An inertial‐dissipation method for estimating turbulent flux in buoyancy‐driven, convective boundary layers
- 15 February 1998
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Oceans
- Vol. 103 (C2) , 3249-3255
- https://doi.org/10.1029/97jc02263
Abstract
No abstract availableKeywords
This publication has 10 references indexed in Scilit:
- Lead convection measured with an autonomous underwater vehicleJournal of Geophysical Research: Oceans, 1998
- Turbulence in the statically unstable oceanic boundary layer under Arctic leadsJournal of Geophysical Research: Oceans, 1996
- On the Turbulent Mixing Length in the Oceanic Boundary LayerJournal of Physical Oceanography, 1994
- Turbulent Mixing Under Drifting Pack Ice in the Weddell SeaScience, 1994
- The LeadEx experimentEos, 1993
- The oceanography of winter leadsJournal of Geophysical Research: Oceans, 1992
- A study of the inertial‐dissipation method for computing air‐sea fluxesJournal of Geophysical Research: Oceans, 1991
- The Skewness of Temperature Derivatives in Oceanic Boundary LayersJournal of Physical Oceanography, 1991
- Convectively Driven Turbulent Mixing in the Upper OceanJournal of Physical Oceanography, 1986
- Spectral Scaling in a Tidal Boundary LayerJournal of Physical Oceanography, 1985