidő: (580–240 millió éve) A Föld kora 4600 millió év. Hazánk legrégibb kőzete alig 1000 millió éves, az is mélyen a felszín alatt van hazánk területe az eddigi ismereteink szerint nem tartozott az ősidőben keletkezett területek közé. -
Dr. Jenő PAPP's Curriculum Vitae
Dr. Jenő PAPP’s Curriculum Vitae Born 20 May 1933 in Budapest. Mother’s maiden name: Ibolya Marcsekényi, primary school teacher, deceased 1969. Father dr. Ágoston Papp, paediatrist, deceased 1960. His highest qualification is university, graduated as certified zoologist at the Lorand Eötvös University, Budapest 1951–1956. Obtained university doctorate 1962. Earned the academic honour Candidate of Biological Science (=PhD) 1976. Title of his dissertation: “Evolutionary trends of the braconid species Apanteles and their significance in the biological control”, 233 pages + 78 figures. In an academic public debate acquired the honorary Doctor of the Hungarian Academy of Sciences (biology). Title of the doctorate dissertation “Taxonomical, systematical, zoogeographical and applied entomological studies on braconid wasps”, 117 pages. Married twice: first wife Irma Kolep, librarian (deceased 2008), by whom he has two adult children, Zsófia (1962) and Jenő (1964). Second wife Ágnes Árpási, retired secondary school teacher. Job experience –– From 3 April to 30 September 1956 trainee journalist for weekly “Élet és Tudomány” (=Life and Science). 1 October 1956 moves to Bakony Museum, Veszprém, and assumes assistant museologist’s post; from this time on keeps serving the cause of Hungarian museology. From 1962 museologist in the staff of the Directorate of County Museum Veszprém and from 1967 holds the position of deputy director of the County Museum Veszprém, simultaneously appointed as principal research fellow. Employment at the Directorate terminated 31 December 1969. 1 January 1970 transferred to the Department of Zoology, Hungarian Natural History Museum, Budapest, and put in curatorship of the Hymenoptera Section and appointed as principal research worker (senior entomologist). -
MAGYARORSZÁG Névanyaga
MAGYARORSZÁG névanyaga Domborzat, vízrajz Alföld: Mezőföld, Duna–Tisza köze, Kiskunság, Bácska, Duna-mellék, Pesti-síkság, Solti-síkság, Sárköz, Csepel-sziget, Mohácsi-sziget, Tiszántúl, Nyírség, Hajdúság, Maros-Körös köze, Körös- vidék, Szatmári-síkság, Hortobágy, Nagykunság, Tiszazug, Bodrogköz, Jászság, Dráva-mellék (Dráva menti síkság) Kisalföld: Győri-medence, Szigetköz, Mosoni-síkság, Rábaköz, Fertő–Hanság-medence, Marcal- medence (Somló 432 m) Alpokalja (Nyugat-magyarországi-peremvidék): Soproni-hegység, Kőszegi-hegység (Írott-kő 882 m), Vasi-hegyhát, Kemeneshát, Őrség Dunántúli-dombság (Dunántúli-domb- és hegyvidék): Zalai-dombság, Somogyi-dombság Î Belső-Somogy, Külső-Somogy, Tolnai-hegyhát, Szekszárdi-dombság, Mecsek (Zengő 680 m), Baranyai-dombság, Villányi-hegység Dunántúli-középhegység: Bakony Î Északi-Bakony (Kőris-hegy 709 m) és Déli-Bakony (Kab- hegy 599 m), Keszthelyi-hegység, Tapolcai-medence, Badacsony, Szt. György-hegy, Balaton- felvidék, Tihanyi-félsziget, Bakonyalja, Sokoró, Móri-árok, Vértes (Nagy-Csákány 487 m), Zámolyi-medence, Velencei-hegység, Tatai-árok, Gerecse (633 m), Dunazug-hegység, Zsámbéki- medence, Dunakanyar, Visegrádi-hegység (Dobogó-kő 699 m), Pilis (757 m), Szentendrei-sziget, Budai-hegység *(Hármashatár-hegy, Szabadság-hegy, Nagy-Kopasz), Tétényi-fennsík Északi-középhegység: Börzsöny (Csóványos 939 m), Nógrádi-medence, Cserhát (Naszály 652 m), Gödöllői-dombság, Mátra (Kékes 1014 m, Galya-tető 964 m), Mátraalja, Bükk (Istállós-kő 958 m), Bükk-fennsík, Bükkalja, Borsodi-medence, Aggteleki-karszt, -
Modelling the Impacts of Climate Change on Shallow Groundwater Conditions in Hungary
water Article Modelling the Impacts of Climate Change on Shallow Groundwater Conditions in Hungary Attila Kovács 1,* and András Jakab 2 1 Department of Engineering Geology and Geotechnics, Budapest University of Technology and Economics, M˝uegyetemrkp. 1, 1111 Budapest, Hungary 2 Jakab és Társai Kft., 32 Jászóvár utca, 2100 Gödöll˝o,Hungary; [email protected] * Correspondence: [email protected] Abstract: The purpose of the present study was to develop a methodology for the evaluation of direct climate impacts on shallow groundwater resources and its country-scale application in Hungary. A modular methodology was applied. It comprised the definition of climate zones and recharge zones, recharge calculation by hydrological models, and the numerical modelling of the groundwater table. Projections of regional climate models for three different time intervals were applied for the simulation of predictive scenarios. The investigated regional climate model projections predict rising annual average temperature and generally dropping annual rainfall rates throughout the following decades. Based on predictive modelling, recharge rates and groundwater levels are expected to drop in elevated geographic areas such as the Alpokalja, the Eastern parts of the Transdanubian Mountains, the Mecsek, and Northern Mountain Ranges. Less significant groundwater level drops are predicted in foothill areas, and across the Western part of the Tiszántúl, the Duna-Tisza Interfluve, and the Szigetköz areas. Slightly increasing recharge and groundwater levels are predicted in the Transdanubian Hills and the Western part of the Transdanubian Mountains. Simulation results Citation: Kovács, A.; Jakab, A. represent groundwater conditions at the country scale. However, the applied methodology is suitable Modelling the Impacts of Climate for simulating climate change impacts at various scales. -
Hungarian Geographical Names in English Language Publications
HUNGARIAN GEOGRAPHICAL NAMES IN ENGLISH LANGUAGE PUBLICATIONS GÁBOR GERCSÁK Összefoglalás A magyar természetföldrajzi nevek az angol nyelvû szakirodalomban és népszerûsítõ kiadványokban rendkívül sokféle alakban fordulnak elõ. A magyar földrajzinév-írás sokat foglalkozott az idegen nyelvû földrajzi nevek magyar átírásával, de még nem kapott kellõ figyelmet, hogyan szerepeljenek a magyar földrajzi nevek az egyre szaporodó angol nyelvû kiadványokban, így térképeken, ábrákon, útikönyvben, geológiai, földrajzi és régészeti munkákban. Sokszor zavaró, félrevezetõ, ha az olvasó ugyanannak a tájnak több angol nyelvû változatával talákozik, esetenként egyazon könyvben, vagy nem tudja az eredeti magyar alakot visszakeresni. Ez a dolgozat a magyarországi természetföldrajzi nevek angol nyelvû használatát tekinti át, és javaslatot ad az egységes használatra. This paper forms part of an extensive study on the geographical names of present Hungary. Probably, this is the first attempt to introduce the English language readers to some of the practical questions of using the English translation of Hungarian toponyms in maps and publications. (The use of Hungarian street and other public area names as well as administrative units and institution names etc. in English is not discussed here.) In Hungary, there is a rich literature of writing foreign geographical names. These studies discuss the Hungarian transliteration of those names which are written in non-Latin script and the rules or traditions of transcribing those names which are not written by letters but by various "pictures" of the ideas or objects. Further, the use of exonyms or conventional names – due to the specific character of Hungarian language and to the fact that the language is spoken by millions well beyond the present borders of the country – is also a popular topic for Hungarian cartographers, geographers and historians. -
A Joint Report on Geomanifestations in the Pannonian Basin
Project approved for funding as part of the ERA-NET GeoERA Authors and affiliation: Nina Rman, GeoZS Éva Kun, MBFSZ Natalija Samardžić, FZZG Dejan Šram, GeoZS Jure Atanackov, GeoZS Deliverable 4.2 Miloš Markič, GeoZS Andrej Lapanje, GeoZS Dušan Rajver, GeoZS A joint report on Ildikó Sarolta Selmeczi, MBFSZ geomanifestations in the Gyula Maros, MBFSZ Pannonian basin Tamara Marković, CGS-HGI Tamás Budai, MBFSZ Edit Babinszki, MBFSZ E-mail of contact person: [email protected] Version: 21.05.2021 This report is part of a project that has received funding by the European Union’s Horizon 2020 research and innovation programme under grant agreement number 731166. Deliverable Data Deliverable number D4.2 Dissemination level Public Deliverable name A joint report on geomanifestations in the Pannonian basin Work package WP4, T4.2 Geomanifestations Lead WP/Deliverable beneficiary MBFSZ/GeoZS and MBFSZ Deliverable status Submitted (Author(s)) 21/05/2021 Rman Nina et al. Verified (WP leader) 24/05/2021 Gyula Maros Approved (Coordinator) 25/05/2021 Renata Barros TABLE OF CONTENTS 1 INTRODUCTION ..................................................................................................................... 2 2 STRUCTURAL FRAMEWORK OF THE PANNONIAN BASIN ........................................ 3 2.1 The Pannonian Basin in the frame of the Alpine orogeny .............................................. 3 2.1.1 Pre-Pannonian phase ......................................................................................... 5 2.1.2 Pannonian Basin evolution -
Powerpoint Bemutató
Hungary National report Ádám Kertész Head of Department Geographical Research Institute Hungarian Academy of Sciences 1112 Budapest, Budaörsi út 45. E-mail: [email protected] Land use changes in Hungary 1895-2001 (1000 ha) Non- Arable Agricult. Cult. Year Orchards Vineyard Meadow Pasture Forest Reed cult. land land* area area 1895 5103 95 175 798 1268 7439 1191 49 8678 528 1930 5587 107 214 668 1001 7577 1095 30 8702 595 1945 5567 115 215 639 962 7498 1116 29 8643 650 1950 5518 152 230 609 865 7376 1166 29 8571 728 1965 5085 319 247 419 885 6954 1422 29 8404 900 1970 5046 318 230 407 876 6875 1471 32 8378 925 2001 4516 195 93 1061 5865 1772 60 7697 1606 * Agricultural land is arable land, orchard, vineyard, meadow and pasture alltogether. Environmental management of forested areas • Forestry policy is directed towards nature conservation and environmental protection • Focus on socio-economic and cultural benefits and not on production • Ecology and biodiversity • 2004: National Forest Program of Hungary The main objective of the National Forest Program is to ensure long term sustainability and to satisfy the demands of consumption, environmental protection, recreation taking socio-economic and cultural aspects into account. Strategic objectives • Protection and support of natural processes • Conservation and rehabilitation of quasi natural forests • Protection of protected and rare species • Landscape protection • Maintenance of forested area Territorial data • Forest area: 1.974 million ha • Area covered by trees: 1.843 million ha • Percentage of forested area: 19.8% • 387 million ha are protected (20%) Changes of the forested area Forested areas in Hungary (2006) Afforestation between 1920 and 2005 Mountains of Hungary Hungary has several moderately high ranges of mountains. -
Surface Geology of Hungary : Explanatory Notes to the Geological
Surface geology of Hungary Explanatory notes to the Geological map of Hungary (1:500 000) Edited by: Zsolt KERCSMÁR Written by: Tamás BUDAI, Gábor, CSILLAG Zsolt KERCSMÁR, Ildikó SELMECZI, Orsolya SZTANÓ Budapest, 2015 Copyright Geological and Geophysical Institute of Hungary 2015 All rights reserved! Rewier: Gyula KONRÁD English text: Daniella TOLMÁCS Linguistic reviewer: Philip RAWLINSON Technical editor: Olga PIROS DTP: OLGA PIROS PÉTER KŐBÁNYAI Published by the Geological and Geophysical Institute of Hungary Responsible editor: FANCSIK Tamás director Reference: KERCSMÁR, ZS. (ed.), BUDAI, T., CSILLAG, G., SELMECZI, I., SZTANÓ, O. 2015: Surface geology of Hungary. Explanatory notes to the Geological map of Hungary (1:500 000). — Geological and Geophysical Institute of Hungary, Budapest. ISBN 978-963-671-302-7 Contents Introduction (Zsolt KERCSMÁR) . 5 Geological build-up of the regions of Hungary (Tamás BUDAI) . 7 Dunántúli-középhegység (Transdanubian Range) . 7 Északi-középhegység (North Hungarian Range) . 9 The Mecsek and the Villány Hills . 10 Dunántúli-dombság (Transdanubian Hills) . 11 Kisalföld (Little Hungarian Plain) and Alpokalja . 11 Alföld (Great Hungarian Plain) . 11 Geological description of the superficial formations of Hungary (Tamás BUDAI – TB, Gábor CSILLAG – GCs, Zsolt KERCSMÁR – ZsK, Ildikó SELMECZI – IS, Orsolya SZTANÓ – OSz) . 12 Palaeozoic (undivided) (TB) . 12 Ordovician–Silurian (TB) . 12 Ordovician–Devonian (TB) . 13 Silurian–Devonian (TB) . 13 Devonian (TB) . 13 Carboniferous (TB) . 14 Permian (TB) . 15 Triassic (TB) . 17 Lower Triassic . 17 Middle Triassic . 17 Middle–Upper Triassic . 19 Upper Triassic . 20 Triassic–Jurassic (TB) . 22 Triassic–Cretaceous (TB) . 22 Jurassic . 23 Lower–Middle Jurassic (TB) . 23 Middle–Upper Jurassic (TB) . 24 Jurassic (undivided) (TB) . 25 Jurassic–Cretaceous (TB) . -
Hungary Hungary
COUNTRY REPORT ON THE STATE OF PLANT GENETIC RESOURCES FOR FOOD AND AGRICULTURE HUNGARY HUNGARY MINISTRY OF AGRICULTURE AND RURAL DEVELOPMENT HUNGARY SECOND COUNTRY REPORT CONCERNING THE STATE OF PLANT GENETIC RESOURCES FOR FOOD AND AGRICULTURE Supervising Authority Central Agricultural Office Responsible Body of the Report Central Agricultural Office, Research Centre for Agrobotany September 2008 2 Note by FAO This Country Report has been prepared by the national authorities in the context of the preparatory process for the Second Report on the State of World’s Plant Genetic Resources for Food and Agriculture. The Report is being made available by the Food and Agriculture Organization of the United Nations (FAO) as requested by the Commission on Genetic Resources for Food and Agriculture. However, the report is solely the responsibility of the national authorities. The information in this report has not been verified by FAO, and the opinions expressed do not necessarily represent the views or policy of FAO. 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 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. -
Surface Geology of Hungary Explanatory Notes to the Geological Map of Hungary (1:500 000)
Surface geology of Hungary Explanatory notes to the Geological map of Hungary (1:500 000) Edited by: Zsolt KERCSMÁR Written by: Tamás BUDAI, Gábor, CSILLAG Zsolt KERCSMÁR, Ildikó SELMECZI, Orsolya SZTANÓ Budapest, 2015 Copyright Geological and Geophysical Institute of Hungary 2015 All rights reserved! Rewier: Gyula KONRÁD English text: Daniella TOLMÁCS Linguistic reviewer: Philip RAWLINSON Technical editor: Olga PIROS DTP: OLGA PIROS PÉTER KŐBÁNYAI Published by the Geological and Geophysical Institute of Hungary Responsible editor: FANCSIK Tamás director Reference: KERCSMÁR, ZS. (ed.), BUDAI, T., CSILLAG, G., SELMECZI, I., SZTANÓ, O. 2015: Surface geology of Hungary. Explanatory notes to the Geological map of Hungary (1:500 000). — Geological and Geophysical Institute of Hungary, Budapest. ISBN 978-963-671-302-7 Contents Introduction (Zsolt KERCSMÁR) . 5 Geological build-up of the regions of Hungary (Tamás BUDAI) . 7 Dunántúli-középhegység (Transdanubian Range) . 7 Északi-középhegység (North Hungarian Range) . 9 The Mecsek and the Villány Hills . 10 Dunántúli-dombság (Transdanubian Hills) . 11 Kisalföld (Little Hungarian Plain) and Alpokalja . 11 Alföld (Great Hungarian Plain) . 11 Geological description of the superficial formations of Hungary (Tamás BUDAI – TB, Gábor CSILLAG – GCs, Zsolt KERCSMÁR – ZsK, Ildikó SELMECZI – IS, Orsolya SZTANÓ – OSz) . 12 Palaeozoic (undivided) (TB) . 12 Ordovician–Silurian (TB) . 12 Ordovician–Devonian (TB) . 13 Silurian–Devonian (TB) . 13 Devonian (TB) . 13 Carboniferous (TB) . 14 Permian (TB) . 15 Triassic (TB) . 17 Lower Triassic . 17 Middle Triassic . 17 Middle–Upper Triassic . 19 Upper Triassic . 20 Triassic–Jurassic (TB) . 22 Triassic–Cretaceous (TB) . 22 Jurassic . 23 Lower–Middle Jurassic (TB) . 23 Middle–Upper Jurassic (TB) . 24 Jurassic (undivided) (TB) . 25 Jurassic–Cretaceous (TB) . -
Neuroptera: Osmylidae, Sisyridae)
A study on the Hungarian freshwater osmylid and sponge-flies fauna (Neuroptera: Osmylidae, Sisyridae) ABRAHAM LEVENTE ABRAHAM, L.: A study on the Hungarian freshwater osmylid Hungarian freshwater Neuroptera fauna based on the 'and sponge-flies fauna (Neuroptera: Osmyfidae, Sisyridae). collection of their data from the literature and different Abstract: There are four species in the Hungarian freshwater collections of Hungarian museums. Neuroptera fauna according to the redeterminated collections Besides, the seasonal activity of freshwater neu found in six Hungarian museums: Osmylus fulvicephalus, Sisyra fuscata, Sisyra terminalis, Sisyra jutlandica. The author ropteroids species in Hungary, the flight activity pat gives the collecting data, the distribution maps and both the terns of these species were studied. It gives an impor seasonal activity graphs and flight activity patterns of these tant information on their collection possibilities. species. Short evaluations on these species from faunistical, and chorological points of view are also given. Materials and methods Key words: Neuroptera, Osmylidae, Sisyridae, distribution, seasonal activity, day and night activity. The determined collections found in Bakony Natural History Museum (Zirc), Janus Pannonius Museum Introduction Natural History Department (Pecs), Hungarian Natural History Museum (HNHM Budapest), Matra Natural Neuroptera species living presently in. the world are History Museum (Gyongyos), Somogy County Museum known to belong to 17 families (NEW 1989). Most of Natural History Department (Kaposvar) and the Ujhe them are considered to be found in terrestrial habitat, Iyi's collection (Budapest) later deposited in HNHM, only five of Neuroptera families (Rapismatidae, were revised. All the other available data from the data Osmylidae, Neurothidae, Sisyridae, Polystoechotidae) bases cited in the Hungarian literature were made use .have aquatic larvae or larvae living only near water.