16 March 2023

Webinaire Kwok P. Chun

Dr Kwok P Chun (Sun) is a lecturer whose interests lie in nonstationary environmental processes related to the atmosphere, hydrosphere, and biosphere. His work involves developing tools and numerical models to analyse dynamic systems, with a particular focus on qualifying and quantifying risks, extremes, and irreversible shifts in the UK and other parts of the world. With a background in Climatology and Hydrology, Sun is currently exploring the use of convection-permitting models to investigate climate patterns in South America in collaboration with researchers from the US National Center for Atmospheric Research. Additionally, he is working with Prof Luminita Danaila and Dr Manuel Fossa from the University of Rouen to develop mesoscale models that examine the potential use of blue and green infrastructure to promote thermal comfort and mitigate hydrological hazards. Sun is dedicated to understanding the constituting components and processes of our physical environment and how changing earth systems impact various aspects of daily life, in order to prepare for forthcoming challenges and create a better world. He welcomes conversations on the topics of water and environment.
Drift and Diffusion Functions of Historical Time Series and UKCP18 Convection-Permitting Model Outputs for Bristol and Filton

Kwok P Chun, Luminita Danaila and Manuel Fossa

As global temperatures continue to rise and affect atmospheric dynamics, there is a growing need to develop methods for investigating the temporal evolution of climate fields. These methods are useful to quantify both short- and long-term changes, as a function of geographical locations, seasons, and large-scale atmospheric conditions.
Using the Fokker-Planck equation, we investigate the deterministic drift and diffusion processes of measured and modelled time series. Specifically, we derive the drift and diffusion functions of
1) Bristol and Filton’s historical hourly temperature data.
2) the corresponding UK convective permitting model outputs for the RCP 8.5 climate projection scenarios.
The drift function varies linearly for the two data types, although the exact function forms differ for different periods. Moreover, the diffusion function depends more on the investigated geographical locations and the period. These results suggest the potential role of turbulent statistics at all scales.
Furthermore, we will propose using the stochastic differential equation approach to capture the complexity of temperature dynamics and study the effect of other factors, such as atmospheric circulation patterns. We aim to (i) provide insight into the relationship between drift, diffusion, and turbulence in temperature dynamics and (ii) lay the groundwork for further analysis of convection-permitting model simulations.

16 March 2023, 16h3017h30
Wébinaire: veuillez contacter F. Romano ou J.-P pour obtenir le lien.