Supporting Data for "Measuring gas transfer velocity in a steep tropical stream: method evaluation and implications or upscaling"
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This contains two datasets that support the manuscript referenced in the titleK<sub>600</sub> dataset contains the k<sub>600</sub> values and hydrology parameters for the study sites. See sections 2.2-2.6 for more details on the methodology for each method. The columns are as follows:Date: YYYY-MM-DDSite: Denotes the siteRaymond2: K<sub>600</sub> calculated from Raymond eq 2 (m d<sup>-1</sup>)Raymond5: K<sub>600</sub> calculated from Raymond eq 5 (m d<sup>-1</sup>)Natchimuthu: K<sub>600</sub> calculated from Natchimuthu (m d<sup>-1</sup>)Ulseth: K<sub>600</sub> calculated from Ulster (m d<sup>-1</sup>)Chamber: K<sub>600</sub> calculated from the floating chamber (m d<sup>-1</sup>)CO2.MassBalance: K<sub>600</sub> calculated from the CO2 tracer gas as a mass balance (m d<sup>-1</sup>)CO2.FirstOrder: K<sub>600</sub> calculated from the CO2 tracer gas as a first order (m d<sup>-1</sup>)Propane.FirstOrder: K<sub>600</sub> calculated from the propane tracer gas as a first order (m d<sup>-1</sup>)V: flow velocity (m s<sup>-1</sup>)Q: flow rate (L s<sup>-1</sup>)<br>The fluxes dataset contains upscaled flux estimates for three different day for the entire study reach using 9 different methods. See section 2.7 and SI Text 2 for detailed info. All flux units are mol CO<sub>2</sub> d<sup>-2</sup>.<br>
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figshare
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2024-12-06



