| contributor author | Noh, Yign | |
| contributor author | Choi, Yeonju | |
| date accessioned | 2019-09-19T10:02:31Z | |
| date available | 2019-09-19T10:02:31Z | |
| date copyright | 2/1/2018 12:00:00 AM | |
| date issued | 2018 | |
| identifier other | jpo-d-17-0135.1.pdf | |
| identifier uri | http://yetl.yabesh.ir/yetl1/handle/yetl/4260884 | |
| description abstract | AbstractUsing 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. | |
| publisher | American Meteorological Society | |
| title | Comments on “Langmuir Turbulence and Surface Heating in the Ocean Surface Boundary Layer” | |
| type | Journal Paper | |
| journal volume | 48 | |
| journal issue | 2 | |
| journal title | Journal of Physical Oceanography | |
| identifier doi | 10.1175/JPO-D-17-0135.1 | |
| journal fristpage | 455 | |
| journal lastpage | 458 | |
| tree | Journal of Physical Oceanography:;2018:;volume 048:;issue 002 | |
| contenttype | Fulltext | |
