A multilayer upper-boundary condition for longwave radiative flux to correct temperature biases in a mesoscale model

The bias originates from the Rapid Radiative Transfer Model longwave radiation physics scheme and can be reduced substantially by 1) modifying the treatment within the scheme by adding a multilayer buffer between the model top and top of the atmosphere and 2) constraining stratospheric water vapor to remain within the estimated climatology in the stratosphere.

These changes reduce the longwave heating rate bias at the model top to ±0.5 K day⁻¹. Corresponding bias reductions are also seen, particularly near the tropopause.