Geographia Polonica (2025) vol. 98, iss. 2
Articles
Geographia Polonica (2025) vol. 98, iss. 2, pp. 121-147 | Full text
doi: https://doi.org/10.7163/GPol.0296
Abstract
Coastal deltaic landscapes under tropical monsoon regions are sensitive to sea level changes exacerbated by human interventions. In low-lying areas, rising relative sea level (RSL) and such interventions are intensifying geohazards like coastal erosion and land subsidence. This study examines erosion and flooding risks in the Sundarbans mangroves along the Bay of Bengal using statistical models – Endpoint Rate (EPR) and Shoreline Change Envelope (SCE) incorporated in Digital Shoreline Analysis System (DSAS). “Patharpratima Block”comprises thirteen estuarine islands, part of the delta formed via confluence of three rivers, the Ganges, the Brahmaputra, and the Meghna. EPR and SCE were applied via geospatial modelling, and remote sensing to evaluate coastal changes between 1990-2020. Results show the shoreline undergoes gradual to significant changes due to fluctuating erosion and deposition, impacting local residents. Surendranagar and Dhanchiwere identified as the most vulnerable, followed by moderately vulnerable Lothian. With observed RSL rise, shoreline dynamics were modeled using EPR and SCE to estimate past and future changes. Additionally, the Sundarban Reserve Forest (SRF), the world’s largest mangrove forest, is at risk of disappearing. The region’s population has increased, while total area has shrunk due to erosion. Urgent sustainable measures are neededto prevent biodiversity loss and displacement of livelihoods into environmental refugees.
Keywords: sea level rise, river estuarine islands, shoreline, coastline, geospatial modeling, Patharpratima Block
rituparna.acharyya@ukw.edu.pl], Faculty of Geographical Sciences Kazimierz Wielki University Plac Koscieleckich 8, 85-064 Bydgoszcz: Poland
, School of Oceanographic Studies Jadavpur University Kolkata, West Bengal: India
, Department of Environmental Science University of Calcutta Kolkata, West Bengal: India
, Directorate of Forests Government of West Bengal Kolkata, West Bengal: India
, Nature Mates-Nature Club Kolkata, West Bengal: India
, Nature Mates-Nature Club Kolkata, West Bengal: India
, Nature Mates-Nature Club Kolkata, West Bengal: India
, Nature Mates-Nature Club Kolkata, West Bengal: India
, Nature Mates-Nature Club Kolkata, West Bengal: India
Geographia Polonica (2025) vol. 98, iss. 2, pp. 149-169 | Full text
doi: https://doi.org/10.7163/GPol.0297
Abstract
The expansion of cities, alongside increasing climate-related risks, requires a better understanding of urban thermal patterns for sustainable planning. This study identifies thermal hot and cold spots in Warsaw using 25 land surface temperature (LST) images (2002-2018), air temperature data from 21 sites, spatial developmentindicators, CORINE Land Cover, and local climate zones. Spatial autocorrelation (Getis-Ord Gi*) and correlation analyses reveal that LST extremes are related to land cover, spatial development, and city centre proximity. Cluster analysis highlights distinct seasonal and diurnal air temperature regimes in hot/cold spots, emphasizing the need for integrated approaches in urban climate research.
Keywords: cold spot, hot spot, land surface temperature, air temperature, land cover, local climate zones, spatial development
czarnecka@twarda.pan.pl], Institute of Geography and Spatial Organization, Climate Research Department Polish Academy of Sciences Twarda 51/55, 00-818 Warsaw: Poland
[Application of optical microscopy to assessment of solid waste contamination of soils
Geographia Polonica (2025) vol. 98, iss. 2, pp. 171-183 | Full text
doi: https://doi.org/10.7163/GPol.0298
Abstract
Solid waste contamination in soils is an extremely important and relevant problem for recreational areas and sports centers. Solid wastes, such as glass, plastics, and metals, do not degrade quickly and accumulate in thes oil at shallow depths or remain on the surface. This is a particularly dangerous situation for recreational area users and may lead to cuts, which can cause severe infections. In the analyzed case, pollutants were present at the junction of a beach and a nearby area that was covered with a small amount of grassy vegetation, which further limited the visibility of solid wastes. A microscopic analysis method was used to assess the presence of hazardous waste in the soil qualitatively and quantitatively. Petrographic analysis revealed the presenceof glass and metals in the examined material, as well as other solid components. In addition, areas where the concentration of these hazardous pollutants had increased and those where they had not been identified
Keywords: soil pollution, petrography, hazardous waste, hazards at recreation areas and sports centers
zjelonek@us.edu.pl], Faculty of Natural Sciences University of Silesia in Katowice Będzińska 60, 41-200 Sosnowiec: Poland; Center for Biomass Energy Research and Education University of Silesia in Katowice Będzinska 60, 41-200 Sosnowiec: Poland
[iwona.jelonek@us.edu.pl], Faculty of Natural Sciences University of Silesia in Katowice Będzińska 60, 41-200 Sosnowiec: Poland; Center for Biomass Energy Research and Education University of Silesia in Katowice Będzinska 60, 41-200 Sosnowiec: Poland
[dymytro.khomenko@us.edu.pl], Faculty of Natural Sciences University of Silesia in Katowice Będzińska 60, 41-200 Sosnowiec: Poland
Geographia Polonica (2025) vol. 98, iss. 2, pp. 185-209 | Full text
doi: https://doi.org/10.7163/GPol.0299
Abstract
This article presents research results on the water chemistry of 16 reservoirs adjacent to post-mining waste landfills in the Upper Silesian Coal Basin, sampled in 2022 and 2023. The waters of these reservoirs are anthropogenically modified; in terms of hydrochemical type, they are multi-ionic waters: Cl––SO42––Na+, Cl––SO4––HCO3––Na2–,and Cl––SO42––HCO3––Na+–Ca2+. They are characterized by high electrical conductivity (EC; up to 21.5 mS/cm), high concentrations of Cl– (up to 9.279 mg/L), SO42– (up to 5.277 mg/L), and Na+ (up to 4.783 mg/L). They are considered waters of poor quality (class V) due to their increased concentrations of Cl– and SO42– and high ECvalues. The Comprehensive Pollution Index (CPI) was also used to assess the degree of water pollution. Calculations indicated that the waters are either moderately (0.47 < CPI < 1.92) or heavily polluted (CPI > 2). Research has also shown that areas reclaimed with mining waste are informal post-mining waste dumps and should be treated as potential sources of groundwater pollution. In nearby reservoirs, there is a potential threat to shallow (0-10 m) groundwater of the first aquifer, which is especially important when the first aquifer is being used.
Keywords: mining waste dumps, water reservoirs, Upper Silesian Coal Basin, environmental hazards
marek.soltysiak@us.edu.pl], Institute of Earth Sciences University of Silesia in Katowice Będzińska 60, 41-200 Sosnowiec: Poland
[jacek.rozkowski@us.edu.pl], Institute of Earth Sciences University of Silesia in Katowice Będzińska 60, 41-200 Sosnowiec: Poland
Geographia Polonica (2025) vol. 98, iss. 2, pp. 211-229 | Full text
doi: https://doi.org/10.7163/GPol.0300
Abstract
Reservoirs created by damming rivers significantly modify abiotic and biotic environmental components. A major consequence is the accumulation of sediments and nutrients, degrading water quality through eutrophication.This study focused on the Sulejów Reservoir in Central Poland, examining nutrient balance,phytoplankton blooms using Sentinel-2 satellite data, and wind-driven surface currents with the CCHE2D hydrodynamic model. Eight Sentinel-2 images from the 2020 vegetation season and the Normalized Difference Chlorophyll Index (NDCI) were used to assess phytoplankton distribution. Results indicate the reservoirmainly acts as a nutrient sink, but under low-flow and intense bloom conditions, it can become a nutrient source. Coupling remote sensing with hydrodynamic modeling effectively interpreted flow patterns and nutrient dynamics. For the first time, the influence of eddy structures and wind on phytoplankton distribution in the lacustrine zone was demonstrated.
Keywords: eutrophication, phytoplankton blooms, Sentinel-2, hydrodynamic modelling, Pilica River, Sulejów Reservoir, NDCl, CCHE2D
peshang.hamakarim@student.uw.edu.p], Doctoral School of Exact and Natural Sciences Discipline of Earth and Related Environmental Sciences, University of Warsaw Stefana Banacha 2c, 02-097 Warsaw: Poland
[mkalinow@igf.edu.pl], Institute of Geophysics Polish Academy of Sciences Księcia Janusza 64, 01-452 Warsaw: Poland
[aleksandra.zieminska-stolarska@p.lodz.pl], Faculty of Process and Environmental Engineering Technical University of Lodz Wólczańska 213, 93-005 Łódź: Poland
[asmagnus@uw.edu.pl], Faculty of Geography and Regional Studies University of Warsaw Krakowskie Przedmieście 30, 00-927 Warsaw: Poland
Reconstruction of geodynamic processes on the Vistula riverbank in Medieval Toruń (Poland)
Geographia Polonica (2025) vol. 98, iss. 2, pp. 231-249 | Full text
doi: https://doi.org/10.7163/GPol.0301
Abstract
During roadworks on Bulwar Filadelfijski in Toruń, the foundations of a Benedictine monastery and the Holy Spirit Church were uncovered. Geoarchaeological research analyzed fluvial, denudational, and anthropogenic layers in the Vistula riverbank. The aim was to determine the spatial and stratigraphic relationships between fluvial and denudational sedimentsand anthropogenic embankments in the Vistula riverbank zone. Key findings:(1) Early medieval fluvial and denudational processes shaped sediments, with Bronze Age and Roman artifacts redeposited by medieval floods. (2) Late medieval construction (monastery, perimeter wall) led toanthropogenic embankments dominating the area. (3) After the monastery’s mid-17th-century destruction, major floods deposited overbank alluvium. The study clarifies the site’s stratigraphic evolution under naturaland human influence.
Keywords: geoarchaeological reconstruction, fluvial and denudational processes, anthropogenic embankments deposits, medieval town, Vistuli River valley
jacek.szmanda@twarda.pan.pl], Institute of Geography and Spatial Organization Polish Academy of Sciences Kopernika 19, 87-100 Toruń: Poland
[piotr.gierszewski@twarda.pan.pl], Institute of Geography and Spatial Organization Polish Academy of Sciences, Kopernika 19, 87-100 Toruń, Poland
[mateusz.kramkowski@twarda.pan.pl], Institute of Geography and Spatial Organization Polish Academy of Sciences Kopernika 19, 87-100 Toruń: Poland
[karol.witkowski@twarda.pan.pl], Institute of Geography and Spatial Organization Polish Academy of Sciences Św. Jana 22, 31-018 Kraków: Poland
[sebastian. tyszkowski@twarda.pan.pl], Institute of Geography and Spatial Organization Polish Academy of Sciences Kopernika 19, 87-100 Toruń: Poland
[michał.fojutowski@twarda. pan.pl], Institute of Geography and Spatial Organization Polish Academy of Sciences Kopernika 19, 87-100 Toruń: Poland
[piotr.kittel@geo.uni.lodz.pl], Faculty of Geographical Sciences University of Lodz Narutowicza 88, 90-139 Łódź: Poland
[mkrapiec@agh.edu.pl], Faculty of Geology, Geophysics and Environmental Protection AGH University of Science and Technology Mickiewicza 30, 30-059 Kraków: Poland
[wojchud@umk.pl], Institute of Archaeology Nicolaus Copernicus University in Toruń Szosa Bydgoska 44/48, 87-100 Toruń: Poland
[rynius@umk.pl], Institute of Archaeology Nicolaus Copernicus University in Toruń Szosa Bydgoska 44/48, 87-100 Toruń: Poland
[malgorzata.luc@uj.edu.pl], Institute of Geography and Spatial Management Jagiellonian University in Kraków Gronostajowa 7, 30-387 Kraków: Poland