4.7 Article

Derivation of lake mixing and stratification indices from high-resolution lake buoy data

Journal

ENVIRONMENTAL MODELLING & SOFTWARE
Volume 26, Issue 11, Pages 1325-1336

Publisher

ELSEVIER SCI LTD
DOI: 10.1016/j.envsoft.2011.05.006

Keywords

Lake analyzer; Stability; Mixing; Lake number; Wedderburn number; Schmidt stability; Thermocline depth; Software; Instrumented buoy; GLEON

Funding

  1. National Science Foundation [DBI-0446017, DBI-0639229]
  2. Gordon and Betty Moore Foundation
  3. Natural Environment Research Council [ceh010022] Funding Source: researchfish
  4. Direct For Biological Sciences
  5. Division Of Environmental Biology [0941510, 0941573] Funding Source: National Science Foundation
  6. Direct For Biological Sciences
  7. Division Of Environmental Biology [822700] Funding Source: National Science Foundation

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Lake Analyzer is a numerical code coupled with supporting visualization tools for determining indices of mixing and stratification that are critical to the biogeochemical cycles of lakes and reservoirs. Stability indices, including Lake Number, Wedderburn Number, Schmidt Stability, and thermocline depth are calculated according to established literature definitions and returned to the user in a time series format. The program was created for the analysis of high-frequency data collected from instrumented lake buoys, in support of the emerging field of aquatic sensor network science. Available outputs for the lake Analyzer program are: water temperature (error-checked and/or down-sampled), wind speed (error-checked and/or down-sampled), metalimnion extent (top and bottom), thermocline depth, friction velocity, Lake Number, Wedderburn Number, Schmidt Stability, mode-1 vertical seiche period, and Brunt-Vaisala buoyancy frequency. Secondary outputs for several of these indices delineate the parent thermocline depth (seasonal thermocline) from the shallower secondary or diurnal thermocline. Lake Analyzer provides a program suite and best practices for the comparison of mixing and stratification indices in lakes across gradients of climate, hydro-physiography, and time, and enables a more detailed understanding of the resulting biogeochemical transformations at different spatial and temporal scales. (C) 2011 Elsevier Ltd. All rights reserved.

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