Abstract
Using large-eddy simulations (LES) it is shown that the depth of a diurnal thermocline h should be scaled by the Zilitinkevich scale LZ, not by the Monin-Obukhov length scale LMO, contrary to the proposition by Pearson et al. Their argument to explain the slower increase of h than LMO using the effect of the preexisting thermocline is also invalid.
Original language | English |
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Pages (from-to) | 455-458 |
Number of pages | 4 |
Journal | Journal of Physical Oceanography |
Volume | 48 |
Issue number | 2 |
DOIs | |
Publication status | Published - 2018 Feb 1 |
Bibliographical note
Funding Information:Acknowledgments. This work was supported by the National Research Foundation of Korea grant funded by the Korean government (MEST Grant NRF-2009-C1AAA001-0093068).
Publisher Copyright:
© 2018 American Meteorological Society.
All Science Journal Classification (ASJC) codes
- Oceanography