@article{MTMT:34568108, title = {Review on vegetation, landscape and climate changes in the Carpathian Basin during the Neolithic and Chalcolithic period}, url = {https://m2.mtmt.hu/api/publication/34568108}, author = {Magyari, Enikő Katalin and Raczky, P and Merkl, Máté and Pálfi, Ivett and Darabos, Gabriella and Hajnalova, M and Moskal-Hoyo, M}, doi = {10.1007/s00334-024-00986-w}, journal-iso = {VEG HIST ARCHAEOBOT}, journal = {VEGETATION HISTORY AND ARCHAEOBOTANY}, unique-id = {34568108}, issn = {0939-6314}, abstract = {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.}, year = {2024}, eissn = {1617-6278}, orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Pálfi, Ivett/0000-0001-9814-3410; Darabos, Gabriella/0000-0001-8070-5630} } @article{MTMT:34252361, title = {Patterns of snow avalanche activity during the last century in Chornohora Range (Eastern Carpathians, Ukraine): Tree-ring reconstruction coupled with synoptic conditions analysis}, url = {https://m2.mtmt.hu/api/publication/34252361}, author = {Decaulne, Armelle and Rachita, Ionela-Georgiana and Kholiavchuk, Dariia and Pop, Olimpiu and Holobaca, Iulian Horia and Ridush, Oles and Ridush, Bogdan and Horváth, Csaba}, doi = {10.1016/j.catena.2023.107523}, journal-iso = {CATENA}, journal = {CATENA}, volume = {233}, unique-id = {34252361}, issn = {0341-8162}, abstract = {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.}, year = {2023}, eissn = {1872-6887}, orcid-numbers = {Kholiavchuk, Dariia/0000-0002-7489-7848; Horváth, Csaba/0000-0002-5691-2485} } @article{MTMT:32871525, title = {Lipid biomarker (brGDGT)- and pollen-based reconstruction of temperature change during the Middle to Late Holocene transition in the Carpathians}, url = {https://m2.mtmt.hu/api/publication/32871525}, author = {Ramos-Román, MJ. and De Jonge, C and Magyari, Enikő Katalin and Veres, D and Ilvonen, L and Develle, AL and Seppä, H}, doi = {10.1016/j.gloplacha.2022.103859}, journal-iso = {GLOBAL PLANET CHANGE}, journal = {GLOBAL AND PLANETARY CHANGE}, volume = {215}, unique-id = {32871525}, issn = {0921-8181}, year = {2022}, eissn = {1872-6364}, orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937} } @article{MTMT:32057844, title = {Clay mineralogy of the Stari Slankamen (Serbia) loess-paleosol sequence during the last glacial cycle — Implications for dust provenance and interglacial climate}, url = {https://m2.mtmt.hu/api/publication/32057844}, author = {Fu, Y and Hao, Q and Peng, S and Markovic, SB and Gao, X and Han, L and Wu, X and Namier, N and Zhang, W and Gavrilov, MB and Markovic, R and Guo, Z}, doi = {10.1016/j.quascirev.2021.106990}, journal-iso = {QUATERN SCI REV}, journal = {QUATERNARY SCIENCE REVIEWS}, volume = {263}, unique-id = {32057844}, issn = {0277-3791}, year = {2021}, eissn = {1873-457X} } @article{MTMT:32291436, title = {Influence of the East Atlantic/West Russia pattern on precipitation over Serbia}, url = {https://m2.mtmt.hu/api/publication/32291436}, author = {Tosic, Ivana and Putnikovic, Suzana}, doi = {10.1007/s00704-021-03777-9}, journal-iso = {THEORET APPL CLIMAT}, journal = {THEORETICAL AND APPLIED CLIMATOLOGY}, unique-id = {32291436}, issn = {0177-798X}, abstract = {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.}, year = {2021}, eissn = {1434-4483} } @article{MTMT:34021488, title = {'HESS-BREZOWSKY' ATMOSPHERIC CLASSIFICATION TYPES ASSOCIATED WITH NAO AND AO PHASES IN THE NORTHERN PART OF MOLDOVA}, url = {https://m2.mtmt.hu/api/publication/34021488}, author = {Ilie, Nicolae and Axinte, Aurel-Danut and Apostol, Liviu}, doi = {10.15551/pesd2020142014}, journal-iso = {PRESENT ENVIRONMENT AND SUSTAINABLE DEVELOPMENT}, journal = {PRESENT ENVIRONMENT AND SUSTAINABLE DEVELOPMENT}, volume = {14}, unique-id = {34021488}, issn = {1843-5971}, abstract = {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.}, keywords = {North Atlantic Oscillation; ARCTIC SEA-ICE; Arctic Oscillation; Omega ridge; Hess-Brezowsky; ATLANTIC OSCILLATION}, year = {2020}, eissn = {2284-7820}, pages = {176-191} } @article{MTMT:3354021, title = {Comparison of an Automated Classification System with an Empirical Classification of Circulation Patterns over the Pannonian Basin, Central Europe.}, url = {https://m2.mtmt.hu/api/publication/3354021}, author = {Maheras, P and Tolika, K and Tegoulias, I and Anagnostopoulou, C and Szpirosz, K and Károssy, Csaba and Makra, László}, doi = {10.1007/s00703-018-0601-x}, journal-iso = {METEOROL ATMOS PHYS}, journal = {METEOROLOGY AND ATMOSPHERIC PHYSICS}, volume = {131}, unique-id = {3354021}, issn = {0177-7971}, abstract = {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.}, year = {2019}, eissn = {1436-5065}, pages = {739-751}, orcid-numbers = {Makra, László/0000-0001-7424-8963} } @article{MTMT:30624047, title = {Egy automata és egy empirikus légcirkulációs osztályozási rendszer összehasonlító elemzése a kárpát-medencére}, url = {https://m2.mtmt.hu/api/publication/30624047}, author = {Szpirosz, Klicász and Maheras, Panagiotis and Tolika, Konstantina and Tegoulias, Ioannis and Anagnostopoulou, Christina and Károssy, Csaba and Makra, László}, doi = {10.32643/fk.143.1.6}, journal-iso = {FÖLDRAJZI KÖZLEMÉNYEK}, journal = {FÖLDRAJZI KÖZLEMÉNYEK}, volume = {143}, unique-id = {30624047}, issn = {0015-5411}, year = {2019}, pages = {71-88}, orcid-numbers = {Makra, László/0000-0001-7424-8963} } @article{MTMT:3409009, title = {Relationship between mean and extreme precipitation and circulation types over Hungary}, url = {https://m2.mtmt.hu/api/publication/3409009}, author = {Maheras, P and Tolika, K and Anagnostopoulou, Ch and Makra, László and Szpirosz, K and Károssy, Cs}, doi = {10.1002/joc.5684}, journal-iso = {INT J CLIMATOL}, journal = {INTERNATIONAL JOURNAL OF CLIMATOLOGY}, volume = {38}, unique-id = {3409009}, issn = {0899-8418}, year = {2018}, eissn = {1097-0088}, pages = {4518-4532}, orcid-numbers = {Makra, László/0000-0001-7424-8963} } @article{MTMT:3196733, title = {Terrestrial and aquatic ecosystem responses to early Holocene rapid climate change (RCC) events in the South Carpathian Mountains, Romania}, url = {https://m2.mtmt.hu/api/publication/3196733}, author = {Pál, Ilona and Buczkó, Krisztina and Vincze, Ildikó and Finsinger, Walter and Braun, Mihály and Biró, Tamás and Magyari, Enikő Katalin}, doi = {10.1016/j.quaint.2016.11.015}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {477}, unique-id = {3196733}, issn = {1040-6182}, abstract = {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.}, keywords = {POLLEN; NW ROMANIA; charcoal; THERMOHALINE CIRCULATION; diatom; LAKE-LEVEL FLUCTUATIONS; COLD EVENT; GREENLAND ICE-CORE; 8.2 event; 10.2 event; Preboreal oscillation; Preboreal oscillation; Rapid ecosystem response; CATASTROPHIC DRAINAGE; 8.2 KA; VEGETATION RESPONSES; WEST-CENTRAL EUROPE; NORTH-ATLANTIC CIRCULATION}, year = {2018}, eissn = {1873-4553}, pages = {79-93}, orcid-numbers = {Biró, Tamás/0000-0001-5198-7210; Magyari, Enikő Katalin/0000-0002-2844-8937} } @article{MTMT:3045521, title = {TESTING PLANT PHENOPHASE AS PROXY: SENSITIVITY ANALYSIS OF FIRST FLOWERING DATA FROM THE 19TH CENTURY}, url = {https://m2.mtmt.hu/api/publication/3045521}, author = {LEHOCZKY, A and Templ, Barbara Andrea and Pongrácz, Rita and SZENTKIRÁLYI, F}, doi = {10.15666/aeer/1402_213233}, journal-iso = {APPL ECOL ENV RES}, journal = {APPLIED ECOLOGY AND ENVIRONMENTAL RESEARCH}, volume = {14}, unique-id = {3045521}, issn = {1589-1623}, year = {2016}, eissn = {1785-0037}, pages = {213-233}, orcid-numbers = {Pongrácz, Rita/0000-0001-7591-7989} } @article{MTMT:3009250, title = {Flowering phenological changes in relation to climate change in Hungary}, url = {https://m2.mtmt.hu/api/publication/3009250}, author = {Templ, Barbara Andrea and Vincze, E and Czúcz, Bálint}, doi = {10.1007/s00484-015-1128-1}, journal-iso = {INT J BIOMETEOROL}, journal = {INTERNATIONAL JOURNAL OF BIOMETEOROLOGY}, volume = {60}, unique-id = {3009250}, issn = {0020-7128}, year = {2016}, eissn = {1432-1254}, pages = {1347-1356} } @article{MTMT:24852191, title = {Large-scale synoptic types and their impact on European precipitation}, url = {https://m2.mtmt.hu/api/publication/24852191}, author = {Hoy, Andreas and Schucknecht, Anne and Sepp, Mait and Matschullat, Jorg}, doi = {10.1007/s00704-013-0897-x}, journal-iso = {THEORET APPL CLIMAT}, journal = {THEORETICAL AND APPLIED CLIMATOLOGY}, volume = {116}, unique-id = {24852191}, issn = {0177-798X}, year = {2014}, eissn = {1434-4483}, pages = {19-35} } @article{MTMT:1985862, title = {Mid-Holocene climate conditions and moisture source variations based on stable H, C and O isotope compositions of speleothems in Hungary}, url = {https://m2.mtmt.hu/api/publication/1985862}, author = {Demény, Attila and Czuppon, György and Siklósy, Zoltán and Leél-Őssy, Szabolcs and Lin, K and Shen, C-C and Gulyás, Krisztina}, doi = {10.1016/j.quaint.2012.05.035}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {293}, unique-id = {1985862}, issn = {1040-6182}, keywords = {MASS-SPECTROMETRY; TEMPERATURE; Precipitation; VARIABILITY; fractionation; Oxygen Isotopes; record; Stalagmite; NORTH-ATLANTIC OSCILLATION; SCALE CHANGES}, year = {2013}, eissn = {1873-4553}, pages = {150-156}, orcid-numbers = {Demény, Attila/0000-0003-0522-9018; Czuppon, György/0000-0002-7231-6042} } @article{MTMT:2269081, title = {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}, url = {https://m2.mtmt.hu/api/publication/2269081}, author = {Magyari, Enikő Katalin and Demény, Attila and Buczkó, Krisztina and Kern, Zoltán and Vennemann, T and Fórizs, István and Vincze, Ildikó and Braun, Mihály and Kovács, István János and Udvardi, Beatrix and Veres, D}, doi = {10.1016/j.quaint.2012.05.042}, journal-iso = {QUATERN INT}, journal = {QUATERNARY INTERNATIONAL}, volume = {293}, unique-id = {2269081}, issn = {1040-6182}, keywords = {VARIABILITY; LAKE; BIOGENIC SILICA; NW ROMANIA; BASIN; SIGNALS; Holocene; CAVE; STABLE-ISOTOPE; CLIMATIC RECORD}, year = {2013}, eissn = {1873-4553}, pages = {136-149}, orcid-numbers = {Magyari, Enikő Katalin/0000-0002-2844-8937; Demény, Attila/0000-0003-0522-9018; Kern, Zoltán/0000-0003-4900-2587; Fórizs, István/0000-0003-0813-6079; Kovács, István János/0000-0002-3488-3716} } @article{MTMT:23328942, title = {Spatial distribution of heavy precipitation events in Romania between 1980 and 2009}, url = {https://m2.mtmt.hu/api/publication/23328942}, author = {Stefanescu, Victor and Stefan, Sabina and Georgescu, Florinela}, doi = {10.1002/met.1391}, journal-iso = {METEOROL APPL}, journal = {METEOROLOGICAL APPLICATIONS}, unique-id = {23328942}, issn = {1350-4827}, year = {2013}, eissn = {1469-8080}, pages = {n/a-n/a} } @article{MTMT:34580803, title = {The possibilities of decreasing the urban heat Island}, url = {https://m2.mtmt.hu/api/publication/34580803}, author = {Oláh, A.B.}, doi = {10.15666/aeer/1002_173183}, journal-iso = {APPL ECOL ENV RES}, journal = {APPLIED ECOLOGY AND ENVIRONMENTAL RESEARCH}, volume = {10}, unique-id = {34580803}, issn = {1589-1623}, year = {2012}, eissn = {1785-0037}, pages = {173-183} } @article{MTMT:3088977, title = {The Possibilities of Decreasing the Urban Heat Island}, url = {https://m2.mtmt.hu/api/publication/3088977}, author = {Oláh, András Béla}, doi = {10.15666/aeer/1002_173183}, journal-iso = {APPL ECOL ENV RES}, journal = {APPLIED ECOLOGY AND ENVIRONMENTAL RESEARCH}, volume = {10}, unique-id = {3088977}, issn = {1589-1623}, year = {2012}, eissn = {1785-0037}, pages = {173-183} }