the Atmospheric and Oceanic Boundary Layers During Convection with the Latitudinal Dependence

These are the large eddy simulation data which are used for comparing the boundary layers of the atmosphere and the ocean during convection and investigating their latitudinal dependence.The data are obtained by using PALM (https://palm.muk.uni-hannover.de/trac) . The configuration of Langmuir circulation is the same as in Noh et al. (2011). The simulations are conducted with two different latitudes (10N, 40N). The period of integration is twice the inertial time scale of each latitude. Constant wind stress (u*=0~0.02m/s) or geostrophic wind(Ug=0~20m/s) is applied in ocean and atmosphere simulations. The data representing the characteristics of the boundary layers (ex. horizontal velocity, potential temperature, boundary layer depth(height), vertical buoyancy flux, bulk Richarson number, vertical turbulent kinetic energy etc.) are available in netCDF format.Most of the simulations have been carried out on the supercomputer system supported by the National Center for Meteorological Supercomputer of Korea Meteorological Administration (KMA).<br>