| contributor author | Pearson, Brodie C. | |
| contributor author | Grant, Alan L. M. | |
| contributor author | Polton, Jeff A. | |
| contributor author | Belcher, Stephen E. | |
| date accessioned | 2019-09-19T10:02:39Z | |
| date available | 2019-09-19T10:02:39Z | |
| date copyright | 2/1/2018 12:00:00 AM | |
| date issued | 2018 | |
| identifier other | jpo-d-17-0176.1.pdf | |
| identifier uri | http://yetl.yabesh.ir/yetl1/handle/yetl/4260911 | |
| description abstract | AbstractThe differences between the conclusions of Noh and Choi and of Pearson et al., which are largely a result of defining different length scales based on different quantities, are discussed. This study shows that the layer over which Langmuir turbulence mixes (nominally hTKE) under a stabilizing surface buoyancy flux should be scaled by a combination of the Langmuir stability length LL and initial/nocturnal boundary layer depth h0 rather than by the Zilitinkevich length. | |
| publisher | American Meteorological Society | |
| title | Reply to “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-17-0176.1 | |
| journal fristpage | 459 | |
| journal lastpage | 462 | |
| tree | Journal of Physical Oceanography:;2018:;volume 048:;issue 002 | |
| contenttype | Fulltext | |
