Tibor Bíró

Prof. Dr. Tibor Bíró


Research Focus & Metrics

Academic Career Length

11Years (2016-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 March 2016 in Bioresource Technology
Verified
Journal Article
Closed access
IBIulian Zoltan Boboescu
Iulian Zoltan Boboescu
VGVasile Daniel Gherman
Vasile Daniel Gherman
GLGergely Lakatos
Gergely Lakatos
BPBernadett Pap
Bernadett Pap
TBTibor Bíró
Tibor Bíró
GMGergely Maroti
Gergely Maroti

1 February 2022 in Science of The Total Environment
Verified
Journal Article
Closed access
ARAlexander G. Rusanov
Alexander G. Rusanov
TBTibor Bíró
Tibor Bíró
KKKeve T. Kiss
Keve T. Kiss
Krisztina BuczkóKrisztina Buczkó
Krisztina Buczkó
Grigorszky IstvánGrigorszky István
Grigorszky István
Éva ÁcsÉva Ács
Éva Ács

1 December 2017 in Algal Research
Verified
Journal Article
Closed access
GLGergely Lakatos
Gergely Lakatos
DBDaniella Balogh
Daniella Balogh
AFAttila Farkas
Attila Farkas
VÖVince Ördög
Vince Ördög
PNPéter Tamás Nagy
Péter Tamás Nagy
GMGergely Maroti
Gergely Maroti

6 May 2020 in Remote Sensing
Verified
Journal Article
Open access
PDF file
LSLoránd Szabó
Loránd Szabó
DBDeák Balázs
Deák Balázs
TBTibor Bíró
Tibor Bíró
GDGareth J. Dyke
Gareth J. Dyke
Szabó SzilárdSzabó Szilárd
Szabó Szilárd
Observing wetland areas and monitoring changes are crucial to understand hydrological and ecological processes. Sedimentation-induced vegetation spread is a typical process in the succession of lakes endangering these habitats. We aimed to survey the tendencies of vegetation spread of a Hungarian lake using satellite images, and to develop a method to identify the areas of risk. Accordingly, we performed a 33-year long vegetation spread monitoring survey. We used the Normalized Difference Vegetation Index (NDVI) and the Modified Normalized Difference Water Index (MNDWI) to assess vegetation and open water characteristics of the basins. We used these spectral indices to evaluate sedimentation risk of water basins combined with the fact that the most abundant plant species of the basins was the water caltrop (Trapa natans) indicating shallow water. We proposed a 12-scale Level of Sedimentation Risk Index (LoSRI) composed from vegetation cover data derived from satellite images to determine sedimentation risk within any given water basin. We validated our results with average water basin water depth values, which showed an r = 0.6 (p < 0.05) correlation. We also pointed on the most endangered locations of these sedimentation-threatened areas, which can provide crucial information for management planning of water directorates and management organizations.

26 May 2023 in Climate
Verified
Journal Article
Open access
PDF file
IJImre M. Janosi
Imre M. Janosi
TBTibor Bíró
Tibor Bíró
Boglárka LakatosBoglárka Lakatos
Boglárka Lakatos
JGJason Gallas
Jason Gallas
ASAndrás Szöllosi-Nagy
András Szöllosi-Nagy
In this mini-review, we present evidence from the vast literature that one essential part of the coupled atmosphere–ocean system that makes life on Earth possible, the water cycle, is exhibiting changes along with many attributes of the global climate. Our starting point is the 6th Assessment Report of the IPCC, which appeared in 2021, where the almost monograph-size Chapter 8, with over 1800 references, is devoted entirely to the water cycle. In addition to listing the main observations on the Earth globally, we focus on Europe, particularly on the Carpathian (Pannonian) Basin. We collect plausible explanations of the possible causes behind an observably accelerating and intensifying water cycle. Some authors still suggest that changes in the natural boundary conditions, such as solar irradiance or Earth’s orbital parameters, explain the observations. In contrast, most authors attribute such changes to the increasing greenhouse gas concentrations since the industrial revolution. The hypothesis being tested, and which has already yielded convincing affirmative answers, is that the hydrological cycle intensifies due to anthropogenic impacts. The Carpathian Basin, a part of the Danube watershed, including the sub-basin of the Tisza River, is no exception to these changes. The region is experiencing multiple drivers contributing to alterations in the water cycle, including increasing temperatures, shifting precipitation regimes, and various human impacts.

11 February 2020 in Water
Verified
Journal Article
Open access
PDF file
ZTZsuzsa Trábert
Zsuzsa Trábert
MDMónika Duleba
Mónika Duleba
TBTibor Bíró
Tibor Bíró
PDPéter Dobosy
Péter Dobosy
AFAngéla Földi
Angéla Földi
Éva ÁcsÉva Ács
Éva Ács
(1) Urbanization significantly influences the ecosystems of rivers in various ways, including the so-called loading effect of wastewater production. Benthic diatoms are used in ecological status assessments of waters. Beside species composition, traits can be used as indicators. We aimed to evaluate how the loading of the large city of Budapest manifests in the physico-chemical variables of the River Danube and what species composition and trait response this loading results in for the benthic diatom communities. (2) Weekly samplings were performed at points upstream and downstream of Budapest on both riverbanks. Samples were compared, based on general physical-chemical variables and the concentration of thirty-four elements, as well as species composition and seven traits of species of diatom communities. Ecological status was assessed using the Specific Pollution Sensitivity Index (IPS). (3) Only a few measured environmental variables showed differences between the sampling points, suggesting that the nutrient loading has significantly decreased due to the installation of several efficiently working wastewater treatment plants since the introduction of the European Union Water Framework Directive. In contrast, the species composition and traits of species showed the effect of land use. Benthic diatoms indicate the environmental changes caused by land use in the longer-term, while chemical measurements reflect instantaneous status.