2011
DOI: 10.1016/j.envsoft.2011.05.006
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Derivation of lake mixing and stratification indices from high-resolution lake buoy data

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Cited by 390 publications
(325 citation statements)
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“…Two physical factors (wind and rain) appear to be the main drivers of metabolism across multiple temporal scales, likely by altering lake stratification and mixing. Less wind and rain promote increased stability of the water column, as determined by buoyancy frequency, lake number, and Schmidt stability (Read et al 2011). For all of these metrics, greater stability was positively correlated with GPP and R in Lake Sunapee (Table 2).…”
Section: Drivers Of Intra-annual Metabolism Trendsmentioning
confidence: 92%
See 1 more Smart Citation
“…Two physical factors (wind and rain) appear to be the main drivers of metabolism across multiple temporal scales, likely by altering lake stratification and mixing. Less wind and rain promote increased stability of the water column, as determined by buoyancy frequency, lake number, and Schmidt stability (Read et al 2011). For all of these metrics, greater stability was positively correlated with GPP and R in Lake Sunapee (Table 2).…”
Section: Drivers Of Intra-annual Metabolism Trendsmentioning
confidence: 92%
“…We used the buoy data to calculate a number of physical lake metrics at the 10-min scale using thermistor data, including buoyancy frequency, lake number, and Schmidt stability of Lake Sunapee during the monitoring period (Read et al 2011;Bruesewitz et al 2015). We obtained precipitation and air temperature data for 20 May to 15 October for 2008-2013 from the National Climate Data Center (NCDC) website (ncdc.noaa.gov/cdo-web/search, last accessed on 14 October 2014) for Newport, New Hampshire, which is 10 km from the LSPA buoy.…”
Section: Drivers Of Daily Metabolismmentioning
confidence: 99%
“…We determined the depth of epilimnion as the shallowest depth with a water-density gradient equal to or above a suitable threshold (, 0.07 kg m 23 m 21 ) for each time step according to Read et al (2011) and will refer to that depth as Z mix . Water density was calculated from temperature (in uC) assuming negligible effects of solutes as in Read et al (2011). The thermocline depth was defined as the depth with the maximum temperature gradient, and the lower limit of the metalimnion was calculated as thermocline depth plus the distance between Z mix and the thermocline.…”
Section: Methodsmentioning
confidence: 99%
“…An in-depth description of the state-of-the art in measuring and computing lake metabolism, based on high-frequency free-water gas measurements (Staehr et al 2010), helped catalyze researchers to improve measurements as well as the software commonly used in metabolism calculations (Winslow et al 2016). The use of lake physics indices has become more accessible to ecologists through the development of software (LakeMetabolizer; Read et al 2011) that calculates common metrics of lake physical state, such as the depth of the thermocline, Schmidt stability, and buoyancy frequency. The biophysical dynamics of lakes and reservoirs are difficult to model due to ecosystem complexity; however, through leadership of GLEON members with expertise in numerical simulation, an open-source numerical simulation (GLM -AED2) has been developed as a community initiative in support of community needs (Hipsey et al 2013).…”
Section: Multiscale Observationsmentioning
confidence: 99%