Energy input and dissipation in a temperate lake during the spring transitionReportar como inadecuado




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Ocean Dynamics

pp 1–13

First Online: 07 June 2017Received: 18 October 2016Accepted: 19 May 2017DOI: 10.1007-s10236-017-1072-1

Cite this article as: Woolway, R.I. & Simpson, J.H. Ocean Dynamics 2017. doi:10.1007-s10236-017-1072-1

Abstract

ADCP and temperature chain measurements have been used to estimate the rate of energy input by wind stress to the water surface in the south basin of Windermere. The energy input from the atmosphere was found to increase markedly as the lake stratified in spring. The efficiency of energy transfer Eff, defined as the ratio of the rate of working in near-surface waters RW to that above the lake surface P10, increased from ∼0.0013 in vertically homogenous conditions to ∼0.0064 in the first 40 days of the stratified regime. A maximum value of Eff∼0.01 was observed when, with increasing stratification, the first mode internal seiche period decreased to match the diurnal wind period of 24 h. The increase in energy input, following the onset of stratification was reflected in enhancement of the mean depth-varying kinetic energy without a corresponding increase in wind forcing. Parallel estimates of energy dissipation in the bottom boundary layer, based on determination of the structure function show that it accounts for ∼15% of RW in stratified conditions. The evolution of stratification in the lake conforms to a heating stirring model which indicates that mixing accounts for ∼21% of RW. Taken together, these estimates of key energetic parameters point the way to the development of full energy budgets for lakes and shallow seas.

KeywordsLakes Shelf seas Mixing Stratification Dissipation R. Iestyn Woolway and John H. Simpson contributed equally to this work.

Responsible Editor: Emil Vassilev Stanev





Autor: R. Iestyn Woolway - John H. Simpson

Fuente: https://link.springer.com/







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