@article{MTMT:34819318,
	title = {A numerical investigation of aerosol effect on cloud microphysics in an idealized tropical cyclone using the WRF piggybacking framework},
	url = {https://m2.mtmt.hu/api/publication/34819318},
	author = {Deng, L. and Xue, L. and Huang, W. and Wu, W. and Thompson, G. and Gao, W. and Sarkadi, Noémi and Geresdi, István},
	doi = {10.1016/j.atmosres.2024.107422},
	journal-iso = {ATMOS RES},
	journal = {ATMOSPHERIC RESEARCH},
	volume = {304},
	unique-id = {34819318},
	issn = {0169-8095},
	year = {2024},
	eissn = {1873-2895},
	orcid-numbers = {Sarkadi, Noémi/0000-0002-2370-8621; Geresdi, István/0000-0002-3160-7900}
}

@article{MTMT:34766498,
	title = {Sediment dredging assessment of the Mrica Banjarnegara hydroelectric reservoir based on technical and economic aspects},
	url = {https://m2.mtmt.hu/api/publication/34766498},
	author = {Waluyo, G and Laksono, Fx Anjar Tri and Zaenurrohman, J A and Mishra, M and Piranti, A S and Kovács, János},
	doi = {10.1080/10402381.2024.2319590},
	journal-iso = {LAKE RESERV MANAGE},
	journal = {LAKE AND RESERVOIR MANAGEMENT},
	unique-id = {34766498},
	issn = {1040-2381},
	year = {2024},
	eissn = {0743-8141},
	orcid-numbers = {Laksono, Fx Anjar Tri/0000-0002-6061-6136; Kovács, János/0000-0001-7742-5515}
}

@article{MTMT:34764189,
	title = {Age, Kinematic and Thermal Constraints of Syn‐Orogenic Low‐Temperature Deformation Events: Insights From Thermochronology and Structural Data of the Nekézseny Thrust (Alpine‐Carpathian‐Dinaric Area)},
	url = {https://m2.mtmt.hu/api/publication/34764189},
	author = {Oravecz, Éva and Benkó, Zsolt and Arató, Róbert and Dunkl, István and Héja, G and Kövér, Szilvia and Németh, Tibor and Fodor, László},
	doi = {10.1029/2023TC008189},
	journal-iso = {TECTONICS},
	journal = {TECTONICS},
	volume = {43},
	unique-id = {34764189},
	issn = {0278-7407},
	abstract = {Unraveling the age and kinematics of low temperature deformation events is crucial in understanding the late‐stage evolution of orogens. However, accurate age constraints can often be challenging to obtain due to unideal outcrop conditions, large sedimentary hiatuses or the lack of well‐defined thermal events. In this study, we show on the example of the Nekézseny Thrust, a poorly exposed late orogenic thrust in the southern Western Carpathians, that a combined approach of structural analysis and multi‐method thermochronology can provide the necessary temporal, kinematic and thermal constraints for a detailed reconstruction of the deformation history. While structural mapping revealed that the Late Cretaceous Uppony Gosau Basin in the footwall of the Nekézseny Thrust underwent a significant post‐Campanian and pre‐Miocene shortening, K/Ar dating of fault gouge samples from the main fault zone constrained the primary thrusting event to the Maastrichtian. Based on the acquired apatite fission‐track and (U‐Th)/He ages, subsequent heating of the Upper Cretaceous sediments due to tectonic burial was limited to 75–100°C, followed by deformation‐related and gradual cooling between the Eocene and Early Miocene. Considering the reconstructed deformation history, as well as the large‐scale tectonic affinity of the displaced units in its footwall and hanging wall, the Nekézseny Thrust is a far‐traveled (ca. 600 km) segment of the Late Cretaceous Alps‐Dinarides contact zone, whose development was linked to the switch from lower plate to upper plate position with respect to the Sava Zone and Alpine Tethys sutures, respectively.},
	year = {2024},
	eissn = {1944-9194},
	orcid-numbers = {Kövér, Szilvia/0000-0002-6736-4226; Németh, Tibor/0000-0002-1836-6006}
}

@article{MTMT:34758659,
	title = {Numerical prediction of fog: A novel parameterization for droplet formation},
	url = {https://m2.mtmt.hu/api/publication/34758659},
	author = {Peterka, András and Thompson, Gregory and Geresdi, István},
	doi = {10.1002/qj.4704},
	journal-iso = {Q J ROY METEOR SOC},
	journal = {QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY},
	unique-id = {34758659},
	issn = {0035-9009},
	abstract = {Abstract A novel aerosol activation scheme was developed and implemented into the WRF Thompson?Eidhammer Aerosol-Aware microphysical module. While in most of the numerical weather prediction (NWP) models the activation is based on updraft velocity, even in the fog, the new parameterization considers the local rate of cooling and water vapor flux in the evaluation of the aerosol activation rate. In addition, diagnostic variables are added to evaluate the visibility reduction due to formation of haze droplets. The impact of changing the activation scheme is demonstrated by a case study of a well-observed fog event. Data observed during the fog event campaign at Budapest and observed at standard meteorological stations are compared with the output of the numerical model. The results are summarized as follows: (i) the inhomogeneous spatial and temporal distribution of the number concentration of droplets is an inherent characteristic of the new parameterization scheme. (ii) Compared to the prior parameterization based on updraft velocity, the new parameterization scheme increases the number concentration of the droplets significantly, especially at the top of the fog. As a consequence, it reduces the downward short-wave radiation flux prolonging the lifetime of the fog by about 30?60?min. (iii) Analyses reveal that earlier dissipation of the fog comparing to the observed data cannot be explained only by overestimation of the downward short-wave radiation flux. (iv) The new method is able to evaluate the reduction of visibility due to haze.},
	keywords = {Modeling; fog; WRF; microphysics},
	year = {2024},
	eissn = {1477-870X},
	orcid-numbers = {Geresdi, István/0000-0002-3160-7900}
}

@article{MTMT:34746792,
	title = {Marine Strontium Isotope Evolution at the Triassic‐Jurassic Transition Links Transient Changes in Continental Weathering to Volcanism of the Central Atlantic Magmatic Province},
	url = {https://m2.mtmt.hu/api/publication/34746792},
	author = {Heszler, Bernát and Katchinoff, Joachim and Palcsu, László and Horváth, Anikó and Vallner, Zsolt and Kovács, Emma Blanka and Planavsky, Noah and Pálfy, József},
	doi = {10.1029/2024GC011464},
	journal-iso = {GEOCHEM GEOPHY GEOSY},
	journal = {GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS},
	volume = {25},
	unique-id = {34746792},
	abstract = {The end‐Triassic extinction (ETE) is one of the most severe biotic crises in the Phanerozoic. This event was synchronous with volcanism of the Central Atlantic Magmatic Province (CAMP), the ultimate cause of the extinction and related environmental perturbations. However, the continental weathering response to CAMP‐induced warming remains poorly constrained. Strontium isotope stratigraphy is a powerful correlation tool that can also provide insights into the changes in weathering regime, but the scarcity of 87 Sr/ 86 Sr data across the Triassic‐Jurassic boundary (TJB) hindered the use of this method. Here we present new high‐resolution 87 Sr/ 86 Sr data from bulk carbonates at Csővár, a continuous marine section that spans 2.5 Myrs across the TJB. We document a continuing decrease in 87 Sr/ 86 Sr ratio from the late Rhaetian to the ETE, terminated by a 300 kyr interval of a flat trend and followed by a transient increase in the early Hettangian that levels off. We suggest that the first in the series of perturbations is linked to the influx of non‐radiogenic Sr from the weathering of freshly erupted CAMP basalts, leading to a delay in the radiogenic continental weathering response. The subsequent rise in 87 Sr/ 86 Sr after the TJB is explained by intensified continental crustal weathering from elevated CO 2 levels and reduced mantle‐derived Sr flux. Using Sr flux modeling, we also find support for such multiphase, prolonged continental weathering scenarios. Aggregating the new data set with published records employing an astrochronological age model results in a highly resolved Sr isotope reference curve for an 8.5 Myr interval around the TJB.},
	year = {2024},
	eissn = {1525-2027},
	orcid-numbers = {Katchinoff, Joachim/0000-0003-1286-8344; Planavsky, Noah/0000-0001-5849-8508; Pálfy, József/0000-0001-9686-1849}
}

@article{MTMT:34734182,
	title = {Combined use of HYSPLIT model and MODIS aerosols optical depth to study the spatiotemporal circulation patterns of Saharan dust events over Central Europe},
	url = {https://m2.mtmt.hu/api/publication/34734182},
	author = {Gammoudi, Nadia and Kovács, János and Gresina, Fruzsina and Varga, György},
	doi = {10.1016/j.aeolia.2024.100899},
	journal-iso = {AEOLIAN RES},
	journal = {AEOLIAN RESEARCH},
	volume = {67-69},
	unique-id = {34734182},
	issn = {1875-9637},
	year = {2024},
	eissn = {2212-1684},
	orcid-numbers = {Kovács, János/0000-0001-7742-5515; Gresina, Fruzsina/0000-0003-2187-6864; Varga, György/0000-0003-4784-6372}
}

@article{MTMT:34643332,
	title = {Iron-Bearing Minerals in the Boda Claystone Formation: Correspondences with Stages of Evolution Revealed by Mössbauer Spectroscopy},
	url = {https://m2.mtmt.hu/api/publication/34643332},
	author = {Lázár, Károly and Máthé, Z and Németh, Tibor and Kovácsné Kis, Viktória and Stichleutner, Sándor and Kovács, Ivett},
	doi = {10.3390/min14020196},
	journal-iso = {MINERALS-BASEL},
	journal = {MINERALS},
	volume = {14},
	unique-id = {34643332},
	year = {2024},
	eissn = {2075-163X},
	orcid-numbers = {Németh, Tibor/0000-0002-1836-6006; Kovács, Ivett/0000-0001-7015-7909}
}

@article{MTMT:34576792,
	title = {Exploring the Mediterranean tsunami research landscape: scientometric insights and future prospects},
	url = {https://m2.mtmt.hu/api/publication/34576792},
	author = {Laksono, Fx Anjar Tri and Mishra, Manoranjan and Mulyana, Budi and Kovács, János},
	doi = {10.1186/s40677-024-00269-6},
	journal-iso = {GEOENVIRONMENTAL DISASTERS},
	journal = {GEOENVIRONMENTAL DISASTERS},
	volume = {11},
	unique-id = {34576792},
	year = {2024},
	eissn = {2197-8670},
	orcid-numbers = {Laksono, Fx Anjar Tri/0000-0002-6061-6136; Kovács, János/0000-0001-7742-5515}
}

@misc{MTMT:34376925,
	title = {The Legal Governance of Geothermal Energy in Europe: A Historical Review and an Indicator Analysis},
	url = {https://m2.mtmt.hu/api/publication/34376925},
	author = {Tamas, Hamor and Rim, Khedri and Katalin, Bódis and Anikó, Tóth and Hámorné, Vidó Mária},
	doi = {10.2139/ssrn.4611193},
	unique-id = {34376925},
	year = {2024}
}

@article{MTMT:34376505,
	title = {Geology in legislation making: Past experience, and future opportunities in Europe},
	url = {https://m2.mtmt.hu/api/publication/34376505},
	author = {Tamás, Hámor and Pavlos, Tyrologou and Hámorné, Vidó Mária},
	doi = {10.5281/zenodo.10304868},
	journal-iso = {EUR GEOL},
	journal = {EUROPEAN GEOLOGIST},
	unique-id = {34376505},
	issn = {1028-267X},
	keywords = {EU legislation; Good Governance; Underground space; role of geologists},
	year = {2024}
}