Coastal Engineering 1996 1997
DOI: 10.1061/9780784402429.341
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Design Considerations for Coastal Projects in Cold Regions

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Cited by 5 publications
(7 citation statements)
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“…If the drainage rate is high, hydrodynamics (high velocity currents) of the draining water at the seafloor can scour seabed sediment (leaving a circular or linear scour in the seabed), which can potentially expose and impose high current loads on a pipeline ( Figure 2). These are known as strudel scours and they usually occur in 2 to 8m (6.6 to 26.2ft) depth offshore from river deltas (Leidersdorf et al, 1996).It is unlikely that every drain hole in the sheet ice produces a scour in the seafloor. The deepest scours are found in shallow water (i.e.…”
Section: Strudel Scour and Hydrodynamic Scourmentioning
confidence: 99%
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“…If the drainage rate is high, hydrodynamics (high velocity currents) of the draining water at the seafloor can scour seabed sediment (leaving a circular or linear scour in the seabed), which can potentially expose and impose high current loads on a pipeline ( Figure 2). These are known as strudel scours and they usually occur in 2 to 8m (6.6 to 26.2ft) depth offshore from river deltas (Leidersdorf et al, 1996).It is unlikely that every drain hole in the sheet ice produces a scour in the seafloor. The deepest scours are found in shallow water (i.e.…”
Section: Strudel Scour and Hydrodynamic Scourmentioning
confidence: 99%
“…If the drainage rate is high, hydrodynamics (high velocity currents) of the draining water at the seafloor can scour seabed, which can potentially expose and impose high current loads on a pipeline. These are known as strudel scours and they usually occur in 2 to 8m (6.6 to 26.2ft) depth offshore from river deltas (Leidersdorf et al, 1996). Hydrodynamic scour may reduce the cover initially placed over a pipeline and long-term sediment migration should be assessed and considered as part of burial depth requirements.…”
Section: Introductionmentioning
confidence: 99%
“…Further descriptions of coastal engineering issues in the Alaskan Arctic have been previously presented (Leidersdorf, et al, 1996;1990;1982).…”
Section: Figure 2 Man-made Islands In the Alaskan Beaufort Seamentioning
confidence: 99%
“…In the absence of long-term measurements in the Alaskan Beaufort Sea, it was necessary to develop design water level and wave conditions using a numerical hindcast approach (Leidersdorf, et al, 1996). Boundary conditions for site-specific surge and wave models were derived from a synoptic hindcast study prepared as a Joint Industry Project known as "BORE" ("Beaufort Sea Response Extremes"; Oceanweather, 2005).…”
Section: Oceanographic Design Conditionsmentioning
confidence: 99%