@CONFERENCE{MTMT:30848604,
	title = {Exploring potential Late Pleistocene linkages between different geomorphological domains in the SE Carpathian Basin},
	url = {https://m2.mtmt.hu/api/publication/30848604},
	author = {Sipos, György and Urdea, P and Kiss, Tímea and Markovic, S and Ruszkiczay-Rüdiger, Zsófia and Gavrilov, M and Kern, Zoltán and Tóth, Orsolya and Bartyik, Tamás and Sümeghy, Borbála and Hernesz, Péter and Páll, Dávid Gergely},
	booktitle = {Book of Abstracts},
	unique-id = {30848604},
	year = {2018},
	pages = {196-197},
	orcid-numbers = {Sipos, György/0000-0001-6224-2361; Kiss, Tímea/0000-0002-2597-5176; Kern, Zoltán/0000-0003-4900-2587}
}

@article{MTMT:3163613,
	title = {Késő pleisztocén és holocén ártérfejlődés az Alsó-Tisza mentén},
	url = {https://m2.mtmt.hu/api/publication/3163613},
	author = {Hernesz, Péter and Kiss, Tímea},
	journal-iso = {GEOSZFÉRÁK},
	journal = {GEOSZFÉRÁK: A SZEGEDI TUDOMÁNYEGYETEM FÖLDTUDOMÁNYOK DOKTORI ISKOLÁJÁNAK EREDMÉNYEI},
	volume = {36},
	unique-id = {3163613},
	issn = {2062-2465},
	year = {2016},
	pages = {139-157},
	orcid-numbers = {Kiss, Tímea/0000-0002-2597-5176}
}

@mastersthesis{MTMT:3028749,
	title = {Késő-pleisztocén és holocén ártérfejlődés az Alsó-Tisza mentén},
	url = {https://m2.mtmt.hu/api/publication/3028749},
	isbn = {9798381051742},
	author = {Hernesz, Péter},
	doi = {10.14232/phd.2652},
	publisher = {SZTE},
	unique-id = {3028749},
	year = {2015}
}

@article{MTMT:2985975,
	title = {Ártéri szintek és paleo-medrek: ártérfejlődés az Alsó-Tisza mentén},
	url = {https://m2.mtmt.hu/api/publication/2985975},
	author = {Hernesz, Péter and Kiss, Tímea and Sipos, György},
	journal-iso = {FÖLDTANI KÖZLÖNY},
	journal = {FÖLDTANI KÖZLÖNY},
	volume = {145},
	unique-id = {2985975},
	issn = {0015-542X},
	year = {2015},
	eissn = {2559-902X},
	pages = {273-286},
	orcid-numbers = {Kiss, Tímea/0000-0002-2597-5176; Sipos, György/0000-0001-6224-2361}
}

@article{MTMT:2778316,
	title = {The evolution of the Great Hungarian Plain fluvial system - Fluvial processes in a subsiding area from the beginning of the Weichselian},
	url = {https://m2.mtmt.hu/api/publication/2778316},
	author = {Kiss, Tímea and Hernesz, Péter and Sümeghy, Borbála and Györgyövics, Katalin and Sipos, György},
	doi = {10.1016/j.quaint.2014.05.050},
	journal-iso = {QUATERN INT},
	journal = {QUATERNARY INTERNATIONAL},
	volume = {388},
	unique-id = {2778316},
	issn = {1040-6182},
	abstract = {In the Great Hungarian Plain (GHP), one of the most complex 
		fluvial systems of Europe developed through tectonic and 
		climatic factors and vegetation change. The aim of the 
		present study is to summarise these controlling factors and 
		to describe the evolution of the GHP. Special attention is 
		paid to the latest results on late Weichselian and Holocene 
		development in the Tisza River and their effects on the 
		river's largest tributary: the Maros River. Several 
		tectonically active subsiding basins existing in the GHP have 
		determined the direction of river courses and erosional-
		accumulational fluvial processes. As a result of uneven 
		subsidence, the river's flow routes have shifted frequently. 
		For example, the Danube and the Tisza shifted 80-100 km, 
		abandoning their alluvial fans where extensive aeolian 
		processes started. Upstream from the subsiding areas, 
		incision propagated headward, which resulted in the 
		development of floodplain levels and terraces. Though climate 
		and vegetation changes also simultaneously influenced the 
		rivers' hydro-morphology, channel pattern changes were found 
		just along the margin of the plain, and only meandering 
		paleo-channels remained in the center of the GHP. During dry 
		and cold periods, braided patterns appeared in the alluvial 
		fans, most likely the result of abundant sediment supply and 
		due to the inability of sparse riparian vegetation to 
		stabilise the banks effectively. Based on paleo-discharge 
		calculations, by the end of the Pleistocene the rivers of the 
		GHP produced three to eight times more discharge than they do 
		currently, and discharge levels continuously decreased during 
		the Holocene. However, due to the long length of the rivers, 
		there is a considerable time lag between the response rates 
		of the different river sections, which makes creating paleo-
		hydrological reconstructions even more difficult. © 2014 
		Elsevier Ltd and INQUA.},
	keywords = {Tisza river; Great Hungarian Plain; Paleo-hydrology; Tectonism; Paleo-direction},
	year = {2015},
	eissn = {1873-4553},
	pages = {142-155},
	orcid-numbers = {Kiss, Tímea/0000-0002-2597-5176; Sipos, György/0000-0001-6224-2361}
}

@article{MTMT:2491446,
	title = {Az Alsó-Tisza menti ártér és a Maros hordalékkúp késő-pleisztocén és holocén fejlődéstörténete},
	url = {https://m2.mtmt.hu/api/publication/2491446},
	author = {Kiss, Tímea and Sümeghy, Borbála and Hernesz, Péter and Sipos, György and Mezősi, Gábor},
	journal-iso = {FÖLDRAJZI KÖZLEMÉNYEK},
	journal = {FÖLDRAJZI KÖZLEMÉNYEK},
	volume = {137},
	unique-id = {2491446},
	issn = {0015-5411},
	year = {2013},
	pages = {269-277},
	orcid-numbers = {Kiss, Tímea/0000-0002-2597-5176; Sipos, György/0000-0001-6224-2361}
}

@article{MTMT:2491407,
	title = {A Tisza-meder partfalának vizsgálata. késő pleisztocén és holocén folyamatok az Alsó-Tiszán},
	url = {https://m2.mtmt.hu/api/publication/2491407},
	author = {Hernesz, Péter and Kiss, Tímea},
	journal-iso = {HIDROL KOZL},
	journal = {HIDROLÓGIAI KÖZLÖNY},
	volume = {93},
	unique-id = {2491407},
	issn = {0018-1323},
	year = {2013},
	eissn = {2939-8495},
	pages = {13-19},
	orcid-numbers = {Kiss, Tímea/0000-0002-2597-5176}
}

@{MTMT:2366811,
	title = {Extreme Weather and the Rivers of Hungary: Rates of Bank Retreat},
	url = {https://m2.mtmt.hu/api/publication/2366811},
	author = {Kiss, Tímea and Blanka, Viktória and Andrási, Gábor and Hernesz, Péter},
	booktitle = {Geomorphological Impacts of Extreme Weather},
	doi = {10.1007/978-94-007-6301-2_6},
	unique-id = {2366811},
	year = {2013},
	pages = {83-98},
	orcid-numbers = {Kiss, Tímea/0000-0002-2597-5176; Blanka, Viktória/0000-0001-6364-109X}
}

@article{MTMT:2203126,
	title = {Meander cores on the floodplain – the early Holocene development of the low-floodplain along the Lower Tisza Region, Hungary},
	url = {https://m2.mtmt.hu/api/publication/2203126},
	author = {Kiss, Tímea and Hernesz, Péter and Sipos, György},
	journal-iso = {J ENVIRON GEOGR},
	journal = {JOURNAL OF ENVIRONMENTAL GEOGRAPHY},
	volume = {5},
	unique-id = {2203126},
	issn = {2060-3274},
	year = {2012},
	eissn = {2060-467X},
	pages = {1-10},
	orcid-numbers = {Kiss, Tímea/0000-0002-2597-5176; Sipos, György/0000-0001-6224-2361}
}

@inbook{MTMT:2202314,
	title = {Egyensúly és érzékenység, küszöbérték és agressziós hullám: a folyó, mint tájalkotó elem rendszeralapú értelmezése},
	url = {https://m2.mtmt.hu/api/publication/2202314},
	author = {Kiss, Tímea and Sipos, György and Blanka, Viktória and Sümeghy, Borbála and Andrási, Gábor and Hernesz, Péter and Benyhe, Balázs},
	booktitle = {Táj - érték, lépték, változás},
	unique-id = {2202314},
	year = {2012},
	pages = {107-119},
	orcid-numbers = {Kiss, Tímea/0000-0002-2597-5176; Sipos, György/0000-0001-6224-2361; Blanka, Viktória/0000-0001-6364-109X}
}