2012
DOI: 10.1007/s10201-012-0372-x
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Long-term light environment variability in Lake Biwa and Lake Kasumigaura, Japan: modeling approach

Abstract: Light environment variability was investigated in the two Japanese lakes Biwa and Kasumigaura, which offer a broad range of optical conditions in the water bodies due to their diverse morphometries and limnological characteristics. To elucidate their light environments, Secchi depths (SDs) were related to long-term monitored datasets of concentrations of optically active substances (OASs) using two approaches based on statistical and mechanistic models. A good estimate for the nonphytoplanktonic suspended soli… Show more

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Cited by 8 publications
(5 citation statements)
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“…; Terrel et al . ). Although many hypotheses relating to biotic and/or abiotic factors were proposed for the increased sediment resuspension, no definitive conclusion currently exists (Fukushima et al .…”
Section: Discussionmentioning
confidence: 97%
See 1 more Smart Citation
“…; Terrel et al . ). Although many hypotheses relating to biotic and/or abiotic factors were proposed for the increased sediment resuspension, no definitive conclusion currently exists (Fukushima et al .…”
Section: Discussionmentioning
confidence: 97%
“…The increased T-Si in lake water was supported by laboratory experiments on Si release from suspended and bottom sediments (Arai et al 2012), and diatom dominance was predicted using a simple diatom growth model (Arai & Fukushima 2014). The high turbidity likely attributable to sediment resuspension (Fukushima et al 2005;Seki et al 2006;Terrel et al 2012). Although many hypotheses relating to biotic and/or abiotic factors were proposed for the increased sediment resuspension, no definitive conclusion currently exists (Fukushima et al 2005).…”
Section: Silicon (Si) Changes Around Shift Bmentioning
confidence: 96%
“…We used previously measured, average values of limnetic sites from each basin, 1.03 and 2.28, for a CDOM (320) for the North Basin and the South Basin, and 0.017 for S [ 85 , 92 ] ( S4B Appendix ). a NAP was estimated as a NAP = a NAP (440) exp(-S(λ-440)) [ 93 ]. We used 0.264 for a NAP (440) and 0.004 for S as typical values for the area ( S4C Appendix ).…”
Section: Methodsmentioning
confidence: 99%
“…We used previously measured, average values of limnetic sites from each basin, 1.03 and 2.28, for a CDOM ( 320) for the North Basin and the South Basin, and 0.017 for S [77,81] (S4 Appendix B). a NAP was estimated as a NAP = a NAP (440) EXP(-S (λ-440)) [82]. We used 0.264 for a NAP (440) and 0.004 for S as typical values for the area (S4 Appendix C).…”
Section: Methodsmentioning
confidence: 99%