Temat: anthropogenic change - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Wybrane problemy geomorfologiczne Mazowsza
Selected geomorphological problems of Mazovia
Autorzy:: Smolska, E.
Giriat, D.
Tsermegas, I.
Szwarczewski, P.
Zawadzka-Pawlewska, U.
Błoński, M.
Powiązania:: https://bibliotekanauki.pl/articles/294378.pdf
Data publikacji:: 2017
Wydawca:: Stowarzyszenie Geomorfologów Polskich
Tematy:: cechy rzeźby
zmiana naturalna
zmiana antropogeniczna
Kotlina Warszawska
Wysoczyzna Ciechanowska
dolina dolnej Narwi
landforms features
natural change
anthropogenic change
Warsaw Basin
Ciechanowska upland
Lower Narew Valley
Opis:: Celem artykułu jest zaprezentowanie charakterystycznych cech rzeźby wybranych obszarów Mazowsza ze szczególnym zwróceniem uwagi na jej uwarunkowania zarówno naturalne, jak i antropogeniczne. Przedstawiono holoceńskie zmiany w obrębie zbocza doliny Wisły na przykładzie Skarpy Ursynowskiej, zmiany w dnie doliny związane z osadnictwem olęderskim, wybrane aspekty budowy geologicznej i cechy rzeźby w okolicy Łubienicy na Wysoczyźnie Ciechanowskiej, morfologię zboczy i dna doliny dolnej Narwi w okolicy Łubienicy i Pułtuska oraz rekonstrukcję zmian środowiska przyrodniczego w okolicach Nasielska (od początku wczesnego średniowiecza po okres nowożytny).
The main aim of the article is to present the landforms characteristics of the selected Mazovian areas with particular focus on its natural and anthropogenic conditions. This paper concerns the problems of: the Holocene changes within the Vistula River valley on the example of the the Ursynów Scarp development; the geomorphic changes in the bottom of the valley due to the Olęder settlements (the Kiełpińska Holm site), selected issues of geology and landscape evolution of the Ciechanowska Upland (The Lubienica-Superunki site), morphology of the slopes and of the Lower Narew Valley bottom near Łubienica and Pułtusk sites and the reconstruction of natural environment changes (from the early Middle Ages to the Early Modern Period) in the Nasielsk area.
Źródło:: Landform Analysis; 2017, 33; 3-16
1429-799X
Pojawia się w:: Landform Analysis
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:: Przekształcenia warunków hydrologicznych w dolinie Dolnej Wdy wskutek budowy stopni wodnych
The transformation of hydrological conditions in the lower part of the Wda valley as a result of the building barrages
Autorzy:: Szumińska, Danuta
Powiązania:: https://bibliotekanauki.pl/articles/87515.pdf
Data publikacji:: 2010
Wydawca:: Polskie Towarzystwo Geograficzne
Tematy:: dolina Wdy
stopień wodny
zbiornik zaporowy
elektrownia wodna
przepływ
antropopresja
the Wda river valley
barrage
storage reservoir
water power station
flow
anthropogenic change
Opis:: W pracy omówiono zmiany warunków wodnych spowodowane budową stopni piętrzących w dolnym biegu Wdy. Najsilniejsze przekształcenia związane są z funkcjonowaniem kaskady hydroenergetycznej Żur-Gródek. Jej obecność spowodowała znaczne zwiększenie powierzchni zbiorników wodnych oraz przekształcenie reżimu Wdy poniżej kaskady. Na odcinkach zbiornikowych, a w szczególności w Zbiorniku Żur ma miejsce akumulacja materiału wnoszonego przez Wdę i jej dopływy. Wskutek wykorzystania hydroenergetycznego, poniżej kaskady wzrosła nieregularność przepływów, co powoduje zmiany warunków życia biologicznego w korycie. Znaczne i częste wahania przepływów są też przyczyną uruchamiania rumowiska, które akumulowane jest w kolejnym zbiorniku - Kozłowo i na odcinku Wdy powyżej tego zbiornika. Pomimo pewnych negatywnych aspektów zbiorniki zaporowe, w połączeniu z otaczającymi lasami, stanowią atrakcyjny element krajobrazu doliny Wdy i główną atrakcję Wdeckiego Parku Krajobrazowego.
The paper presents the changes of water conditions in the lower part of the Wda river, caused by the construction of barrages. The strongest transformation are connected with the use of the water power stations Żur and Gródek. This two barrages caused considerable enlargement of the water areas and changed regime of the Wda river downstream the Gródek dam. The bed load from the Wda river and their tributaries has been accumulating in the reservoirs, especially in the Żur reservoir. The outflow irregularity increased in the part of the Wda river downstream of the cascade, as the effect of using water for power stations. Large and frequent changes in the volume of the flow cause decrease of the number of species and the size of populations in the Wda river. Despite of some negative aspects reservoirs and their surrounding there are the most attractive element of the Wda valley landscape and the main attraction of the Wda Landscape Park.
Źródło:: Prace Komisji Krajobrazu Kulturowego; 2010, 13; 110-121
1896-1460
2391-5293
Pojawia się w:: Prace Komisji Krajobrazu Kulturowego
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 3.

Tytuł:: Geospatial assessment of land use and land cover dynamics in the mid-zone of Ghana
Autorzy:: Koranteng, Addo
Adu-Poku, Isaac
Donkor, Emmanuel
Zawiła-Niedźwiecki, Tomasz
Powiązania:: https://bibliotekanauki.pl/articles/2041498.pdf
Data publikacji:: 2020
Wydawca:: Instytut Badawczy Leśnictwa
Tematy:: LULC change
anthropogenic pressures
Cellular-Automata-Markov
forest loss
urbanization
Opis:: Land use and land cover (LULC) terrain in Ghana has undergone profound changes over the past years emanating mainly from anthropogenic activities, which have impacted countrywide and sub-regional environment. This study is a comprehensive analysis via integrated approach of geospatial procedures such as Remote Sensing (RS) and Geographic Information System (GIS) of past, present and future LULC from satellite imagery covering Ghana’s Ashanti regional capital (Kumasi) and surrounding districts. Multi-temporal satellite imagery data sets of four different years, 1990 (Landsat TM), 2000 (Landsat ETM+), 2010 (Alos and Disaster Monitoring Constellation-DMC) and 2020 (SENTINEL), spanning over a 30-year period were mapped. Five major LULC categories – Closed Forest, Open Forest, Agriculture, Built-up and Water – were delineated premised on the prevailing geographical settings, field study and remote sensing data. Markov Cellular Automata modelling was applied to predict the probable LULC change consequence for the next 20 years (2040). The study revealed that both Open Forest and Agriculture class categories decreased 51.98 to 38.82 and 27.48 to 20.11, respectively. Meanwhile, Built-up class increased from 4.8% to 24.8% (over 500% increment from 1990 to 2020). Rapid urbanization caused the depletion of forest cover and conversion of farmlands into human settlements. The 2040 forecast map showed an upward increment in the Builtup area up to 35.2% at the expense of other LULC class categories. This trend from the past to the forecasted future would demand that judicious LULC resolutions have to be made to keep Ghana’s forest cover, provide arable land for farming activities and alleviate the effects of climate change.
Źródło:: Folia Forestalia Polonica. Series A . Forestry; 2020, 62, 4; 288-305
0071-6677
Pojawia się w:: Folia Forestalia Polonica. Series A . Forestry
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 4.

Tytuł:: Challenges and perspectives for human activity in Arctic coastal environments – a review of selected interactions and problems
Autorzy:: Jaskólski, Marek Wojciech
Powiązania:: https://bibliotekanauki.pl/articles/1069041.pdf
Data publikacji:: 2021
Wydawca:: Uniwersytet Warszawski. Wydział Geografii i Studiów Regionalnych
Tematy:: Arctic settlements
climate change
geohazards
environmental changes
anthropogenic impact
arctic sustainability
Opis:: The currently observed increase in human activity in the Arctic accelerates the negative impact on the environment as well as increases the risk of threats to mankind itself. This paper reviews and summarises a selection of studies on the interaction between humans and the environment in the Arctic coastal zone, which is impacted by a warming climate and associated geohazards. The paper presents a general description of human presence in the Arctic, identifies and describes the processes that are threatening the infrastructure, and the anthropogenic processes that have a negative impact on the Arctic. It considers the possible future economic opportunities, and presents the sustainable requirements for modern human activity in the Arctic. The paper demonstrates the urgent need to develop a common, Arctic-wide strategy based on sustainable development. The time has come to change human perception of the Arctic because, in the near future, it may be considered as a refuge for climate change refugees.
Źródło:: Miscellanea Geographica. Regional Studies on Development; 2021, 25, 2; 127-143
0867-6046
2084-6118
Pojawia się w:: Miscellanea Geographica. Regional Studies on Development
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 5.

Tytuł:: Changes in Atlantic water characteristics in the South-Eastern Mediterranean Sea as a result of natural and anthropogenic activities
Autorzy:: Said, M.A.
Gerges, M.A.
Maiyza, I.A.
Hussein, M.A.
Radwan, A.A.
Powiązania:: https://bibliotekanauki.pl/articles/47724.pdf
Data publikacji:: 2011
Wydawca:: Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:: Atlantic water
change
Mediterranean Sea
Egypt
natural activity
anthropogenic activity
temperature
salinity
trend
water mass
subsurface water
water column
Źródło:: Oceanologia; 2011, 53, 1
0078-3234
Pojawia się w:: Oceanologia
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 6.

Tytuł:: The pH changes of the soils formed as a result of reclamation of the sand-pits
Autorzy:: Drab, M
Greinert, H.
Powiązania:: https://bibliotekanauki.pl/articles/1450179.pdf
Data publikacji:: 2001
Wydawca:: Polska Akademia Nauk. Instytut Agrofizyki PAN
Tematy:: Bobr River
agricultural reclamation
pH change
soil
soil acidification
soil property
sandpit
degraded ecosystem
recultivated soil
reclamation
anthropogenic ecosystem
alluvial soil
Opis:: The alluvial soils in the Bóbr river valley, devastated by sand and gravel exploitation, were reclaimed for agricultural use. After reclamation treatment, the newly formed soil was very acid. Application of 5 Mg/ha lime elevated soil pH to 6-7, but during the following years, soil pH dropped again by about one half of the pH unit a year. Rapid drop in the pH level can result both from geological and soil-forming processes. Efficiency of mineral fertilizers applied in various combinations did not give the expected results and the yield of cultivated plants was not satisfactory. Mineral fertilization in various combinations did not result in the expected yield levels.
Źródło:: Acta Agrophysica; 2001, 51; 37-43
1234-4125
Pojawia się w:: Acta Agrophysica
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 7.

Tytuł:: Zmiany poziomu morza : przyczyny, skale czasowe i historia ich poznania
Sea level changes : causes, time scales and the history of their recognition
Autorzy:: Boski, Tomasz
Wilamowski, Andrzej
Powiązania:: https://bibliotekanauki.pl/articles/2076015.pdf
Data publikacji:: 2020
Wydawca:: Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:: zmiana poziomu morza
zapis geologiczny
zapis miernika pływów
altimetria satelitarna
wpływ antropogeniczny
sea level change
geological record
tide gauge record
satellite altimetry
anthropogenic impact
Opis:: Sea level changes provoked by multiple forcings that act in a wide range of time scales attracted human interest for several millennia. However, the bases of modern understanding of this phenomenon and its quantitative expression were achieved during the last two centuries. At present, owing to a series of altimetric observations made by 4 satellite missions in the last 30years, the mean sea level (MSL) rise calculated for the whole Earth is estimated to be 3-3.5 mm per year, with at least half of this value being attributable to human-induced climate warming. About 125,000 years ago, during the last interglacial (Eemian) that was warmer than the current period, the MSL was about 5 m higher than today. Approximately 116,000 years ago, the sea level began to decline as a result of gradual cooling of the climate that led to glaciation, which in the Northern Hemisphere had a climax at 20-30 ka BP. The transition from the last glacial maximum to the current warm period, covering the last 20,000years, includes the transfer of about 35 106 km3 of water from melting ice caps of the Northern Hemisphere to the oceanic reservoir, causing an increase in sea level of about 130 m. The average rate of MSL rise was about 10 mm per year, although over the last seven millennia, the MSL rising rate dropped to about 1-1.5 mm per year. These changes are considered representative of the natural variability of the Earth's climate system over the past 2 million years.
Źródło:: Przegląd Geologiczny; 2020, 68, 11; 820--823
0033-2151
Pojawia się w:: Przegląd Geologiczny
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 8.

Tytuł:: Physiographic and meteorological conditions in the Doplyw spod Nowej Wsi catchment during the last 150 years
Autorzy:: Okonski, B.
Miler, A.T.
Panfil, M.
Powiązania:: https://bibliotekanauki.pl/articles/59808.pdf
Data publikacji:: 2008
Wydawca:: Polska Akademia Nauk. Stowarzyszenie Infrastruktura i Ekologia Terenów Wiejskich PAN
Tematy:: physiography
meteorological condition
Doplyw spod Nowej Wsi catchment
catchment
history
Warmia region
forested-agricultural catchment
pond storage
natural pond storage
anthropogenic factor
air temperature
long-term change
Opis:: The paper covers research on physiographic features and anthropogenic factors influence on natural pond water storage. The problem was investigated both at the level of the Dopływ spod Nowej Wsi catchment (27.53 km2) and the smaller spatial unit Bagna Ramuckie natural pond (12.4 ha). Dynamics of physiographic features, changes of hydrographical network and anthropogenic factors including water, land and forest management practices were investigated. The decisive factor modulating processes of water storage rebuilding for investigated spatial units seems to be dynamics and long-term directional changes of air temperature. Rebuilding of pond water storage occurred after a 40-year period of air temperature decrease and the decline of water storage after a 20-year period of air temperature increase. Precipitation had minor significance in modulating pond water storage in long-term periods, because lack of long-term precipitation trends in analysed period. Although in short-term periods precipitation have important modulating impact on a decline of pond storage. The decline occurred after the dry period from 1989 to 1995 as a result of high deficit of climatic water balance. Spectacular rebuilding of pond water storage occurred in Bagna Ramuckie after the cold and wet period from 1956 to 1965. Non-climatic physiographic features and anthropogenic factors did not influence the processes of pond water storage rebuilding and decline because both of these factors seemed to be stationary over at least eight decades of 20th century, while processes of storage rebuilding or decline lasted over the investigated spatial unit.
Źródło:: Infrastruktura i Ekologia Terenów Wiejskich; 2008, 06
1732-5587
Pojawia się w:: Infrastruktura i Ekologia Terenów Wiejskich
Dostawca treści:: Biblioteka Nauki