CENTRE for REGIONAL STUDIES of HUNGARIAN ACADEMY of SCIENCES DISCUSSION PAPERS No. 28 Climate History of Hungary Since 16Th Cent

Total Page:16

File Type:pdf, Size:1020Kb

CENTRE for REGIONAL STUDIES of HUNGARIAN ACADEMY of SCIENCES DISCUSSION PAPERS No. 28 Climate History of Hungary Since 16Th Cent Discussion Papers 1999. No. 28. Climate History of Hungary Since 16th Century: Past, Present and Future CENTRE FOR REGIONAL STUDIES OF HUNGARIAN ACADEMY OF SCIENCES DISCUSSION PAPERS No. 28 Climate History of Hungary Since 16th Century: Past, Present and Future by Lajos RACZ Series editor Zoltan GAL Pecs 1999 Discussion Papers 1999. No. 28. Climate History of Hungary Since 16th Century: Past, Present and Future Publishing of this paper is supported by the Research Fund of the Centre for Regional Studies, Hungary Translated by Rita Konta Translation revised by Neil MacAskill Figures Katalin Molnarne Kasza Technical editor Mihaly Fodor Tiberias BT ISSN 0238-2008 © 1999 by Centre for Regional Studies of the Hungarian Academy of Sciences Typeset by Centre for Regional Studies of HAS Printed in Hungary by Siimegi Nyomdaipari, Kereskedelmi es Szolgaltato Ltd., Pecs Discussion Papers 1999. No. 28. Climate History of Hungary Since 16th Century: Past, Present and Future CONTENTS Foreword 5 Acknowledgements 6 1. Territorial Variations of the Hungarian State since 1000 AD 7 2. Sources for Hungarian Climate History Research 12 2.1. Documentary Sources of Rethly's Source Book 14 2.1.1. Chronicles, Annals 15 2.1.2. Records of Public Administration 17 2.1.3. Private Estate Records 18 2.1.4. Personal Papers 18 2.1.5. Early Journalism 20 2.1.6. Early Instrument Based Records 20 2.1.7. Meteorological Instrument Records 21 2.2. Method of Analyzing the Source Documents 22 3. Climate Characteristics of the Carpathian Basin 25 3.1. Temperature Conditions of Hungary 25 3.2. Precipitation in Hungary 27 4. Climate Variations by Month in Hungary during the Little Ice Age 29 and Recent Global Warming 4.1. January 29 4.1.1. January Temperature Anomalies and Medium Term Trends 29 4.1.2. January Precipitation Anomalies and Medium Term Trends 33 4.1.3. January Climate Change Trends over the Centuries 34 4.2. February 36 4.2.1. February Temperature Anomalies and Medium Term Trends 36 4.2.2. February Precipitation Anomalies and Medium Term Trends 40 4.2.3. February Climate Change Trends over the Centuries 41 4.3. March 43 4.3.1. March Temperature Anomalies and Medium Term Trends 43 4.3.2. March Precipitation Anomalies and Medium Term Trends 46 4.3.3. March Climate Change Trends over the Centuries 47 4.4. April 49 4.4.1. April Temperature Anomalies and Medium Term Trends 49 4.4.2. April Precipitation Anomalies and Medium Term Trends 52 4.4.3. April Climate Change Trends over the Centuries 53 4.5. May 55 4.5.1. May Temperature Anomalies and Medium Term Trends 55 4.5.2. May Precipitation Anomalies and Medium Term Trends 58 4.5.3. May Climate Change Trends over the Centuries 60 4.6. June 62 4.6.1. June Temperature Anomalies and Medium Term Trends 62 Discussion Papers 1999. No. 28. Climate History of Hungary Since 16th Century: Past, Present and Future 4.6.2. June Precipitation Anomalies and Medium Term Trends 64 4.6.3. June Climate Change Trends over the Centuries 66 4.7. July 68 4.7.1. July Temperature Anomalies and Medium Term Trends 68 4.7.2. July Precipitation Anomalies and Medium Term Trends 71 4.7.3. July Climate Change Trends over the Centuries 73 4.8. August 75 4.8.1. August Temperature Anomalies and Medium Term Trends 75 4.8.2. August Precipitation Anomalies and Medium Term Trends 78 4.8.3. August Climate Change Trends over the Centuries 80 4.9. September 82 4.9.1. September Temperature Anomalies and Medium Term Trends 82 4.9.2. September Precipitation Anomalies and Medium Term Trends 84 4.9.3. September Climate Change Trends over the Centuries 86 4.10. October 88 4.10.1. October Temperature Anomalies and Medium Term Trends 88 4.10.2. October Precipitation Anomalies and Medium Term Trends 90 4.10.3. October Climate Change Characteristics over the Centuries 92 4.11. November 94 4.11.1. November Temperature Anomalies and Medium Term Trends 94 4.11.2. November Precipitation Anomalies and Medium Term Trends 96 4.11.3. November Climate Change Trends over the Centuries 97 4.12. December 99 4.12.1. December Temperature Anomalies and Medium Term Trends 99 4.12.2. December Precipitation Anomalies and Medium Term Trends 102 4.12.3. December Climate Change Trends over the Centuries 103 5. Seasonal Climate Trends of the Decades and Centuries 105 5.1. Winter 105 5.2. Spring 109 5.3. Summer 112 5.4. Autumn 115 6. Half-Yearly and Yearly Climate Change Trends 118 6.1. Winter Half-Year 118 6.2. Summer Half-Year 122 6.3. Yearly Temperature and Precipitation Time Series 125 7. Climate Change Characteristics in Hungary during the Little 128 Ice Age and the Recent Warming 7.1. Correlation Study of the Climate History and Meteorological 128 Monthly Time Series 7.2. Hungarian Features of the Climate Changes 132 References 134 Appendix 142 Discussion Papers 1999. No. 28. Climate History of Hungary Since 16th Century: Past, Present and Future In memory of Antal Rethly FOREWORD The history of this booklet begins as far back as March 1985 when, as a second-year university student of both geography and history, I was trying to find a topic for my research work that was related to both sciences. My university professors, Lciszlo Makra and Gyorgy Peczely introduced me to the reference work of Antal Rethly. During my university studies Gcibor Mezosi acted ,as my tutor, while the first studies I made were commented on by Vera Zimcinyi, Agnes R. Vcirkonyi, Scindor Gyimesi, Lciszlo Katus, Lciszlo Kordos, Jcinos Mika and Jcinos Justycik. In 1990 I was fortunate enough to make contact with the prominent actor and coordinator of European climate history research, Professor Christian Pfister, who played a very dominant role in my profession- al career. At Prof. Pfister's invitation I worked at the Department of Regional and Environmental History of the University of Bern in the 1990's. During my studies in Bern Christian Pfister and Hannes Schule introduced me to the method of using docu- mentary sources, while the availability of adequate software and hardware resources further supported me in my ongoing research work. In addition to the climate history work completed in Bern, I enjoyed the benefit of considerable assistance in my research from historians such as Bernard Lepetit and Jean-Yves Grenier of `Ecole des Hautes Etudes en Sciences Sociales' in Paris. The final impetus to produce this booklet was provided by the Hungarian Scholarship Committee ensuring a two-month scholar- ship in the Czech Republic at the end of 1998. The manuscript of this edition was pre- pared at the Geographic Institute of the Masaryk University in Brno with the assistance of Professor Rudolf Brcizdil and Petr Dobrovolny. Brno, 12 December 1998 Lajos Racz 5 Discussion Papers 1999. No. 28. Climate History of Hungary Since 16th Century: Past, Present and Future ACKNOWLEDGEMENTS The study was realized with the financial support of the OTKA Foundation (F 20829, F 22261 and T 29183), the OKTK Foundation (1089/III.b. and 1502/III.b.) and Eotvos Fellowship Foundation. This paper contains the results of Alfold-2 Research Program' of Hungarian Academy of Sciences. 6 Rácz, Lajos: Climate History of Hungary Since 16th Century: Past Present and Future. Pécs: Centre for Regional Studies, 1999. 160 p. Discussion Papers, No. 28. 1. TERRITORIAL VARIATIONS OF THE HUNGARIAN STATE SINCE 1000 AD The Hungarian tribes reached their final homeland, the Carpathian Basin during one of the last migrational waves at the end of the 9' century. The 300,000 square kilo- meter area of the Carpathian Basin became the geographical site of the Hungarian State for centuries. Figure 1 Central Europe in the 11th century 0 SOOkin \ I. ) GRAND PRINCEDOM I I OF KIEV / i %.,. 1 s...C ..... e C...4,.• POLISH ( 4. ;.. GERMAN-ROMAN JKIKODOM • .0' , 't EMPIRE .7. s ) • i..i t tirmisom f .+•.......; ._. —•-• ! HUNGARIAN .k C.." KINGDOM j C nit7 t......•.'*".. ..r ' 4 1‘1 N % s.' 4VP/,b, I ' se (St.) Stephen I (Istvcin) (997-1038) officially adopted Christianity in 1000 AD and founded the Hungarian Kingdom. In the Middle Ages the area of the country gradual- ly expanded following several conquests and inheritances. In the 12' century the Croatian crown went to the Hungarian king as the Croatian royal family died out. The Croatian-Hungarian personal union endured until the beginning of the 20" century. The Hungarian State occupied the largest amount of territory in the Middle Ages when, in the 14' century, the Hungarian King Lajos I the Great took the title of King of Poland. 7 Rácz, Lajos: Climate History of Hungary Since 16th Century: Past Present and Future. Pécs: Centre for Regional Studies, 1999. 160 p. Discussion Papers, No. 28. Figure 2 Borders of the Hungarian Kingdom in the 14th century I . , . . L i 1 r ./ 1 - - - :-.:. .1' 0 • c.., • s ■ • • .,. v . 1 5 .A.7 . .....% ‘. L• 4"' ‘ .4. .." t . ••••••., ..0 'A. .,. r 7 C. s''''' I.; 0)„ GERMAN- 1. ' • ROMAN '""1E HEEZ.../4.6 00 4;; EMPIRE (KINGDOM HUNGARIAN Y, to, • KINGDOM rvii % •••• • — ••••• NptlAC":::* %e • .1" e•—• 1 00474'%, S . In the 15th century the Turks appeared at the southern border of Hungary and con- quered the southern and central territory of the country after a struggle of one and a half centuries, while the eastern territory, Transylvania, became a Turkish satellite- principality. The Hungarian Kingdom was then limited to the northern and northwest- ern regions of the Carpathian Basin and became part of the Central European Habsburg Monarchy together with Croatia.
Recommended publications
  • The Relationship Between Landslide Activity and Weather: Examples from Hungary
    Natural Hazards and Earth System Sciences (2003) 3: 43–52 c European Geosciences Union 2003 Natural Hazards and Earth System Sciences The relationship between landslide activity and weather: examples from Hungary J. Szabo´ Department of Physical Geography, P.O. Box 9, H-4010 Debrecen, Hungary Received: 27 November 2001 – Revised: 7 May 2002 – Accepted: 8 May 2002 Abstract. The paper presents the impact of irregular rainfall by them may be largely variable in the geomorphic evolution events triggering landslides in the regional context of land- of regions where conditions are favourable. Rock quality, slides in Hungary. The author’s experience, gathered from stratification, slopes with high variability locally (e.g. as a decades of observations, confirms that landslide processes result of lateral river erosion) lead to various landslide types, are strongly correlate with precipitation events in all three and the changing weather conditions affect them in different landscape types (hill regions of unconsolidated sediments; ways. high bluffs along river banks and lake shores; mountains of The paper investigates some aspects of the relationship be- Tertiary stratovolcanoes). Case studies for each landscape tween landslides and weather in the regional context of land- type underline that new landslides are triggered and old ones slides in Hungary (Szabo,´ 1992, 1993, 1996a). In addition, are reactivated by extreme winter precipitation events. This the author introduces some case studies, particularly from the assertion is valid mainly for shallow and translational slides. northeastern part of the country. Wet autumns favour landsliding, while the triggering influ- ence of intense summer rainfalls is of a subordinate nature. A recent increasing problem lies in the fact that on previously 2 Methods unstable slopes, stabilised during longer dry intervals, an in- The author has been investigating landslides and the fea- tensive cultivation starts, thus increasing the damage caused tures produced by them for more than thirty years.
    [Show full text]
  • Budapest, 1900-1918
    The First Nyugat Generation and the Politics of Modern Literature: Budapest, 1900-1918 Maxwell Staley 2009 Central European University, History Department Budapest, Hungary Supervisor: Gábor Gyáni Second Reader: Matthias Riedl In partial fulfillment of the requirements for the degree of Masters of Arts CEU eTD Collection 2 Copyright in the text of this thesis rests with the Author. Copies by any process, either in full or part, may be made only in accordance with the instructions given by the Author and lodged in the Central European Library. Details may be obtained from the librarian. This page must form a part of any such copies made. Further copies made in accordance with such instructions may not be made without the written permission of the Author. CEU eTD Collection 3 Abstract This thesis investigates the connections between arts and politics in fin-de-siècle Hungary, as expressed in the writings of the First Nyugat Generation. Various elements of the cultural debate in which the Nyugat writers participated can illustrate the complexities of this relationship. These are the debate over the aesthetics of national literature, the urban-versus-rural discourse, and the definition of the national community. Through close reading of the Nyugat group’s writings on these topics, two themes are explored, relating to the ambivalence with which the Nyugat writers implemented their project of westernizing Hungarian culture. The first is the dominant presence of the nationalist discourse within an ostensibly cosmopolitan endeavor. This fits in with a general artistic trend of Hungarian modernism, and can be explained with reference to the ambiguous position of Hungary within Europe and the subsequent complexities present in the national discourse.
    [Show full text]
  • The Late Quaternary Paleoecology and Environmental History of Hortobágy, a Unique Mosaic Alkaline Steppe from the Heart of the Carpathian Basin
    In: Steppe Ecosystems ISBN: 978-1-62808-298-2 Editors: M. B. Morales Prieto and J. Traba Diaz © 2013 Nova Science Publishers, Inc. No part of this digital document may be reproduced, stored in a retrieval system or transmitted commercially in any form or by any means. The publisher has taken reasonable care in the preparation of this digital document, but makes no expressed or implied warranty of any kind and assumes no responsibility for any errors or omissions. No liability is assumed for incidental or consequential damages in connection with or arising out of information contained herein. This digital document is sold with the clear understanding that the publisher is not engaged in rendering legal, medical or any other professional services. Chapter 8 THE LATE QUATERNARY PALEOECOLOGY AND ENVIRONMENTAL HISTORY OF HORTOBÁGY, A UNIQUE MOSAIC ALKALINE STEPPE FROM THE HEART OF THE CARPATHIAN BASIN Pál Sümegi1,2,, Gábor Szilágyi3, Sándor Gulyás1, Gusztáv Jakab4 and Attila Molnár3 1University of Szeged, Department of Geology and Paleontology, Szeged, Hungary 2Institute of Archeology, Hungarian Academy of Science, Budapest, Hungary 3Headquaters of the Hortobágy National Park, Debrecen, Hungary 4University of Szent István, Tessedik Campus, Szarvas, Hungary ABSTRACT The first national park in Hungary was established in 1973 in the area of Hortobágy with the aim of protecting dry and humid alkaline steppe areas and concomitant fauna. In 1999 the Hortobágy National Park was included in the world heritage list of the UNESCO. The outstanding importance of the park comes from dominantly non-arboreal, steppe vegetation harboring a unique avifauna and highly variable alkaline and chernozem soils displaying a complex mosaic-like spatial patterning.
    [Show full text]
  • Clim Mate C Change an Cas ESPO E and T Nd Loc Fin a Se Stu on Clim
    Versioon 31/05/2011 ESPON Climate: Climate Change and Territorial Effects on Regions and Local Economies Applied Research Project 2013/1/4 Final Report Annex 2 Case Study Tisza River Csete, Mária (BME) Dzurdzenik, Jan (ARR) Göncz, Annamária (VÁTI) Király, Dóra (VÁTI) Pálvölgyi, Tamás (BME) Peleanu, Ion (URBAN-INCERC) Petrisor, Alexandru-Ionut (URBAN-INCERC) Schneller, Krisztián (VÁTI) Staub, Ferenc (VÁTI) Tesliar, Jaroslav (ARR) Visy, Erzsébet 1 This report presents the final results of an Applied Research Project conducted within the framework of the ESPON 2013 Programme, partly financed by the European Regional Development Fund. The partnership behind the ESPON Programme consists of the EU Commission and the Member States of the EU27, plus Iceland, Liechtenstein, Norway and Switzerland. Each partner is represented in the ESPON Monitoring Committee. This report does not necessarily reflect the opinion of the members of the Monitoring Committee. Information on the ESPON Programme and projects can be found on www.espon.eu The web site provides the possibility to download and examine the most recent documents produced by finalised and ongoing ESPON projects. This basic report exists only in an electronic version. ISBN 978-2-919777-04-4 © ESPON & VATI, 2011 Printing, reproduction or quotation is authorised provided the source is acknowledged and a copy is forwarded to the ESPON Coordination Unit in Luxembourg. Contents 0. Introduction 1 1. Characterisation of the region 3 2. Main effects of climate changes on case study region 12 3. Validation of the exposure indicators of pan-European analysis from a regional aspect 25 4. Climate change impacts on river floods based on national and regional level literatures 40 5.
    [Show full text]
  • Precipitation in the Carpathian Basin
    TEMPORALTEMPORAL ANDAND SPATIALSPATIAL CHANGESCHANGES OFOF CLIMATECLIMATE ELEMENTSELEMENTS ININ HUNGARYHUNGARY PRECIPITATIONPRECIPITATION © As the climate of Hungary tends to drought , temporal and spatial distribution of precipitation has of special importance in agriculturala nd ecological point of view . © Precipitation in Hungary is generally less than the requirement of vegetation . A csapad ék által ában kevesebb, mint a veget áci ó ig énye. The climatic water balance is negative in the substantial part of the country. Mean monthly and annual sums of precipitation in Hungary, mm, 1961-1990 station year Temporal dynamics of precipitation © The annual cozrse of precipitation shows double wave . Minimum precipitation falls in January . This is due to the low vapour pressure and frequent anticyclonic large -scale weather situations (Siberian maximum). © Most of the precipitation falls between May to July . This may be associated with the maximum vapour pressure , near the Medard cyclone activity , and the intensifying convection . © Maximum precipitation shows slight temporal delays in different regions of the country . © In the Transdanubian Hills and the Bakony area the most precipitation occurs in May , in West Hungary in July , while in the major part of the country in June . Temporal dynamics of precipitation © A secondary maximum of precipitation can also be observed at autumn (October -November ) in South Dun ánt úl and in the south - east slopes of Dun ánt úli Medium-high Mountains . © It comes from the rains of warm fronts of the Mediterranean cyclones (Genoa cyclones ) originating from Ligurian sea area . © It is not uncommon that , due to abundant autumn rains , winter hal - year is wetter (in 20 -30% of the cases ).
    [Show full text]
  • 137. Évfolyam, 2. Szám
    Krónika Bérci Károly (1952–2012) – SCHWEITZER FERENC – TINER TIBOR ......................................................... 209 Irodalom Frisnyák Sándor: Tájhasználat és térszervezés. Történeti földrajzi tanulmányok. – BOROS LÁSZLÓ ... 211 Gál András (szerk.): A Zempléni-hegység tudományos feltárói és gazdaságfejlesztői. – BOROS LÁSZLÓ ................................................................................................................................. 212 Hardi Tamás: Duna-stratégia és területi fejlődés. – GÁL ZOLTÁN ......................................................... 214 Illés Sándor: Időskori nemzetközi migráció – magyar eset. – IRIMIÁS ANNA ...................................... 217 Sallai János: Egy idejét múlt korszak lenyomata: a vasfüggöny története. – KOVÁLY KATalIN ........... 218 Földrajzi Közlemények 2013. 2.szám Támogatóink: Kiadja a MAGYAR FÖLDRAJZI TÁRSASÁG A Nemzeti Kulturális Alap és a Magyar Tudományos Akadémia támogatásával A kiadásért felel: Michalkó Gábor Tördelés és nyomdai előkészítés: Graphisto Kft. Borítóterv: Liszi János Telefon: (20) 971-6922, e-mail: [email protected] Készült 600 példányban Nyomdai kivitelezés: Heiling Media Kiadó Kft. 137. évfolyam, 2. szám Telefon: (06-1) 231-4040 HU ISSN 0015-5411 2013 Magyar Földrajzi Társaság Földrajzi Közlemények Alapítva: 1872 A Magyar Földrajzi Társaság tudományos folyóirata Tisztikar Geographical Review • Geographische Mitteilungen Elnök: SZABÓ JÓZSEF ny. egyetemi tanár Bulletin Géographique • Bollettino Geografico • Географические Сообщения
    [Show full text]
  • 3RD INTERNATIONAL YOUNG RESEARCHER SCIENTIFIC CONFERENCE on “Sustainable Regional Development - Challenges of Space & Society in the 21St Century”
    3RD INTERNATIONAL YOUNG RESEARCHER SCIENTIFIC CONFERENCE on “Sustainable Regional Development - Challenges of Space & Society in the 21st Century” PAPERS OF THE CONFERENCE Gödöllő 26 April, 2018 Edited by: Bálint Horváth Anikó Khademi-Vidra, Ph.D. habil. Izabella Mária Bakos Printing Supervisor: Szent István University Publisher H-2100 Gödöllő, Páter Károly street 1. Studies published in the conference proceedings were reviewed by the members of the Scientific Committee of the Conference and colleagues with academic degrees from the Szent István University and Warsaw University of Life Sciences ISBN 978-963-269-730-7 Digitally multiplied in 70 copies. TABLE OF CONTENTS SCIENTIFIC COMMITTEE ...................................................................................................... 7 ORGANIZING COMMITTEE .................................................................................................. 9 PAPERS OF THE CONFERENCE ......................................................................................... 11 AGRICULTURAL TRENDS .................................................................................................. 13 LOCAL COMMUNITIES ....................................................................................................... 83 ENVIRONMENTAL APPROACHES OF TERRITORIAL DEVELOPMENT .................. 181 INNOVATIONS OF TOURISM AND MARKETING ......................................................... 264 REGIONAL COMPETITIVENESS .....................................................................................
    [Show full text]
  • Extreme Weather Events and Their Public Health Relevance
    CENTRAL EUROPEAN JOURNAL OF OCCUPATIONAL AND ENVIRONMENTAL MEDICINE 2019; 25 (1-2); · 75 EXTREME WEATHER EVENTS AND THEIR PUBLIC HEALTH RELEVANCE ZSÓFIA TISCHNER1, BÁLINT IZSÁK2, ANNA PÁLDY2 1Szent István University Doctoral School, Budapest, Hungary 2National Public Health Center, Budapest, Hungary ABSTRACT Nowadays more and more extreme weather events occur due to climate change. Hungary is extermely vulnerable to floods, inland water inundations and droughts; they can occur almost every year in any parts of the country due to the geographical position, geological and hydro- logical characteristics. Other events like wildfires are not so serious in Hungary as in the medi- terranean countries. As these extreme events can happen more and more frequently, there is a need to prepare for the reduction of health impacts of these events. The Hyogo Framework for Action, the WHO and the Public Health England have formulated recommendations for risk reduction and measures of prevention of health impacts of extreme weather events. In this paper the authors give a description of the different types of extreme weather events, of their health impacts in Europe and in Hungary and the possible preventive measures based on international recommendations. KEY WORDS: climate change, extreme weather events, mortality, vulnerability, adaptation Corresponding author: Zsófia Tischner Szent István University Doctoral School Budapest, Hungary E-mail: [email protected] Received: 5th May 2019 Accepted: 19th June 2019 INTRODUCTION Climate change is presumably the most serious environmental health problem of the 21st century (Watts et al., 2018). The impacts of climate extremes and the potential for disasters result from the climate extremes themselves and from the exposure and vulnerability of human and natural systems, as it was pointed out in the IPCC Special Report on Managing the Risks of Extreme Events and Disasters to Advance Climate Change Adaptation (Field et al., 2012).
    [Show full text]
  • Shifts and Modification of the Hydrological Regime Under Climate Change in Hungary
    Chapter 6 Shifts and Modification of the Hydrological Regime Under Climate Change in Hungary Béla Nováky and Gábor Bálint Additional information is available at the end of the chapter http://dx.doi.org/10.5772/54768 1. Introduction Hydrological regime of water bodies is highly dependent on climatic factors. The runoff is mainly defined by seasonal distribution of precipitation and intensive rainfall events on one side and potential evapo-transpiration on the other. Near surface air temperatures (and other factors of heat budget) regulate the phase of precipitation and consequently snow accumulation, ablation and snowmelt induced runoff. Change of climate evidently would lead to changes in the hydrological regime. Nevertheless, hydrological regime can also be modified by different human activities towards water bodies directly (river training, flood control, flow regulation, water abstractions and inlets) or indirectly to catchments (urbanization, land use changes, deforestation). The tasks of water management and water related policies may change with climate fluctuations, as it is attested by the historical past. The long lasting wet period in the second half of 19th century resulted the framing the law on water regulation in 1871, and frequent droughts in 1930s led to the law on irrigation in 1937. The given chapter gives an overview of changes in the hydrological regime of water bodies observed in the historical and more recent past and also projected for the future under observed climate change and future climate change scenarios in central regions of Danube River Basin, i.e. in Hungary with limited outlook beyond the national borders, the adaptation possibilities for certain water management sectors to cope with adverse effects of the climate change are also discussed.
    [Show full text]
  • Climate Change and Hungary: Mitigating the Hazard and Preparing for the Impacts (The “Vahava” Report)
    CLIMATE CHANGE AND HUNGARY: MITIGATING THE HAZARD AND PREPARING FOR THE IMPACTS (THE “VAHAVA” REPORT) Budapest 2010 vvahava-2010-12.inddahava-2010-12.indd BB11 22010.12.08.010.12.08. 111:26:251:26:25 The VAHAVA Report is the outcome of the VAHAVA Project, which was implemented in the period of 2003-2006 with some follow-up activities during 2007-2008. The basic objective of the Project was the synthetisation of the scientifi c results on the climate change hazard, assessment of its impacts in our region, and the science-based national mitigation and adaptation response policy options. Edited by TIBOR FARAGÓ, ISTVÁN LÁNG, LÁSZLÓ CSETE The VAHAVA Report is based on the contributions of the following experts: István LÁNG (Foreword) Tibor FARAGÓ (1. International climate policy cooperation and Hungary) Judit BARTHOLY and Rita PONGRÁCZ (2. Climate change scenarios for the Carpathian Basin) István LÁNG (3. The “VAHAVA” project) Gábor VIDA (4. Nature conservation and the climatic factors) Kornél HARKÁNYI (5. Water management and climate change) Márton JOLÁNKAI (6. Agriculture, soil management and climate change) György VÁRALLYAY (7. Soil functions, soil management and the climatic factors) Ernő FÜHRER (8. Forestry and climate change) Tamás JÁSZAY (9. Energy and climate change) Bálint PETRÓ (10. Architecture: climatic impacts and response measures) Katalin TÁNCZOS (11. Traffi c, transportation and the climatic factors) Anna PÁLDY (12. Health, health protection and the climatic factors) Ágnes SALLAY (13. Climate change and tourism) István BUKOVICS (14. Tasks of catastrophe defence in light of global climate change) László CSETE (15. Creating reserves) Zoltán DEZSÉNY (16. Insurance implications of climate change) Viktória SZIRMAI (17.
    [Show full text]
  • Climate Change and Restoration of Degraded Land
    Climate Change and Restoration of Degraded Land Edited by Arraiza Bermúdez-Cañete, Mª Paz Universidad Politécnica de Madrid, Spain Santamarta Cerezal, Juan C. Universidad de La Laguna, Canary Islands, Spain Ioras, Florin Buckinghamshire New University, United Kingdom García Rodríguez, José Luís Universidad Politécnica de Madrid, Spain Abrudan, Ioan Vasile Transilvania University, Romania Korjus, Henn Estonian University of Life Science Borbála Gálos University of West Hungary Climate Change and Restoration of Degraded Land © 2014 The Authors. Published by: Colegio de Ingenieros de Montes Calle Cristóbal Bordiú, 19 28003 Madrid Phone +34 915 34 60 05 [email protected] Depósito Legal: TF 638-2014 ISBN: 978-84-617-1377-6 590 pp. ; 24 cm. 1 Ed: september, 2014 This work has been developed in the framework of the RECLAND Project. It has been funded by the European Union under the Lifelong Learning Programme, Erasmus Programme: Erasmus Multilateral Projects, 526746-LLP-1-2012-1-ES-ERASMUS-EM- CR, MSc Programme in Climate Change and Restoration of Degraded Land. How to cite this book; Arraiza, M.P., Santamarta, J.C., Ioras, F., García-Rodríguez, J.L., Abrudan, I.V., Kor- jus, H., Borála, G. (ed.) (2014). Climate Change and Restoration of Degraded Land. Madrid:Colegio de Ingenieros de Montes. Designed by Alba Fuentes Porto This book was peer-reviewed Contents CHAPTER 1 INTRODUCTION TO CLIMATE CHANGE AND LAND DEGRADATION ���������������������������������15 1 Introduction����������������������������������������������������������������������������������������������������������������������������
    [Show full text]
  • Hungarian Geographical Bulletin 61 (4) (2012) 317–325
    Hungarian Geographical Bulletin 61 (4) (2012) 317–325. Water temperatures of the Danube and Tisza Rivers in Hungary G LOVÁSZ1 Abstract Based on a 60-year long hydrological observation series from the Hungarian Hydrological Service (between 1951 and 2010), the monthly mean water temperatures of both largest rivers in the Carpathian Basin, the Danube and the Tisza, important for a range of practical considerations, are studied. The monthly extremes in water temperatures are explained by the diff erent climatic conditions in the drainage basins of the rivers: the Danube basin up- stream its entrance to Hungarian territory with a marked Atlantic and the Tisza basin with a strong continental character. Changes are followed along the Hungarian stream sections. Trends in water temperature change are established and interpretations are sought with consideration to the climate change trends predicted by climatologists for Hungary. The trends are more clearly manifested for the Danube catchment than for the Tisza catchment. Within the outlined overall trends, positive and negative singularities are also identifi ed for the coldest and ho est months and their occurrence is also analysed in regional contrast. Keywords: water temperature, air masses, climate change, singularities Introduction In the Hungarian literature analyses of river water temperatures fi rst appeared in the second half of the 19th century and included data from the observations on the Danube (G, G. 1866). In the early 20th century observations on the water temperature of the Tisza River were also published (P, D. 1905). In the mid-20th century a synthesis based on a 5-year time series of observations on the temperature conditions of standing waters and streams in Hungary (L, W.
    [Show full text]