Max Engel, Fabian Boesl, and Helmut Brückner (2018)
Anthropogenic and environmental controls of barchan dune dynamics in Qatar
In: BOOK OF ABSTRACTS - Central European Conference on Geomorphology and Quaternary Sciences Joint Conference of AKG and DEUQUA University of Giessen, Germany September 23 – 27, 2018, pp. 95.
Barchan dunes are crescentic aeolian landforms of loose, mostly well-sorted sand with a
convex side directed upwind and two horns pointing downwind. Their migration is mainly
controlled by sand supply, dune size, wind patterns, vegetation cover and human impact. In
Qatar, their distribution is limited to the southeastern part of the peninsula, where they play
an important role for tourism and camping activities among locals. We investigate the
variability of dune migration in Qatar over a time period of 50 years using high-resolution
satellite and aerial imagery. We then explore its relation to the regional Shamal wind system
(NNW–SSE), teleconnection patterns, and limitations in sand supply associated with the
transgression of the Arabian Gulf, which explain the fact that Qatar is gradually being
stripped from aeolian landforms with a remaining dune population in the southeast. Strong
size-dependent differences in migration rates of individual dunes as well as significant
decadal variability on a dune-field scale are detected, the latter closely correlating with
summer Shamal activity. The summer Shamal itself is mainly driven by pressure differences
between the stationary anticyclone over the eastern Mediterranean and the established
summer heat low over Iran and adjacent areas. It seems to be related to the intensity of the
North Atlantic Oscillation and the Indian Summer Monsoon, in particular during years of
relatively strong (weak) summer Shamals. High uncertainties associated with the
extrapolation of migration rates back into the Holocene, however, do not permit further
refining of the timing of the loss of sand supply and the onset of the mid-Holocene relative
sea-level (RSL) highstand. For the youngest phase considered in this study (2006–2015),
human impact has significantly accelerated dune migration under a more or less stable
Shamal regime through systematic sand mining and excessive vehicle traffic upwind of the
core study area, which started in 2007.
Abstract of an Oral Presentation or a Poster
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