The experiment in the tropical Atlantic was performed during the period August-November 2010 where a systematic warm temperature bias with a magnitude ~0.5 K occurred in a deep tropospheric layer centered ~700 hPa. This method revealed that this bias originated primarily from the Kain-Fritsch convective heating parameterization scheme, and furthermore that this bias developed within the first 30-minutes of each forecast. The experiment over the Antarctic was performed during the period September-October 2010 to coin-cide with the Concordiasi intensive observation period, when special droponsonde observations were available as an independent source of model validation. Here, where convection is relatively small, lower-tropospheric biases arose primarily from parameterized boundary layer processes, with results sensitive to the underlying surface type and orography of the Antarctic continent. These experiments furthermore quantify the evolution of model spin-up, where it is concluded that spin-up has distinct phases that can only be minimized when initializing model forecasts from an ensemble member that is generated using a data assimilation system using an identical model configuration.