2005
DOI: 10.1016/j.ecolmodel.2005.03.015
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Suspended particulate matter (SPM) in the Baltic Sea—New empirical data and models

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Cited by 27 publications
(14 citation statements)
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“…In addition, there are lower TSM concentrations in the deep open ocean [13], [18]. Therefore, a significant negative correlation was found between water depth and TSM concentration in the coastal areas and open ocean [36], [37]. The difference between large shallow lakes and oceans was partly attributed to the entirety of Lake Taihu suffering sediment resuspension because of its shallow water depth and high dynamic ratio (the square root of the surface area divided by the mean depth), which was as high as 25.6 km m −1 (100% of the lake bottom subject to sediment resuspension) [38], whereas only part of the coastal waters suffered from sediment resuspension in the ocean.…”
Section: Discussionmentioning
confidence: 95%
“…In addition, there are lower TSM concentrations in the deep open ocean [13], [18]. Therefore, a significant negative correlation was found between water depth and TSM concentration in the coastal areas and open ocean [36], [37]. The difference between large shallow lakes and oceans was partly attributed to the entirety of Lake Taihu suffering sediment resuspension because of its shallow water depth and high dynamic ratio (the square root of the surface area divided by the mean depth), which was as high as 25.6 km m −1 (100% of the lake bottom subject to sediment resuspension) [38], whereas only part of the coastal waters suffered from sediment resuspension in the ocean.…”
Section: Discussionmentioning
confidence: 95%
“…Suspended matter of terrestrial origin settles close to the coast [22]. Low mineral particle load combined with high CDOM concentrations results in a combination of weak light scattering and strong absorption.…”
Section: Introductionmentioning
confidence: 99%
“…The CDOM concentration undergoes seasonal variation, typically reflecting changes in river runoff (Asmala et al, 2012;Kowalczuk et al, 2010). Suspended particulate matter mostly originates from terrigenous inputs or bottom resuspension (Håkanson and Eckhéll, 2005), and may dominate underwater light attenuation, especially close to the mainland (Luhtala et al, 2013). The phytoplankton related PAR attenuation follows well-recognised seasonal development that is controlled by biogeochemical cycles of nutrients: the spring bloom is dominated by diatoms and dinoflagellates exploiting nitrogen, and after the early summer phytoplankton minimum, nitrogen-fixing cyanobacteria bloom, utilising the remaining phosphorus better than the species that suffer from nitrogen limitation (Hällfors et al, 1981).…”
Section: Methodsmentioning
confidence: 99%