2022
DOI: 10.1016/j.jenvman.2022.115082
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Annual water residence time effects on thermal structure: A potential lake restoration measure?

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Cited by 20 publications
(6 citation statements)
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“…The advective heat flux has a larger effect in lakes with shorter residence times and can have a warming or cooling effect on lake water temperature, depending on the seasonal differences between the inflow and lake surface temperature. For example, Olsson et al (2022) found that advective heat flux can be a warming flux in winter and a cooling flux in summer, and that the magnitude of the advective heat flux is determined by the annual water retention time, with the lower the advective heat flux the longer the annual water retention time.…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…The advective heat flux has a larger effect in lakes with shorter residence times and can have a warming or cooling effect on lake water temperature, depending on the seasonal differences between the inflow and lake surface temperature. For example, Olsson et al (2022) found that advective heat flux can be a warming flux in winter and a cooling flux in summer, and that the magnitude of the advective heat flux is determined by the annual water retention time, with the lower the advective heat flux the longer the annual water retention time.…”
Section: Discussionmentioning
confidence: 99%
“…For example, Olsson et al. (2022) found that advective heat flux can be a warming flux in winter and a cooling flux in summer, and that the magnitude of the advective heat flux is determined by the annual water retention time, with the lower the advective heat flux the longer the annual water retention time.…”
Section: Discussionmentioning
confidence: 99%
“…1D lake models are also frequently used to evaluate the effect of meteorological extreme events on in‐lake mixing and heat transport (e.g., Bueche et al., 2017; Mesman et al., 2021; Perga et al., 2018; Shinohara et al., 2023). Further, 1D lake models are frequently used for quantifying heat and mass transport in water bodies and therefore to infer and adapt water management (e.g., Barbosa et al., 2021; Ladwig et al., 2018; Mi et al., 2018; Olsson, 2022; Soares et al., 2019; Weber et al., 2017). Also, important ecological information like the thermal habitat or the solubility of gases can be inferred from the vertical distribution of water temperature (e.g., Butcher et al., 2015; Magee et al., 2019).…”
Section: Classification Of Lake Temperature Modelsmentioning
confidence: 99%
“…These studies suggested that river intrusion and thermal stratification are key factors shaping the seasonal and interannual patterns of C fluxes during typhoon disturbances. River intrusion not only controlled the C fluxes, algal biomass, and nutrient loading, but also influenced the length of stratification and hydraulic retention times (Lin et al, 2021;Lin et al, 2022;Maranger et al, 2018;Nakayama et al, 2020;Olsson et al, 2022a;Olsson et al, 2022b;Zwart et al, 2017;Vachon and Del Giorgio, 2014). We hypothesized that allochthonous C loading and river inflow intrusion may affect the DIC and DOC distributions (Figure 1).…”
Section: Introductionmentioning
confidence: 95%
“…The responses of C fluxes in small lakes (lake area < 1 km 2 ) are sensitive to climate change due to the ease with which these C mix with water columns (Doubek et al, 2021;MacIntyre et al, 2021;Winslow et al, 2015). Moreover, storms induce dramatic changes in thermal stratification and water inflows (Lin et al, 2022;Olsson et al, 2022b;Vachon and Del Giorgio, 2014;Woolway et al, 2018). River inflows and wind turbulence mix the allochthonous C from sediments into the water column after storm events in small stratified lakes (Bartosiewicz et al, 2015;Czikowsky et al, 2018;Vachon and Del Giorgio, 2014).…”
Section: Introductionmentioning
confidence: 99%