Coastal Engineering 2006 2007
DOI: 10.1142/9789812709554_0445
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Strudel Scour Formation Off Arctic River Deltas

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Cited by 7 publications
(8 citation statements)
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“…The change in strudel scour regime after start-up of operations has been investigated by Leidersdorf et al (2006). The change in strudel scour regime after start-up of operations has been investigated by Leidersdorf et al (2006).…”
Section: Strudel Scour and Hydrodynamic Scourmentioning
confidence: 99%
“…The change in strudel scour regime after start-up of operations has been investigated by Leidersdorf et al (2006). The change in strudel scour regime after start-up of operations has been investigated by Leidersdorf et al (2006).…”
Section: Strudel Scour and Hydrodynamic Scourmentioning
confidence: 99%
“…The change in strudel scour regime after start-up of operations has been investigated by Leidersdorf et al (2006). Annual monitoring of the strudel scours formed in the vicinity of the Northstar pipelines indicate that pipeline operations may locally increase the probability of scour formation.…”
Section: Strudel Scour and Hydrodynamic Scourmentioning
confidence: 99%
“…Annual monitoring of the strudel scours formed in the vicinity of the Northstar pipelines indicate that pipeline operations may locally increase the probability of scour formation. The cause of the increase in the frequency of scour formation over the pipelines may be the local thinning of the ice sheet above a buried warm pipeline in shallow water (Leidersdorf et al, 2006).…”
Section: Strudel Scour and Hydrodynamic Scourmentioning
confidence: 99%
“…Alternatively, dynamic sea-ice interaction with the shore may be destructive or constructive, depending on the situation, as ice-driven onshore can erode the backshore and damage infrastructure (Taylor, 1978;Kovacs and Sodhi, 1981), but may also nourish the shore zone through landward transport of nearshore sediments . In the Arctic during the spring thaw, river discharge onto a frozen ocean may drain through cracks and sinkholes to create distinctive strudel scour depressions on the seabed that represent a hazard to pipelines (Reimnitz and Bruder, 1972;Leidersdorf et al, 2006). Many other distinctive nearshore and beachface features attributable to shore ice on cold coasts are described later in the chapter (see also Forbes and Taylor, 1994;Byrne and Dionne, 2002).…”
Section: Ice As the Distinguishing Feature Of Polar And Subpolar Coastsmentioning
confidence: 99%
“…As overflow water begins to drain below the buoyant floating ice through tidal cracks or other orifices, the bottomfast ice remains bonded to the seabed. Strudel scour is now recognized as an active process with important implications for seabed infrastructure in the Prudhoe Bay field (Leidersdorf et al, 2006;Hearon et al, 2009) and the process has recently been confirmed off the Mackenzie Delta (Solomon et al, 2008). These are most abundant just beyond the transition from bot tomfast to floating ice in depths of 1.4-5 m (Reimnitz et al, 1974).…”
Section: Polar Deltasmentioning
confidence: 99%