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INSTYTUT ARCHEOLOGII I ETNOLOGII POLSKIEJ AKADEMII NAUK
INSTYTUT BADAŃ LITERACKICH POLSKIEJ AKADEMII NAUK
INSTYTUT BADAWCZY LEŚNICTWA
INSTYTUT BIOLOGII DOŚWIADCZALNEJ IM. MARCELEGO NENCKIEGO POLSKIEJ AKADEMII NAUK
INSTYTUT BIOLOGII SSAKÓW POLSKIEJ AKADEMII NAUK
INSTYTUT CHEMII FIZYCZNEJ PAN
INSTYTUT CHEMII ORGANICZNEJ PAN
INSTYTUT FILOZOFII I SOCJOLOGII PAN
INSTYTUT GEOGRAFII I PRZESTRZENNEGO ZAGOSPODAROWANIA PAN
INSTYTUT HISTORII im. TADEUSZA MANTEUFFLA POLSKIEJ AKADEMII NAUK
INSTYTUT JĘZYKA POLSKIEGO POLSKIEJ AKADEMII NAUK
INSTYTUT MATEMATYCZNY PAN
INSTYTUT MEDYCYNY DOŚWIADCZALNEJ I KLINICZNEJ IM.MIROSŁAWA MOSSAKOWSKIEGO POLSKIEJ AKADEMII NAUK
INSTYTUT PODSTAWOWYCH PROBLEMÓW TECHNIKI PAN
INSTYTUT SLAWISTYKI PAN
SIEĆ BADAWCZA ŁUKASIEWICZ - INSTYTUT TECHNOLOGII MATERIAŁÓW ELEKTRONICZNYCH
MUZEUM I INSTYTUT ZOOLOGII POLSKIEJ AKADEMII NAUK
INSTYTUT BADAŃ SYSTEMOWYCH PAN
INSTYTUT BOTANIKI IM. WŁADYSŁAWA SZAFERA POLSKIEJ AKADEMII NAUK
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Health resorts beside mineral water and muds should provide the best air quality which enables climatotherapy conducted in the open air. However the air in health resorts is polluted by particulate matter PM10, PM2.5 and benzo(a)pyrene the same as the rest of Poland – the most polluted European country. In Poland there are 45 statutory health resorts, 1 organized in underground salt mine excavation and 8 towns with a status of a spa protection area. In the years 2010-2018 permanent monitoring of PM10 was conducted only in 14 Polish spas and among them only in 5 since 2010. PM2.5 and B(a)P is measured in even less number of stations. The paper analyses the values of the average annual concentration of pollutants, the number of days with permissible levels, the annual courses but also the reasons for this state. A large part of the causes of poor air conditions are due to the lack of a state policy promoting renewable energy sources and "clean" technologies, maintenance and co-financing of unprofitable coal mines, but also because of ordinary poverty, and often the lack of reflection and knowledge about fatal consequences of the burning things that should never be burned at low temperatures. There are many more problems, but first of all without abandoning coal heating, without a wise state policy, spa municipalities cannot cope alone with the problem of air pollution.
Heavy downpours and flash floods accelerate the denudation of slopes, as well as erosion, and hence accumulation in the bottoms of valleys (Słupik, 1981; Starkel, 1996; Gil, 1998). However, the geomorphological impact depends less on the amount and duration of falls of rain, and more on intensity and spatial extent. The intensity of mass movements and floods also depends on relief, the type and thickness of soil, the lithology and tectonic history of rocks, which together determine infiltration rates and runoff. An important role in triggering mass movements is also played by human activity (land use, terracing and the undercutting of slopes). This paper presents the role of short-duration downpours occurring in the July of 1997 and 2008 where the shaping of the Jaszcze and Jamne valleys in the Gorce Mountains is concerned. The narrow valley of the Jaszcze has very steep slopes and is covered by dense patches of forest. In contrast, the Jamne Valley with its predominantly gentle slopes has been largely deforested. At higher elevations, the Jaszcze catchment has a prevalence of meadows and pastures that contrasts with the dominant arable land lower down. The Jamne catchment in turn has meadows and pastures of its own, plus arable fields reaching altitudes of 1100 m a.s.l. (Obrębska-Starklowa, 1970). Following the rainfall of July 1997, it proved possible to register 85 new superficial landslides on air photos (55 in the Jaszcze Valley and 30 in the Jamne Valley), these covering a total area of c. 29,700 m2. Among dominant forms were slumps and mudflows of loamy-sandy regolith, created mainly on steep, grass-covered slopes (≥20°), on the edges of field terraces and on the colluvium of old landslides. A flood of 23 July 2008 was also connected with a heavy downpour, daily rainfall that day reaching 76.3 mm at the river outlet. The highest level in the Jaszcze and Jamne was noted at about 17.00. The most marked changes characterised the Jamne channel, this reflecting its more limited forest cover and the higher density of the river network. Lateral erosion prevailed over downcutting, causing the reactivation of old undercuts and the development of new ones, the height reaching 3.5 m. Boulders up to 25 cm in size were transported, and the deposition of debris followed. Older gravel bars were cut and new ones built up. Only a few small earth slumps appeared on the slopes, and these were never in forest. A map showing the potential susceptibility of the Jaszcze and Jamne catchments was prepared on the basis of field data and a statistical analysis, using the landslide index method (Van Westen, 1994). While the greatest geomorphological effects of rainfall are to be noted in stream channels, the transformation of slopes by mass movements is less remarkable. However superficial landslides are characteristic of deforested slopes covered by a thin loamy regolith over flysch sandstones and shales. GIS analysis and field observations make it clear that the geological structure deeper down does not play an important role in triggering of superficial landslides.
High intensity rains bring about landslides and high surface run‑off in the upper catchment of the Balason River. Huge quantities of weathered materials as sediment load are being deposited in the river’s lower course. The extent and intensity of this bed material extraction have taken such a toll that immediate attention is necessary to reduce the associated effects on the forms and processes of the Balason River’s lower course. In this paper, an attempt has been made to closely analyse the prevailing effects of human interference noticed by the authors during this study. The methodology adopted during this study is field based. The changing cross sections and fluvial characteristic of the river were continuously observed. The extraction of bed materials was done directly from the riverbed and from adjacent flood plains and also from terraces. The extractions are responsible for the prevailing bed erosion and channel diversions because extraction pits are what are left behind. In the long term, if not controlled, the effects would be detrimental to the entire fluvial characteristics of the river.
Higher education has been perceived as a value, necessary for the process of societal development, as well as the development of individuals in post-socialist Europe. In this context, the paper aims to focus on Geography students and graduates to analyse their expectations for their futures in the discipline. Geography students are discussed here at Comenius University, Bratislava, Slovakia, but implications can be applied broadly. In particular, gender-based differences were revealed in Geography students' ambitions related to their future careers. Not surprisingly, attitudes of students and Geography teaching staff differ substantially in some aspects, including labour-market orientation of Geography curriculum. Lack of practical and business-related skills in existing curriculum might be a limitation of the graduates' labour prospects.
Historical changes in land use and development over the last century were analysed to identify the main causes and directions of changes in depression wetland ecosystems in the Włoszczowa Basin, an area of 1600 km2 in southern Poland. The analysis of Military Cartographic Institute maps and orthophotomaps, as well as field surveys, made it possible to determine the scale of degradation of 247 treeless depression wetlands. It was shown that the nature and extent of transformation of individual wetlands varied depending on the type of wetland and the method of land use in adjacent areas. However, the main anthropogenic factor affecting these changes was land drainage, of which the greatest intensity in Central Europe was pursued during the socialist rule between 1945 and 1989. <br>
Housing estates were constructed by public authorities and private investors long before the era of large prefab housing estates. Their dwellings, like almost all flats, became privatised after 1989 in the postsocialist cities, thus they appeared in the housing market. The aim of this paper is to analyse their market position and to explore how their physical characteristics and residential environment influence the dwelling prices. It also examines the impact of the renovation of buildings with a special attention to its housing policy background. <br>
Human activities have brought major changes to landscape, as a result of the expansion of settlements, and other activities. The need to valorise the landscape for the requirements of current and future activities results from the more and more limited space, which in itself becomes an important resource, which should be properly valorised and then shaped. The literature presents a wide variety of landscape valorisation and assessment methods used for various aspects of economic or scientific purposes. However, there is no universal method. This review article summarises selected diverse methods used for valorisation, assessment and economic valuation of the landscape.
Hungary is struggling with its fragmented local governmental system. The so called “public service reform” aimed to offer equal access to all as regards local public services, as well as to encourage efficiency of activity at local administrative level. The government transferred to local actors the responsibility for the implementation of reform commissioned centrally. The organisational and geographical frameworks for the rationalisation of local public administration were in turn devised at micro-regional level. This paper mainly aims to analyse urban-rural connections, as co-operative networks of local authorities have already been created. The issue is the extent to which the horizontal cooperations created to organise public services can be effective if their vertical connections are very weak, and, further, if there is no mechanism to counterbalance regional differences.
Hungary’s capital, Budapest is divided into 23 districts, which have significantly distinct topography: thus, having different level of vulnerability to certain climatic effects; in addition, their climate adaptation potential also varies. This study aimed to analyze the 23 districts of Budapest, Hungary, in terms of their climate adaptation consciousness from governmental perspective. The study compares the 23 districts through a scoring matrix with three main categories – attitude, planning, and implementation – and several criteria. In addition, interviews were organized with municipal employees with 43 questions following the structure of the scorin matrix, learning more about the districts’ commitment to climate adaptation.
Hydrographical mapping carried out by the Author provided for a quantitative evaluation of the distribution of different types of springs located on the homoclinal ridge of Mount Babia Góra – at 1725 m a.s.l., the highest mountain in the Western Carpathians (Fig. 1), built of flysch sediment. Circulation of groundwater on ridge slopes modelled in different ways by landslides was analysed, with particular attention paid to the circulation of water in the deeply-fissured Magura Sandstone that forms the upper part of the massif, as well s the thick cover of colluvia (Figs. 2 and 3). The depth and distance of water circulation on different parts of the slopes were evaluated in relation to altitude, slope exposure, type of flysch rock and landslide topography. Six types of water-bearing sediment were distinguished, and their limits of occurrence identified. Magura Sandstone appeared to be the most water-retaining sediment, proving permeable down to depths of 100 m locally. Three classifications of springs were carried out, in line with geomorphological location (direction of groundwater inflow and means of circulation), type of water-bearing sediment, and local-scale distribution(in connection with landslide forms). Among the 873 springs located in the Polish part of Mt. Babia Góra, over 80% are slope located and can be regarded as descending springs. These include: rock springs (a), rock-debris springs (b), debris springs (c), and rock-mantle springs (d). Other springs occur on valley floors (e) and are also mostly of the descending type, though a few are ascending (mineral and thermal). Most springs are alimented by water flowing out from thick covers of colluvia. Within this group it proved possible to distinguish three subtypes of spring (b2, b3, b4 ) located in different segments of landslides (Fig. 4). Other divisions of springs were into single springs, lines of springs and series of springs (Fig. 5). The number of springs on the slopes of Mt. Babia Góra is similar to the number located at the foot of the mountain comprising lateral ridges and valley floors. Along a profile of altitude, the largest numbers of springs can be seen to be located at the heads of valleys, where the density on the northern slope exceeds 30 per. km-2 (Fig. 6). The density of springs on the southern slope in valleys located at high altitude is even greater. The determined distribution of springs down the altitudinal profile of Mt. Babia Góra allowed for delimitation of three hydrographical belts - of water alimentation, transit and accumulation, which are different from the hydrographical belts noted in the Western Beskidy and Tatra Mountains. The distribution of springs on Mount Babia Góra and their unusually high density are determined first and foremost by the landslide morphology of slopes.
Hydrological investigations require the development of a geodatabase allowing for the calculation of physiographic catchment parameters, as well as the analysis of amounts of water resources and changes therein. Such a geodatabase usually consists of meteorological, hydrological and cartographic data. The present study offers a review of datasets that may be used for geodatabase development in the interests of hydrological research, in catchments located in the Polish-Ukrainian borderland. The catchment of the Wiar River – selected to serve as a case study – is in fact divided by the state border into two equal sub-catchments (395.5 km2 in Poland and 398.9 km2 in Ukraine).The results reveal disparities in the spatial distribution of stream and meteorological gauges. For the Polish part of the catchment datasets include many parameters (in accordance with EU Directive and Regulations) and the results from monitoring are available online as yearly reports. For the Ukrainian part, only chemical components are monitored, and these data are not made available publicly. Consistent data sets such as DEM can be obtained from globally available ASTER and SRTM models. Datasets, such as LiDAR, which are important for medium and large-scale analyses allowing for the development of high-resolution DEMs, do not exist. Use of TanDEM-X data is restricted for the Ukrainian territory. However, comparison between the SRTM and LiDAR models (for the Polish part) revealed that the SRTM model may be optimised to serve the whole area. Land-use and land-cover data (LULC) are important in many hydrological analyses. the authors propose using satellite images in the development of a comparable layer describing land cover of the whole catchment.
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