2003
DOI: 10.1016/s1385-1101(03)00023-6
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Water exchange of the Stockholm archipelago—a cascade framework modelling approach

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Cited by 29 publications
(19 citation statements)
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“…Using long-term data on salinity, it was possible to calculate the average inflow to approximately 325 m 3 s -1 . This order of magnitude is close to what Engqvist and Andrejev (2003) found using a fine resolution hydrodynamical model to calculate the water exchange in Stockholm archipelago for the year 1992. The average inflow in that year was calculated to be around 390 m 3 s -1 (Engqvist and Andrejev 2003).…”
Section: Methodssupporting
confidence: 86%
See 1 more Smart Citation
“…Using long-term data on salinity, it was possible to calculate the average inflow to approximately 325 m 3 s -1 . This order of magnitude is close to what Engqvist and Andrejev (2003) found using a fine resolution hydrodynamical model to calculate the water exchange in Stockholm archipelago for the year 1992. The average inflow in that year was calculated to be around 390 m 3 s -1 (Engqvist and Andrejev 2003).…”
Section: Methodssupporting
confidence: 86%
“…The inflow of water from the outer archipelago goes mainly (around 85%) through the sound Oxdjupet (Fig. 1), but also through the sounds, Kodjupet, Stegesund, Skävsjö-holmssundet, and Baggen-Stäket (Engqvist and Andrejev 2003). The total inflow of water from outside areas to the inner archipelago was calculated through simple mass balance calculations for salt, applying Knudsen's relations (Knudsen 1900).…”
Section: Methodsmentioning
confidence: 99%
“…The transport processes are both advective and diffusive driven by the interacting flows of the northern basins of the Baltic Sea and the North Sea [58]. Particles from Arkona Basin flow northwards along the Stolpe Channel, which is in agreement with Meier et al [6].…”
Section: Transport Mechanismsupporting
confidence: 87%
“…To consider the transport of Cu through the system of recipients, we propose to follow the approach of Engqvist and Andrejev [15] and divide the surface water into connected basins and straits based on geometric form, with straits being narrow, with an associated, expected lower water residence time ( Figure 3). In order to trace the Cu through the system, the water flow through the straits between the basins must be established.…”
Section: Propagation and Fate Of Copper Downstream Of The Sourcementioning
confidence: 99%
“…For the archipelago, Engqvist and Andrejev [15] already suggested a partitioning into basins and straits; for Lake Mälaren and the transitional region, we consider the water bodies with slender form as straits, whereas others were considered as basins ( Figure 6). Basins with a maximum depth of more than 10m were considered deep (full contour ellipse in Figure 6), whereas the rest were considered shallow (dashed contour ellipse in Figure 6).…”
Section: Figurementioning
confidence: 99%