Published September 19, 2019 | Version v1
Journal article Open

Numerical modeling outputs for 'Differential heating drives downslope flows that accelerate mixed-layer warming in ice-covered waters'

Authors/Creators

  • 1. Physics of Aquatic Systems Laboratory, Margaretha Kamprad Chair, École Polytechnique Fédérale de Lausanne, Institute of Environmental Engineering, Lausanne, Switzerland
  • 2. Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA, USA,
  • 3. Eawag, Swiss Federal Institute of Aquatic Science and Technology, Surface Waters – Research and Management, Kastanienbaum, Switzerland

Description

This dataset corresponds to the outputs of two numerical experiments performed to investigate the heating rate of radiatively heated ice-covered lakes. 

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Additional details

References

  • Winters, K. B., & de la Fuente, A. (2012). Modelling rotating stratified flows at laboratory-scale using spectrally-based DNS. Ocean. Model., 49-50, 47-59. doi:10.1016/j.ocemod.2012.04.001
  • Winters, K. B. (2016). The turbulent transition of a supercritical downslope flow: sensitivity to downstream conditions. J. Fluid Mech., 792 , 997-1012. doi: 10 482 .1017/jfm.2016.113
  • Winters, K. B., Ulloa, H. N., Wüest, A., & Bouffard, D. ( 2019). Energetics of radiatively heated ice‐covered lakes. Geophysical Research Letters, 46, 8913– 8925. https://doi.org/10.1029/2019GL084182
  • Ulloa, H. N., Winters, K. B., Wüest, A., & Bouffard, D.. ( 2019), Differential heating drives downslope flows that accelerate mixed‐layer warming in ice‐covered waters. Geophysical Research Letters, 46. https://doi.org/10.1029/2019GL085258