Abstract. A new regional coupled modelling framework is introduced – the Regional
Coupled Suite (RCS). This provides a flexible research capability with which
to study the interactions between atmosphere, land, ocean, and wave processes
resolved at kilometre scale, and the effect of environmental feedbacks on the
evolution and impacts of multi-hazard weather events. A configuration of the
RCS focussed on the Indian region, termed RCS-IND1, is introduced. RCS-IND1
includes a regional configuration of the Unified Model (UM) atmosphere,
directly coupled to the JULES land surface model, on a grid with horizontal
spacing of 4.4 km, enabling convection to be explicitly simulated. These are
coupled through OASIS3-MCT libraries to 2.2 km grid NEMO ocean and WAVEWATCH
III wave model configurations. To examine a potential approach to reduce
computation cost and simplify ocean initialization, the RCS includes an
alternative approach to couple the atmosphere to a lower resolution
Multi-Column K-Profile Parameterization (KPP) for the ocean. Through
development of a flexible modelling framework, a variety of fully and
partially coupled experiments can be defined, along with traceable uncoupled
simulations and options to use external input forcing in place of missing
coupled components. This offers a wide scope to researchers designing
sensitivity and case study assessments. Case study results are presented and
assessed to demonstrate the application of RCS-IND1 to simulate two tropical
cyclone cases which developed in the Bay of Bengal, namely Titli in October
2018 and Fani in April 2019. Results show realistic cyclone simulations, and
that coupling can improve the cyclone track and produces more realistic
intensification than uncoupled simulations for Titli but prevents sufficient
intensification for Fani. Atmosphere-only UM regional simulations omit the
influence of frictional heating on the boundary layer to prevent cyclone
over-intensification. However, it is shown that this term can improve
coupled simulations, enabling a more rigorous treatment of the near-surface
energy budget to be represented. For these cases, a 1D mixed layer scheme
shows similar first-order SST cooling and feedback on the cyclones to a 3D
ocean. Nevertheless, the 3D ocean generally shows stronger localized cooling
than the 1D ocean. Coupling with the waves has limited feedback on the
atmosphere for these cases. Priorities for future model development are
discussed.