The use of idealised experiments in testing a new convective parametrization: Performance of CoMorph‐A

Abstract

CoMorph is a new mass‐flux convection parametrization under development at the Met Office designed for use within the Unified Model and its successor model, LFRic. Use of a three‐dimensional idealised model enables controlled tests of the performance of the scheme across different regimes. This includes the interaction between the physical parametrizations and the resolved dynamics, allowing study of the emergent organisation of convection on the resolved scale. A selection of well‐known cases is revisited here, with the purpose of documenting the extent to which CoMorph captures a range of important, but challenging, behaviour such as the diurnal cycle and sensitivity to tropospheric moisture. Simulations using CoMorph‐A, a new physics package, that has been demonstrated to perform well at numerical weather prediction (NWP) and climate scales, are compared against the current global atmosphere configuration and high‐resolution results. In addition to an entirely new convection scheme, the package of changes includes significant changes to the cloud, microphysics, and boundary‐layer parametrizations. Recognising that CoMorph‐A is the first version of a scheme that will continue to be substantially developed and to obtain good performance, compromises in tuning have had to be made. These idealised tests therefore show what works well in this configuration, and what areas will require further work. As such, it is quite a demanding testbed and could be viewed as some of the equipment required for a “convective playground”.

The Impact of the Explicit Representation of Convection on the Climate of a Tidally Locked Planet in Global Stretched-mesh Simulations

“…Scale-aware convection schemes are a promising solution (Kendon et al 2021), which may also reignite interest in using stretched-mesh GCMs (Uchida et al 2016). One example of a scale-aware scheme is CoMorph, a new convection parameterization under development at the Met Office (Daleu et al 2023;Lavender et al 2024). It is designed for use within both the UM and LFRic-Atmosphere and has already been shown to be close to cloud-resolving models in representing many aspects of convection (Lavender et al 2024).…”

“…One example of a scale-aware scheme is CoMorph, a new convection parameterization under development at the Met Office (Daleu et al 2023;Lavender et al 2024). It is designed for use within both the UM and LFRic-Atmosphere and has already been shown to be close to cloud-resolving models in representing many aspects of convection (Lavender et al 2024). The benefits of applying CoMorph in a stretched-mesh configuration will be explored for a tidally locked exoplanet in a future study.…”