2000
DOI: 10.1579/0044-7447-29.4.238
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Storm Influence on the Accumulation and Lamination of Sediments in Deep Areas of the Northwestern Baltic Proper

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Cited by 32 publications
(10 citation statements)
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“…In addition to this in area of erosion and transportation bottom resuspension of sediment induced by waves and currents, which in the Baltic Sea can be found to depths of 40-60 m (Danielsson et al, 2007), enhances degradation of organic matter and causes the removal of biogenic elements from sediment particles (Christiansen et al, 1997;Cyr et al, 2009). Sediment particles are subsequently transported seaward and accumulated in deeper basins (Eckhell et al, 2000;Christiansen et al, 2002;Damrat et al, 2013). As a consequence, ratios of OC:OP in sediments below the halocline tend to be higher than in the rest of the investigated area (Table 1; Fig.…”
Section: Spatial Distribution In Surface Sediment Layermentioning
confidence: 99%
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“…In addition to this in area of erosion and transportation bottom resuspension of sediment induced by waves and currents, which in the Baltic Sea can be found to depths of 40-60 m (Danielsson et al, 2007), enhances degradation of organic matter and causes the removal of biogenic elements from sediment particles (Christiansen et al, 1997;Cyr et al, 2009). Sediment particles are subsequently transported seaward and accumulated in deeper basins (Eckhell et al, 2000;Christiansen et al, 2002;Damrat et al, 2013). As a consequence, ratios of OC:OP in sediments below the halocline tend to be higher than in the rest of the investigated area (Table 1; Fig.…”
Section: Spatial Distribution In Surface Sediment Layermentioning
confidence: 99%
“…erosion or transportation) bottom -where deposition is interrupted by resuspension of sediments, to accumulation bottom -where conditions favour deposition (Jönsson et al, 2005). In other words, as wave-and current-induced resuspension prevents smaller particles from settling, they are transported seaward and deposited in deeper water basins (Eckhell et al 2000;Christiansen et al 2002;Emeis et al, 2000;Damrat et al, 2013). As a consequence, the percentage contribution of a fine grain fraction in sediment tends to increase with water depth (Eckhell et al, 2000;Hille et al, 2006), and this in turn leads to higher contents of water and organic matter in the sediment (Graca, 2009).…”
Section: Spatial Distribution In Surface Sediment Layermentioning
confidence: 99%
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“…Also the wind direction is of interest. If the fetch is large, the wave base (i.e., the water depth down to which the wave orbitals can resuspend fine partiOperational Effect Variables Table 7 (2000) demonstrate that resuspension correlates with winds higher than 7 m/s in four different archipelago areas in the Baltic Proper, whereas studies by ECKHELL et al (2000) indicate that wind speeds higher than 14 m/s correlate best with resuspension. BURBAN et al (1989BURBAN et al ( , 1990 have demonstrated that changes in water turbulence, SPM and salinity are also key regulatory factors for the aggregation and flocculation of suspended particles and hence also for the fall velocity.…”
Section: Suspended Particulate Matter (Spm)mentioning
confidence: 99%