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György Sipos

Researcher at University of Szeged

Publications -  79
Citations -  757

György Sipos is an academic researcher from University of Szeged. The author has contributed to research in topics: Geology & Floodplain. The author has an hindex of 12, co-authored 61 publications receiving 532 citations.

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Alterations of channel parameters in response to river regulation works since 1840 on the Lower Tisza River (Hungary)

TL;DR: In this paper, the authors focus on river management works and their effect on planimetric and cross-sectional parameters, with special attention to the flood conductivity changes to the river channel.
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Prevailing surface winds in Northern Serbia in the recent and past time periods; modern- and past dust deposition

TL;DR: In this paper, the prevailing surface winds and their associated aeolian processes in Northern Serbia, focusing on the southeastern part of the Carpathian Basin, were examined using wind and atmospheric pressure data from 1939-2014 and 1960-2010.
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The evolution of the Great Hungarian Plain fluvial system – Fluvial processes in a subsiding area from the beginning of the Weichselian

TL;DR: In this article, the authors summarize the controlling factors and describe the evolution of the Great Hungarian Plain (GHP) through tectonic and climatic factors and vegetation change, and pay particular attention 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.
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Braid-scale channel geometry changes in a sand-bedded river : Significance of low stages

TL;DR: In this article, the importance of different stages of bed formation and transportation processes along the partly managed lowland section of Maros River (South Hungary) was determined, applying a series of cross-sectional data.
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Distribution of relict permafrost features in the Pannonian Basin, Hungary

TL;DR: Wedge structures and involutions suggest that Late Pleistocene frozen ground, either permafrost or deep seasonal frost, extended at least as far south as latitude 47°N in central Europe (the Pannonian Basin).