Advertisement

Ocean Dynamics

, Volume 60, Issue 3, pp 629–629 | Cite as

Erratum to: A note on stokes production of turbulence kinetic energy in the oceanic mixed layer: observations in the Baltic Sea

  • Lakshmi KanthaEmail author
  • Hans Ulrich Lass
  • Hartmut Prandke
Erratum
  • 402 Downloads

Erratum to: Ocean Dynamics

DOI 10.1007/s10236-009-0257-7

The original version of this article unfortunately contained a mistake.

The first sentence of the first paragraph under “4. The results” section on page 177 of the article should read:

Figure 3 shows the time series of the wind stress components τ x , τ y , friction velocity u*, the surface Stokes drift speed \( \left| {{{\vec{U}}_S}} \right| \), \( \overline {{\eta^2}} \) and the Langmuir number La defined as \( La = {\left[ {\frac{{\left( {\vec{\tau }/\rho } \right) \cdot {{\vec{U}}_S}}}{{u_*^3}}} \right]^{1/3}} = {\left[ {\frac{{u_*^2\left| {{{\vec{U}}_S}} \right|}}{{u_*^3}}} \right]^{1/3}} = {\left[ {\frac{{\left| {{{\vec{U}}_S}} \right|}}{{{u_*}}}} \right]^{1/3}} \)since \( \vec{\tau } \) and \( {\vec{U}_S} \) are in the same direction. Note that this is a better way to define La than is the current practice since the larger the Langmuir number, the larger the Stokes production of TKE.

Copyright information

© Springer-Verlag 2010

Authors and Affiliations

  • Lakshmi Kantha
    • 1
    Email author
  • Hans Ulrich Lass
    • 2
  • Hartmut Prandke
    • 3
  1. 1.Department of Aerospace Engineering SciencesUniversity of ColoradoBoulderUSA
  2. 2.Baltic Sea Research InstituteRostockGermany
  3. 3.ISW WassermesstechnikPetersdorfGermany

Personalised recommendations