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The formation and closure of the Big Breach of Sacalin spit associated with extreme shoreline retreat and shoreface erosion
Author(s) -
Zăinescu Florin Iulian,
VespremeanuStroe Alfred,
Tătui Florin
Publication year - 2019
Publication title -
earth surface processes and landforms
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.294
H-Index - 127
eISSN - 1096-9837
pISSN - 0197-9337
DOI - 10.1002/esp.4639
Subject(s) - overwash , geology , barrier island , shore , erosion , sediment transport , longshore drift , coastal erosion , bed load , deposition (geology) , aggradation , geomorphology , sediment , bathymetry , oceanography , hydrology (agriculture) , geotechnical engineering , fluvial , structural basin
We document a case of exceptionally large natural breaching of a sandy spit (Sacalin spit, Danube Delta) using multiannual to seasonal surveys of topography and bathymetry on successive cross‐barrier and shoreface profiles, LiDAR data, satellite imagery, and wind and wave data. The large breach, which quickly reached 3.4 km in May 2014, is attributed to morphological preconditioning of the narrow (50–150 m) barrier, which was susceptible to breaching even during moderate storm conditions. The event switched the barrier's decadal evolution from low cross‐shore transport to high cross‐shore transport over the barrier, which is an order of magnitude larger than during the non‐breach period. Upper shoreface erosion, as indicated by the extensive erosion down to −4 m, indicates that this zone is a significant source for the rebuilding of the barrier. Barrier recovery and widening trigger a negative feedback which limits the back‐barrier sediment transfer. As a result, back‐barrier deposition decreases whilst the barrier aggradation through overwash becomes more frequent. The Big Breach (TBB) closed naturally in three years. The very high deposition rate of sediment in the breach is a testimony of the high sediment volumes supplied by the longshore transport and the high sediment released through shoreface retreat, and resulted in widening the barrier to a maximum of 1 km. Since the newly‐formed barrier shoreline retreated 500 m, this reveals that barrier breaching is an important mechanism which significantly accelerates the landward migration of the barrier system and is a proof of the highly non‐linear morphodynamics involved in the barrier island translation. © 2019 John Wiley & Sons, Ltd.