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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:
Wieloletni bilans osadu wydm nadmorskich Mierzei Bramy Świny
The multi-annual sediment balance of the Swina Gate Sandbar coastal dunes
Autorzy:
Labuz, T.
Powiązania:
https://bibliotekanauki.pl/articles/2084344.pdf
Data publikacji:
2012
Wydawca:
Uniwersytet Warszawski. Wydział Geografii i Studiów Regionalnych
Tematy:
wydmy nadmorskie
mierzeje
Mierzeja Bramy Swiny
bilans
Opis:
The study area is located on the Islands of Wolin and Uznam on the Pomeranian Bay coast (Southern Baltic). In Poland, the barrier extends for 16 km. It consists of two sand spits formed between morainic plateau of these islands. At present, the entire barrier is covered by dune ridges formed since Atlantic period (5 000 BP). The youngest ridges (White Dunes) have been growing up since 17th century. Here, during last the 20 years two foredunes have grown up. The last one arose between 1997-2001. On this area author has been carried investigations since end of 1996. Investigations consist of relief measurements of different dune ridges and deflation hollows, phytosociological transects across the ridges (dune vegetation cover and variability of plant species), surface sand sampling and wind measurements. In this work long term of the foredune and upper beach changes were described. In separate parts of the sandbar, during last 14 years abrasion and aeolian processes with plants influence played main role. In the end of 2007, near profile 420th km (middle part of sandbar) on the upper beach embryo dunes formed ridge up to 4 m high. Now this form is rebuild into a new foredune. The foredune and the beach in the middle part of the sandbar are now sufficiently stabilized by grasses and wide enough to withstand heaviest storms. In other parts of sandbar dunes are stili affected by abrasional processes. Sand volume changes show visible increase of the foredunes in accumulative - middle part of the studied place. Sand volume dynamics rate in foredunes reached up to 120 m³ per one meter wide profile in the middle part of sandbar. Accumulation there reached up to 40 m³/m.
Źródło:
Prace i Studia Geograficzne; 2012, 49; 69-89
0208-4589
Pojawia się w:
Prace i Studia Geograficzne
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zmienność kształtu wydm gwiaździstych w obszarach o bimodalnym reżimie wiatru
Star dune shape variability in the area of bimodal wind regime
Autorzy:
Biejat, K.
Powiązania:
https://bibliotekanauki.pl/articles/2084348.pdf
Data publikacji:
2012
Wydawca:
Uniwersytet Warszawski. Wydział Geografii i Studiów Regionalnych
Tematy:
wydmy gwiazdziste
ksztalt wydm
rezim wiatru
rezim bimodalny
wiatry
Opis:
Contemporary morphological changes of star dunes are observed mainly in certain parts of these dunes. They occur as lateral migration of crestlines of dune arms and modifications of inclination of their slopes. The aim of the research was to determine annual variability of shapes of compound and complex star dunes in bimodal wind regime. Precise measurements of 5 star dunes were performed with use of GPS RTK in March, 2011, and March, 2012, on Erg Chebbi (Morocco). Based on these measurements, 3D models of the dunes were created, which in turn, allowed for calculation of annual magnitude and direction of crestlines migration of star dune main arms. The results show that the resultant drift direction was in accordance with long-term regime of active wind in the study area. Both, the resultant drift direction and its magnitude were similar in all studied dunes. Variability of star dune shapes occurred to be independent from their stage of development (size of a dune) or its type. The most important feature determining morphodynamics of the star dune arms are: i) the angle between the arms and the active wind, and ii) slope inclination of the arms.
Źródło:
Prace i Studia Geograficzne; 2012, 49; 33-45
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
    Wyświetlanie 1-4 z 4

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