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2012 | 49 |

Tytuł artykułu

Źródło wilgoci w barchanach Sahary Zachodniej

Treść / Zawartość

Warianty tytułu

EN
Th e sources of moisture in the barchans of Western Sahara

Języki publikacji

PL

Abstrakty

EN
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.

Wydawca

-

Rocznik

Tom

49

Opis fizyczny

s.47-58,rys.,tab.,wykr.,fot.,bibliogr.

Twórcy

autor
  • Zakład Geomorfologii, Wydział Geografii i Studiów Regionalnych, Uniwersytet Warszawski w Warszawie, Warszawie
autor
  • Zakład Klimatologii, Wydział Geografii i Studiów Regionalnych, Uniwersytet Warszawski w Warszawie, Warszawie
autor
  • Zakład Hydrologii, Wydział Geografii i Studiów Regionalnych, Uniwersytet Warszawski w Warszawie, Warszawie
autor
  • Zakład Geomorfologii, Wydział Geografii i Studiów Regionalnych, Uniwersytet Warszawski w Warszawie, Warszawie

Bibliografia

  • Bagnold R.A., 1941, The Physics of Blown Sand and Desert Dunes, Chapman & Hall, London.
  • Belly P.Y., 1964, Sand Movement by Wind, Technical Memorandum 1, Addendum III, US Army Corps of Engineers, Coastal Engineering Research Center, Washington, DC.
  • Berndtsson R., Nodomi K., Yasuda H., Persson T., Chen H., Jinno K., 1996, Soil water and temperature patterns in arid desert dune sand, Journal of Hydrology 185, 221-240.
  • Glennie K.W., 1987, Desert sedimentary environments, past and present - a summary, Sedimentary Geology 50, 135-166.
  • Lancaster N., 1995, Geomorphology of desert dunes, Routledge, London.
  • Martyn D., 2000, Klimaty kuli ziemskiej, Wydawnictwo Naukowe PWN, Warszawa.
  • Marzol M.V., Sánchez J.L., Yanes A., 2011, Meteorological patterns and fog water collection in Marocco and the Canary Islands, Erdkunde, 65, 291-303.
  • Oulehri T., 1992, Etude géodynamique des migrations de sables éoliens dans la région de Laâyoune (Nord du Sahara marocain), Ph. D. Thesis, l'Universite Paris 6, Paris, 92-12.
  • Subramanian A.R., Kesava-Rao A.V.R., 1983, Dew fall in sand dune areas of India, International Journal of Biometeorology 27, 271-280.
  • Thomas D.S.G., 1997, Arid environments: their nature and extent. [w:] D.S.G. Thomas (red.), Arid Zone Geomorphology. Process, Form and Change in Drylands, John Wiley & Sons, Chichester: 3-12.
  • Wasson R.J., Hyde R., 1983, A test of granulometric control of desert dune geometry,Earth Surface Processes and Landforms 8, 301-312.
  • Wiggs G.F.S., 2000, Sediment mobilisation by the wind, [w:] D.S.G. Thomas (red.), Arid Zone Geomorphology, Process, Form and Change in Drylands, John Wiley & Sons, Chichester, 351-372.
  • www.noaa.gov (30.03.2012)
  • www.wetterzentrale.de (30.03.2012)
  • Yair A., Lavee H., Greister N., 1997, Spatial and temporal variability of water percolation and movement in a system of longitudinal dunes, Western Negev, Israel. Hydrological Processes 11, 43-58.

Typ dokumentu

Bibliografia

Identyfikatory

Identyfikator YADDA

bwmeta1.element.agro-aab230d4-97f0-4562-9d6c-940551aab83a
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