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Wyszukujesz frazę "Sahara" wg kryterium: Temat


Wyświetlanie 1-4 z 4
Tytuł:
Kształt barchanów jako wskaźnik reżimu wiatru na przykładzie Sahary Zachodniej Maroko
Shape of barchan dunes as an indicator of wind regime: a case study from the Moroccan Western Sahara
Autorzy:
Dluzewski, M.
Biejat, K.
Powiązania:
https://bibliotekanauki.pl/articles/2084335.pdf
Data publikacji:
2012
Wydawca:
Uniwersytet Warszawski. Wydział Geografii i Studiów Regionalnych
Tematy:
Maroko
Sahara
wiatry
wydmy
Opis:
Barchans are characterized by a symmetric shape independently of their stage of development and the axis of symmetry parallels to the dominant wind direction. However, shape of the dunes can be modified by several factors, among which most important are: change of wind regime, dune collisions or interaction of closely spaced dunes, ground surface relief, asymmetric sediment supply. The aim of the study was to analyze the impact of short-term (diurnal) and long-term (seasonal) changes in wind direction and velocity on shape of barchan dunes. The study was conducted in southern Moroccan area of Western Sahara, between Tarfaya and Laâyoune. This area is characterised by significant variability of active wind (RDP/DP=0,66) which is unfavourable for barchans development. Measurements were conducted in two spring seasons of 2011 and 2012 and two autumn seasons of 2007 and 2011. 52 isolated barchans were selected for detailed studies. Based on GPS-RTK measurements, precise 3D models of the landforms were obtained allowing the detailed analysis of dune shapes. Changes of basie morphological parameters were analyzed as well as shape changes occurring the windward slope and within dunes horns. The shapes of the barchans were correlated with the short-term and the long-term wind regime. It was found that basic morphological parameters are not good indicators of wind variability, with the exception of barchan horns lengths which change according to the seasonal wind regime. Short-term wind regime changes are well registered by: i) "collars" developing along the dune crestlines, ii) "tongues" developing at the ends of dune horns and iii) location of the dune apex. On the other hand, beaded horns testify for very strong wind. I was found, that mentioned features develop and undergo modification during first days or even hours of changed wind regime. The analyzes of barchan shapes, performed in different seasons, proved that even a several-month long period of highly diversified wind regime does not change basie shape of the barchans. Therefore, it can be inferred that barchans development does not depend exclusively on wind regime.
Źródło:
Prace i Studia Geograficzne; 2012, 49; 7-31
0208-4589
Pojawia się w:
Prace i Studia Geograficzne
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wpływ cech teksturalnych na transport eoliczny w wybranych obszarach wydmowych północnej Sahary
Influence of textural features on aeolian transport in selected dune fields of the northern Sahara
Autorzy:
Dluzewski, M.
Powiązania:
https://bibliotekanauki.pl/articles/2084802.pdf
Data publikacji:
2009
Wydawca:
Uniwersytet Warszawski. Wydział Geografii i Studiów Regionalnych
Tematy:
Sahara Polnocna
cechy teksturalne
transport eoliczny
wydmy
piasek
ocena
Opis:
The aim of the study was to determine the influence of textural features of sand on aeolian transport in six designated fields in northern Sahara. An analysis of textural features such as: mineral composition, grain shape, mean grain size diameter and sorting were performed during a multi-year research on dune sediments. Information on the movement of small landforms (1.5m) in areas of similar physico-geographical environments was taken under consideration. It was revealed that the fastest movement, of about 90 my⁻¹, is characteristic for barchans on dune field no. 4. (where gypsum sand dominates). Barchans on dune field no. 1 are slower, with 50 my⁻¹ (where limestone dominates), and the slowest are those on dune field 6 (where quartz dominates), with about 30 my⁻¹. The result of the study proves that textural features have a significant influence on aeolian transport.
Źródło:
Prace i Studia Geograficzne; 2009, 41; 59-71
0208-4589
Pojawia się w:
Prace i Studia Geograficzne
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Źródło wilgoci w barchanach Sahary Zachodniej
Th e sources of moisture in the barchans of Western Sahara
Autorzy:
Dluzewski, M.
Zmudzka, E.
Woronko, D.
Biejat, K.
Powiązania:
https://bibliotekanauki.pl/articles/2084353.pdf
Data publikacji:
2012
Wydawca:
Uniwersytet Warszawski. Wydział Geografii i Studiów Regionalnych
Tematy:
Sahara
wilgotnosc
osady wydmowe
warunki meteorologiczne
transport eoliczny
barchany
Maroko
Opis:
The aim of the study was to determine the impact of climatic and meteorological conditions on aeolian sand transport within barchans. The study area was located at Western Sahara, around the towns of Tarfaya and Laâyoune. Particular attention was paid to the factors that increase the moisture content of the surface and subsurface layers of sand dunes. It could be one of the important factors to have an influence on threshold wind velocity. Western Sahara dune fields are situated in the zone of the dominant wind direction from the northern sector, which determines the barchan dunes shape and orientation, as well as the supply of moisture from the Atlantic Ocean. The results of investigations confirm that dunes receive quite a lot of moisture from rainfall and such phenomena as fog as well. Studies have confirmed that the water supply from the fog is comparable to, or even exceeds the amount of water from rainfall in the area. Wetted surface layer reduces the transport of aeolian material, even in case of a wind speed greater than 4-5 ms⁻¹. The presence of fog and dew does not affect the moisture of the deeper sand layers, which occurs after rainfall. Analysis of aeolian sand transport within the barchan dunes in the areas such a Western Sahara, should not be therefore limited to the measurement of wind speed and its direction. It must include the investigations on other meteorological elements, especially air temperature and humidity conditions, responsible for the amount of atmospheric deposits on the dune surface.
Źródło:
Prace i Studia Geograficzne; 2012, 49; 47-58
0208-4589
Pojawia się w:
Prace i Studia Geograficzne
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Rolnicze wykorzystanie wód na Saharze
The use of water for agriculture in the Sahara
Autorzy:
Walewski, A.
Powiązania:
https://bibliotekanauki.pl/articles/2084715.pdf
Data publikacji:
2010
Wydawca:
Uniwersytet Warszawski. Wydział Geografii i Studiów Regionalnych
Tematy:
Sahara
rolnictwo
wykorzystanie wody
nawadnianie gleby
opady atmosferyczne
suma opadow
wody opadowe
Opis:
The Sahara has exceptionally unfavourable natural conditions for farming. The extremely low precipitation and the high prevailing temperature allow for plant cultivation only in artificial irrigation conditions. The author discusses the regions' water resources (precipitation, surface and underground waters) and describes various ways of their use for agriculture. He also enumerates the main advantages and limitations of the technologies used, both traditional and modern, while placing special emphasis on the natural conditions of irrigated agriculture.
Źródło:
Prace i Studia Geograficzne; 2010, 44; 59-68
0208-4589
Pojawia się w:
Prace i Studia Geograficzne
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-4 z 4

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