Notes from the session:
High resolution modelling discussion
Some representation of : Atmosphere modelling community, ocean modelling community and coupled ocean-atm modelling community, including ocean BGC and atmospheric composition.
Why?
- Better understanding of small scale processes in their own right
Dynamical understanding (Better understand their drivers) and impact
Processes important for hazard: dry condition for fire risk, coastal rainfalls, intense localised rainfall and wind, tropical cyclone.
Localised effect -Processes that interact with and/or driven by complex orography, topography, coastlines: waves, tide and inundation ; Ice-shelf ocean interaction ; shelf-break current interaction with canyons , tidal mixing
Small scale Processes and events that are involved in downstream impact : nutrient supply, water quality, larval dispersal â usually the purpose of coastal modelling
Submesoscale processes in the ocean : coastal and open ocean
- understand small scale processes to fix biases in large scale
examples: Southern Ocean radiation biases , small scale convection in tropical band, submesoscale ocean processes
2ways to get benefit:
- ¡ upscale effect : small scale impact large scale - improve biases in HR global run
- ¡ better understanding of HR process to inform better parameterization in LR global run
- What is the community doing?
We contribute/invest in to 1. and 2.upscale, not so much 2.parameterization
But lots of unknown that need to be understood:
- o Is there benefit? And Can we quantify it?
- o Why high res give us improvement?
- o How to assess performance / validate with obs?
- o What is an optimal resolution? need kmâ scale coupled : 1/4 atm 1/10 ocean , in 7-y 5km atm and ocean?
comment about value in translating the learning of HR into parameterization scheme for LR:
ML space could inform the parameterization.
Example: cloud formation module translated into ML-informed module (which learn from HR)
How?
Lots of different pathways to go to high resolution
Lots of questions, without clear answer â the how? is a scientific question in itself:
- o Global high res or downscaling?
- o Atm only, ocean only, coupling at high resolution ?
- o For downscaling which boundary conditions are best?
- o Does global model provide good enough boundary condition to the regional downscaling?
- o Does global high res provide better climatology ?
Comments :
- o Role to play for relocatable tool for downscaling
- o Role of ~100m resolution model:
Benefit in doing some trial run at a few 100m resolution, for small domains (example for Paris Olympics)
Very HR in coastal modelling (down to ~50m), but big limitation is to have the right atm forcing (sea-breeze, diurnal cycle , island effect, cap effectâŚ.)
Across time-scale value:
event type study or/and climate study or/and decadal study?
Depend on the science Q? but high values across time scale:
For example: extremes rainfall (intensity and location)
high value for forecasting â high value for climate but harder for climate to get/understand the return periods/ frequency
Role of ACCESS-NRI and community
- benchmarking in regional modelling?
can we come up with a protocol to assess the value of HR.
what are the right metrics?
Can we assess benefits across spatial scales : local event/process, but also regional benefit.
The community needs a framework to assess the value of increasing resolution. K-scale project from the MetOffice provides a potential example.
- 1 big Challenge with HR is large database and analysing TB
Postprocessing discussion:
Do we want an equivalent of ESMval tool?
It is important to store the data in the right format - right chunking. in particular space vs time.
We need/want to share the postprocessing methodologies.
Compute vs storage discussion :
compute cheap, storage expensive.
Try to find the right balance between Diagnostic online vs offline
What to save? Discussion:
Finding the right balance between: âPlease Donât output 200 variablesâ, and âplease output moreâ.
Governance discussion:
- o Better tracking of what is going in : input, initial conditions, forcingâŚetc
- o Sometimes outputs are âtoo easilyâ available â data not used in the right way. Misused of data.
- Coordination across communities.
More question than answers. But Clear need and will for coordination and knowledge sharing.
Easy hanging fruit?
A larger atm domain at HR could serve the ocean community.
In coastal ocean: do we need long term projection at the boundary or could a short-term or scenario type forcing be useful? time-slice or scenario are good.