TY - JOUR AU - Magyari, Enikő Katalin AU - Raczky, Pál AU - Merkl, Máté AU - Pálfi, Ivett AU - Darabos, Gabriella AU - Hajnalova, M AU - Moskal-Hoyo, M TI - Review on vegetation, landscape and climate changes in the Carpathian Basin during the Neolithic and Chalcolithic period JF - VEGETATION HISTORY AND ARCHAEOBOTANY J2 - VEG HIST ARCHAEOBOT PY - 2024 SN - 0939-6314 DO - 10.1007/s00334-024-00986-w UR - https://m2.mtmt.hu/api/publication/34568108 ID - 34568108 N1 - ELKH-MTM-ELTE Research Group for Palaeontology, Ludovika Tér 2, Budapest, 1083, Hungary Department of Environmental and Landscape Geography, Eötvös Loránd University, Pázmány Péter Stny 1/C, Budapest, 1117, Hungary Institute of Archaeological Sciences, Eötvös Loránd University, Múzeum Krt. 4/B, Budapest, 1088, Hungary AB - The Neolithic and Copper Age (CA) of Hungary (6000–2800 cal bc ) represents a meticulous construction of settlement structure, material culture, arable farming and herding techniques with at least one, but likely several reappearing population movements that brought in innovations and possibly contributed to the societal changes in this period. The last couple of decades witnessed a considerable progress in the study of concurrent vegetation, climate and landscape management changes particularly via the increased number of high-resolution pollen records, archaeobotanical and archaeological investigations, coupled with stable isotope analyses of the charred cereal assemblages. In this review we synthetize the results of these research projects and demonstrate that the Neolithic and CA landscapes of Hungary were characterised by mixed oak forest communities, and in the territory of Hungary thermophilous steppe oak forests were present in the lowland landscape that were the principal choice of early farmers represented by the Körös-Starčevo-Criş cultures. Climate modelling and climate reconstruction from these regions indicate higher than preindustrial summer mean temperatures and higher than modern summer rainfall. We demonstrate that Linear Pottery Culture was the first culture that technologically advanced to clear larger plots of land for crop cultivation purposes. The first large scale and landscape level clearance is discernible in the Hungarian pollen records in the Late Neolithic period, when population size likely reached its Neolithic maximum, both in the lowlands and the surrounding mid-mountains. LA - English DB - MTMT ER - TY - JOUR AU - Decaulne, Armelle AU - Rachita, Ionela-Georgiana AU - Kholiavchuk, Dariia AU - Pop, Olimpiu AU - Holobaca, Iulian Horia AU - Ridush, Oles AU - Ridush, Bogdan AU - Horváth, Csaba TI - Patterns of snow avalanche activity during the last century in Chornohora Range (Eastern Carpathians, Ukraine): Tree-ring reconstruction coupled with synoptic conditions analysis JF - CATENA J2 - CATENA VL - 233 PY - 2023 PG - 15 SN - 0341-8162 DO - 10.1016/j.catena.2023.107523 UR - https://m2.mtmt.hu/api/publication/34252361 ID - 34252361 AB - This contribution presents a first comprehensive study of snow-avalanche activity in three paths of the Chornohora range, located in southwestern Ukraine, based on historical chronicles and dendrochronology. The results are combined with a statistical analysis of meteorological drivers conducive to snow-avalanche release. While the written chronicles last from 1966 to 2015, the dendrological approach offers results back to the end of the 19th century; however, if the information covers a longer time-lapse, it loses accuracy as only the winter scale is documented through the analysis of tree-ring growing patterns. Weather data highlight the synoptic scenarios over some of the avalanche events that have been recognized as major, as the three paths were concerned: 1947-48, 1976-77, 1993-94, 1998-99, 2001-02. Three weather variables are highlighted: the formation of a consistent snow cover as early as November; positive mean daily temperature in April commands late winter avalanches if the snow cover is maintained with recurrent snow fall. Temperature warming and precipitation increase are also noted on the climatological trends in Chornohora range; however, the winter temperature remains stable, and the snow-avalanche regime might not be affected in the area in the near future. LA - English DB - MTMT ER - TY - JOUR AU - Ramos-Román, MJ. AU - De Jonge, C AU - Magyari, Enikő Katalin AU - Veres, D AU - Ilvonen, L AU - Develle, AL AU - Seppä, H TI - Lipid biomarker (brGDGT)- and pollen-based reconstruction of temperature change during the Middle to Late Holocene transition in the Carpathians JF - GLOBAL AND PLANETARY CHANGE J2 - GLOBAL PLANET CHANGE VL - 215 PY - 2022 SN - 0921-8181 DO - 10.1016/j.gloplacha.2022.103859 UR - https://m2.mtmt.hu/api/publication/32871525 ID - 32871525 N1 - Department of Geography and Geosciences, Faculty of Science, University of Helsinki, Helsinki, Finland ETH Zürich, Geological Institute, Zürich, 8092, Switzerland MTA-MTM-ELTE Research Group for Paleontology, Department of Environmental and Landscape Geography, Eötvös Loránd University, Pázmány Péter stny. 1/C, Budapest, 1117, Hungary Institute of Speleology, Romanian Academy, Clinicilor 5, Cluj-Napoca, 400006, Romania Organismal an Evolutionary Biology Research Program, Research Centre for Ecological Change, University of Helsinki, Finland Université Grenoble Alpes, Université Savoie Mont Blanc, CNRS, EDYTEM, Le Bourget du Lac, France Export Date: 10 August 2022 CODEN: GPCHE Correspondence Address: Ramos-Román, M.J.; Department of Geography and Geosciences, Finland; email: mariajose.ramosroman@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Fu, Y AU - Hao, Q AU - Peng, S AU - Markovic, SB AU - Gao, X AU - Han, L AU - Wu, X AU - Namier, N AU - Zhang, W AU - Gavrilov, MB AU - Markovic, R AU - Guo, Z TI - Clay mineralogy of the Stari Slankamen (Serbia) loess-paleosol sequence during the last glacial cycle — Implications for dust provenance and interglacial climate JF - QUATERNARY SCIENCE REVIEWS J2 - QUATERN SCI REV VL - 263 PY - 2021 PG - 14 SN - 0277-3791 DO - 10.1016/j.quascirev.2021.106990 UR - https://m2.mtmt.hu/api/publication/32057844 ID - 32057844 N1 - Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, 100029, China University of Chinese Academy of Sciences, Beijing, 100049, China Center for Excellence in Life and Paleoenvironment, Chinese Academy of Sciences, Beijing, 100044, China Key Laboratory of Tourism and Resources Environment in Universities of Shandong, Taishan University, Taian, 271021, China Department of Physical Geography, Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovića 3, Novi Sad, 21000, Serbia Export Date: 25 May 2022 CODEN: QSRED Correspondence Address: Hao, Q.; Key Laboratory of Cenozoic Geology and Environment, China; email: haoqz@mail.iggcas.ac.cn Correspondence Address: Peng, S.; Key Laboratory of Tourism and Resources Environment in Universities of Shandong, China; email: pengshuzhen@tsu.edu.cn LA - English DB - MTMT ER - TY - JOUR AU - Tosic, Ivana AU - Putnikovic, Suzana TI - Influence of the East Atlantic/West Russia pattern on precipitation over Serbia JF - THEORETICAL AND APPLIED CLIMATOLOGY J2 - THEORET APPL CLIMAT PY - 2021 PG - 10 SN - 0177-798X DO - 10.1007/s00704-021-03777-9 UR - https://m2.mtmt.hu/api/publication/32291436 ID - 32291436 N1 - Funding Agency and Grant Number: Serbian Ministry of Science, Education and Technological Development [451-03-9/2021-14/200162] Funding text: This research was supported by the Serbian Ministry of Science, Education and Technological Development, under grant No. 451-03-9/2021-14/200162. AB - It is widely known that the North Atlantic Oscillation (NAO) has an influence on precipitation in Europe. There are other modes of variability such as the East Atlantic (EA) pattern, the East Atlantic/West Russia pattern (EA/WR), the Scandinavia pattern (SCAND), and the Pacific/North American pattern (PNA), which characterize the climate variability in the Northern Hemisphere. In this study, the influence of the EA/WR pattern on precipitation over Europe is examined, with a focus on Serbia. In addition, we explore the combined effects of positive and negative phases of the NAO and EA pattern with the EA/WR pattern, on precipitation over Europe and Serbia. Precipitation data are obtained from the Global Precipitation Climatology Centre (GPCC) and 15 stations from the national observational network in Serbia. Precipitation anomalies have been explored in relation to positive and negative phases of the EA/WR pattern using the monthly GPCC dataset. For the negative (positive) EA/WR phase, positive (negative) precipitation anomalies prevail over the Balkan Peninsula and central Mediterranean in January, February, May, and November, while a negative (positive) one dominates in March, April, September, and during the summer months. There is a strong positive (negative) signal over Portugal in October and over Greece and the Ionian Sea in December, for the positive (negative) EA/WR phase. The precipitation anomalies associated with the negative phase of the EA/WR pattern reflect above (up to 6 mm) average precipitation over Serbia. The positive phase of the EA/WR pattern caused precipitation anomalies below (up to - 8 mm) average precipitation over Serbia. We find that the NAO and EA patterns enhance the influence of the EA/WR pattern on precipitation changes over Serbia. High positive values of precipitation anomalies existed over Serbia for the negative phases of the EA/WR pattern and NAO (up to 12 mm), and EA pattern (up to 10 mm). Negative precipitation anomalies (up to - 12 mm) over Serbia are caused by the positive phase of the EA/WR pattern in combination with the positive phases of the NAO and EA pattern. LA - English DB - MTMT ER - TY - JOUR AU - Ilie, Nicolae AU - Axinte, Aurel-Danut AU - Apostol, Liviu TI - 'HESS-BREZOWSKY' ATMOSPHERIC CLASSIFICATION TYPES ASSOCIATED WITH NAO AND AO PHASES IN THE NORTHERN PART OF MOLDOVA JF - PRESENT ENVIRONMENT AND SUSTAINABLE DEVELOPMENT J2 - PRESENT ENVIRONMENT AND SUSTAINABLE DEVELOPMENT VL - 14 PY - 2020 IS - 2 SP - 176 EP - 191 PG - 16 SN - 1843-5971 DO - 10.15551/pesd2020142014 UR - https://m2.mtmt.hu/api/publication/34021488 ID - 34021488 N1 - Funding Agency and Grant Number: European Social Fund, through Operational Programme Human Capital 2014-2020, project [POCU/380/6/13/123623] Funding text: This work was co-funded by the European Social Fund, through Operational Programme Human Capital 2014-2020, project number POCU/380/6/13/123623, project title 'PhD Students and Postdoctoral Researchers Prepared for the Labour Market' AB - The North Atlantic Oscillation (NAO) and that Artic (AO), respectively, are by considerable importance to make the short-time weather forecast (until three days), followed by those of middle range and long time (until two weeks). To analyzing the 'Hess-Brezowsky' weather patterns associated with the NAO and AO during 19 years (2000 to 2018), has highlighted some aspects over the weather kind in the north part of Moldova. The zonal air-masses' movements such as northwestern and western, both of them into the anti-cyclonic and cyclonic regime, were deployed in a predominately positive phase of NAO and AO. In the case of NWA type, NAO was 0.17 and AO 0.60, and for WA, NAO was 0.12 and AO 0.71. From NWZ, the NAO shown values around of 0.03 and AO 0.08. Exceptionally, NAO was into a negative phase in the case of WZ, with a value of around -0.13. Instead, for WZ, the AO was positive, with a yearly average of 0.08. Such air-masses movements are associated with a mild weather pattern, especially during the wintertime. Then, over the southern part of Europe, it's set up the 'Omega' ridge. In doing so, the amounts of the precipitations are low at the studied area's level. By a more significant interest is the southwesterly air-masses movement into a cyclonic regime (SWZ) who shown values of NAO of -0.16 and 00.26 for AO. Also, negative values for NAO were in the case of TRM (Trough over Central Europe), with -0.04 and HNFZ (High over Scandinavia-Iceland, Trough over Central Europe), with -0.64. For the same synoptically contexts (TRM and HNFZ), the AO was of -0.23, respectively, -1.31. Associated with the negative phases of NAO and AO, the planetary waves have shown an undulatory tendency. In such a case, there are development areas with extreme weather. For the studied region, the negative phases of NAO and AO were associated with severe weather events, such as blizzards, storms, and floods. LA - English DB - MTMT ER - TY - JOUR AU - Maheras, P AU - Tolika, K AU - Tegoulias, I AU - Anagnostopoulou, C AU - Szpirosz, K AU - Károssy, Csaba AU - Makra, László TI - Comparison of an Automated Classification System with an Empirical Classification of Circulation Patterns over the Pannonian Basin, Central Europe. JF - METEOROLOGY AND ATMOSPHERIC PHYSICS J2 - METEOROL ATMOS PHYS VL - 131 PY - 2019 IS - 4 SP - 739 EP - 751 PG - 13 SN - 0177-7971 DO - 10.1007/s00703-018-0601-x UR - https://m2.mtmt.hu/api/publication/3354021 ID - 3354021 AB - The aim of the study is to compare the performance of the two classification methods, based on the atmospheric circulation types over the Pannonian basin in Central Europe. Moreover, relationships including seasonal occurrences and correlation coefficients, as well as comparative diagrams of the seasonal occurrences of the circulation types of the two classification systems are presented. When comparing of the automated (objective) and empirical (subjective) classification methods, it was found that the frequency of the empirical anticyclonic (cyclonic) types is much higher (lower) than that of the automated anticyclonic (cyclonic) types both on an annual and seasonal basis. The highest and statistically significant correlations between the circulation types of the two classification systems, as well as those between the cumulated seasonal anticyclonic and cyclonic types occur in winter for both classifications, since the weather-influencing effect of the atmospheric circulation in this season is the most prevalent. Precipitation amounts in Budapest display a decreasing trend in accordance with the decrease in the occurrence of the automated cyclonic types. In contrast, the occurrence of the empirical cyclonic types displays an increasing trend. There occur types in a given classification that are usually accompanied by high ratios of certain types in the other classification. LA - English DB - MTMT ER - TY - JOUR AU - Szpirosz, Klicász AU - Maheras, Panagiotis AU - Tolika, Konstantina AU - Tegoulias, Ioannis AU - Anagnostopoulou, Christina AU - Károssy, Csaba AU - Makra, László TI - Egy automata és egy empirikus légcirkulációs osztályozási rendszer összehasonlító elemzése a kárpát-medencére JF - FÖLDRAJZI KÖZLEMÉNYEK J2 - FÖLDRAJZI KÖZLEMÉNYEK VL - 143 PY - 2019 IS - 1 SP - 71 EP - 88 PG - 18 SN - 0015-5411 DO - 10.32643/fk.143.1.6 UR - https://m2.mtmt.hu/api/publication/30624047 ID - 30624047 LA - Hungarian DB - MTMT ER - TY - JOUR AU - Maheras, P AU - Tolika, K AU - Anagnostopoulou, Ch AU - Makra, László AU - Szpirosz, K AU - Károssy, Cs TI - Relationship between mean and extreme precipitation and circulation types over Hungary JF - INTERNATIONAL JOURNAL OF CLIMATOLOGY J2 - INT J CLIMATOL VL - 38 PY - 2018 IS - 12 SP - 4518 EP - 4532 PG - 15 SN - 0899-8418 DO - 10.1002/joc.5684 UR - https://m2.mtmt.hu/api/publication/3409009 ID - 3409009 LA - English DB - MTMT ER - TY - JOUR AU - Pál, Ilona AU - Buczkó, Krisztina AU - Vincze, Ildikó AU - Finsinger, Walter AU - Braun, Mihály AU - Biró, Tamás AU - Magyari, Enikő Katalin TI - Terrestrial and aquatic ecosystem responses to early Holocene rapid climate change (RCC) events in the South Carpathian Mountains, Romania JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 477 PY - 2018 SP - 79 EP - 93 PG - 15 SN - 1040-6182 DO - 10.1016/j.quaint.2016.11.015 UR - https://m2.mtmt.hu/api/publication/3196733 ID - 3196733 N1 - Department of Physical and Applied Geology, Eötvös Loránd University, Pázmány Péter stny. 1/C, Budapest, H-1117, Hungary MTA-MTM-ELTE Research Group for Paleontology, Pázmány Péter stny. 1/C, Budapest, H-1117, Hungary Hungarian Natural History Museum, P.O. Box 222, Budapest, H-1476, Hungary Palaeoecology, Institut des Sciences de l'Evolution (UMR 5554 CNRS/UM/IRD/EPHE), Place E. Bataillon, Montpellier, 34095, France Department of Inorganic and Analytical Chemistry, University of Debrecen, P.O. Box 21, Debrecen, H-4010, Hungary Hungarian Academy of Sciences, Research Center for Humanities, Institute of Archaeology, Úri u. 49, Budapest, H-1014, Hungary Export Date: 15 October 2019 Correspondence Address: Pál, I.; Department of Physical and Applied Geology, Eötvös Loránd University, Pázmány Péter stny. 1/C, Hungary; email: palilona@caesar.elte.hu AB - Abstract As demonstrated by an increasing number of palaeoclimatic and palaeoecological studies, rapid climate change events (RCCs) occurred frequently in the Holocene and their timing correlates well in the European records. Changes in vegetation composition and environmental conditions were significant during these RCC events. In this study we use high resolution pollen, stomata, micro- and macrocharcoal, macrofossil, siliceous algae, biogenic silica and organic content analyses from two alpine lake sediments (Lake Brazi, 1740 m a.s.l.; Lake Gales, 1990 m a.s.l.) in the Retezat Mts, South Carpathian Mountains, Romania. Our aim is to study ecosystem responses to RCCs between 12,000 and 7000 cal yr BP using high-resolution proxy analyses of the relevant sediment sections. We detected several significant changes in the terrestrial vegetation composition and aquatic ecosystems in case of both lakes. Complex ecosystem responses were found in connection with the early Holocene RCC intervals. Most prominently, the 10.2 ka climatic change likely fostered the extinction of Larix decidua from the shore of Lake Brazi, while climatic change during the 8.2 ka event facilitated the establishment of Carpinus betulus in the lower deciduous mixed oak forests, due to decreasing growing season temperatures, frequent summer droughts and associated recurrent fire events. Taken together, most of the significant pollen compositional changes reflected the periodic spread of pioneer deciduous tree taxa (mainly Fraxinus excelsior and Corylus avellana) during the early Holocene RCCs. In all cases, this change was connectable to increased regional fire activity and the temporary increase of herbs. The most significant change in the lake-ecosystems was often the short-lived spread of various planktonic diatom species, mainly the members of genus Aulacoseira. Sudden appearance and large-scale percentage increase of these taxa suggested higher water-depth and/or intensified water turbulence. LA - English DB - MTMT ER - TY - JOUR AU - LEHOCZKY, A AU - Templ, Barbara Andrea AU - Pongrácz, Rita AU - SZENTKIRÁLYI, F TI - TESTING PLANT PHENOPHASE AS PROXY: SENSITIVITY ANALYSIS OF FIRST FLOWERING DATA FROM THE 19TH CENTURY JF - APPLIED ECOLOGY AND ENVIRONMENTAL RESEARCH J2 - APPL ECOL ENV RES VL - 14 PY - 2016 IS - 2 SP - 213 EP - 233 PG - 21 SN - 1589-1623 DO - 10.15666/aeer/1402_213233 UR - https://m2.mtmt.hu/api/publication/3045521 ID - 3045521 N1 - Cited By :1 Export Date: 10 January 2023 Correspondence Address: Lehoczky, A.; Centre for Climate Change, Campus de les Terres de l'Ebre, Avinguda Remolins, 13-15, Spain; email: annamaria.lehoczky@urv.cat LA - English DB - MTMT ER - TY - JOUR AU - Templ, Barbara Andrea AU - Vincze, E AU - Czúcz, Bálint TI - Flowering phenological changes in relation to climate change in Hungary JF - INTERNATIONAL JOURNAL OF BIOMETEOROLOGY J2 - INT J BIOMETEOROL VL - 60 PY - 2016 IS - 9 SP - 1347 EP - 1356 PG - 10 SN - 0020-7128 DO - 10.1007/s00484-015-1128-1 UR - https://m2.mtmt.hu/api/publication/3009250 ID - 3009250 N1 - Cited By :37 Export Date: 17 October 2022 CODEN: IJBMA Correspondence Address: Szabó, B.; Institute of Ecology and Botany, Alkotmány út 2-4, Hungary; email: barbara.szabo.elte@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Hoy, Andreas AU - Schucknecht, Anne AU - Sepp, Mait AU - Matschullat, Jorg TI - Large-scale synoptic types and their impact on European precipitation JF - THEORETICAL AND APPLIED CLIMATOLOGY J2 - THEORET APPL CLIMAT VL - 116 PY - 2014 IS - 1-2 SP - 19 EP - 35 PG - 17 SN - 0177-798X DO - 10.1007/s00704-013-0897-x UR - https://m2.mtmt.hu/api/publication/24852191 ID - 24852191 N1 - Funding Agency and Grant Number: DAAD; Estonian DORA5 programme; Estonian Science Foundation [7526] Funding text: This work was supported by a DAAD doctoral scholarship for short-term research in Estonia, the Estonian DORA5 programme (EU supported), and the Estonian Science Foundation grant no 7526. We thank Jaak Jaagus and Paul James for their comments on an earlier version of this paper. A very special thanks to Victor Lagun and his colleagues at AARI in St. Petersburg, Russia for the VGc data and to Paul James for the SVGc data. We acknowledge the E-OBS dataset from the EU-FP6 project ENSEMBLES (http://ensembles-eu.metoffice.com) and the data providers in the ECA&D project (http://www.ecad.eu). LA - English DB - MTMT ER - TY - JOUR AU - Demény, Attila AU - Czuppon, György AU - Siklósy, Zoltán AU - Leél-Őssy, Szabolcs AU - Lin, K AU - Shen, C-C AU - Gulyás, Krisztina TI - Mid-Holocene climate conditions and moisture source variations based on stable H, C and O isotope compositions of speleothems in Hungary JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 293 PY - 2013 SP - 150 EP - 156 PG - 7 SN - 1040-6182 DO - 10.1016/j.quaint.2012.05.035 UR - https://m2.mtmt.hu/api/publication/1985862 ID - 1985862 N1 - Funding Agency and Grant Number: Hungarian Scientific Research Fund [OTKA 49713, OTKA 68343]; NSC [99-2611-M-002-006, 99-2628-M-002-012, NSC100-3113-M-002-002] Funding text: The study was financially supported by the Hungarian Scientific Research Fund (OTKA 49713 and OTKA 68343). The mass spectrometry facility of the Institute for Geochemical Research, Budapest, was supported by the National Office for Research and Technology (GVOP-3.2.1-2004-04-0235/3.0). U-series dating at the HISPEC was supported by the NSC grants 99-2611-M-002-006 and 99-2628-M-002-012, and NSC100-3113-M-002-002 to CCS. Among those who kindly contributed to this work, the authors express their gratitude to Istvan Szenthe as he donated the stalagmite of Leany Cave to Z. S. Unpublished information and data were kindly provided by Dr. Gergely Suranyi (internal temperatures of the Leany Cave), Hedvig Nagy (internal temperatures of the Pal-volgyi Cave), Magdolna Virag (Pal-volgyi Cave environment photo and map) and Richard Kovacs (cave maps of the Leany Cave) for which the authors are deeply indebted. The paper greatly benefited from the helpful and constructive reviews of two anonymous reviewers. LA - English DB - MTMT ER - TY - JOUR AU - Magyari, Enikő Katalin AU - Demény, Attila AU - Buczkó, Krisztina AU - Kern, Zoltán AU - Vennemann, T AU - Fórizs, István AU - Vincze, Ildikó AU - Braun, Mihály AU - Kovács, István János AU - Udvardi, Beatrix AU - Veres, D TI - A 13,600-year diatom oxygen isotope record from the South Carpathians (Romania): Reflection of winter conditions and possible links with North Atlantic circulation changes JF - QUATERNARY INTERNATIONAL J2 - QUATERN INT VL - 293 PY - 2013 SP - 136 EP - 149 PG - 14 SN - 1040-6182 DO - 10.1016/j.quaint.2012.05.042 UR - https://m2.mtmt.hu/api/publication/2269081 ID - 2269081 N1 - Megjegyzés-23109790 Megjegyzés-22379662 in press LA - English DB - MTMT ER - TY - JOUR AU - Stefanescu, Victor AU - Stefan, Sabina AU - Georgescu, Florinela TI - Spatial distribution of heavy precipitation events in Romania between 1980 and 2009 JF - METEOROLOGICAL APPLICATIONS J2 - METEOROL APPL PY - 2013 SP - n/a EP - n/a SN - 1350-4827 DO - 10.1002/met.1391 UR - https://m2.mtmt.hu/api/publication/23328942 ID - 23328942 N1 - : Provider: John Wiley & Sons, Ltd : Content:text/plain; charset="UTF-8" LA - English DB - MTMT ER - TY - JOUR AU - Oláh, A.B. TI - The possibilities of decreasing the urban heat Island JF - APPLIED ECOLOGY AND ENVIRONMENTAL RESEARCH J2 - APPL ECOL ENV RES VL - 10 PY - 2012 IS - 2 SP - 173 EP - 183 PG - 11 SN - 1589-1623 DO - 10.15666/aeer/1002_173183 UR - https://m2.mtmt.hu/api/publication/34580803 ID - 34580803 N1 - Cited By :33 Export Date: 14 February 2024 Correspondence Address: OláH, A. B.; Department of Garden and Open Space Design, Villányi út 29-43, 1118 Budapest, Hungary; email: olah.andras.bela@gmail.com LA - English DB - MTMT ER - TY - JOUR AU - Oláh, András Béla TI - The Possibilities of Decreasing the Urban Heat Island JF - APPLIED ECOLOGY AND ENVIRONMENTAL RESEARCH J2 - APPL ECOL ENV RES VL - 10 PY - 2012 IS - 2 SP - 173 EP - 183 PG - 11 SN - 1589-1623 DO - 10.15666/aeer/1002_173183 UR - https://m2.mtmt.hu/api/publication/3088977 ID - 3088977 LA - English DB - MTMT ER -