Project Details
Projekt Print View

Towards stochastic modeling of turbulence in the stable atmospheric boundary layer

Applicant Professor Dr.-Ing. Rupert Klein, since 4/2021
Subject Area Atmospheric Science
Term from 2015 to 2022
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 310574835
 
Final Report Year 2022

Final Report Abstract

Limited computer resources lead to a simplified representation of unresolved small-scale processes in weather and climate models, through parameterisation schemes. Among the parameterised processes, turbulent fluxes exert a critical impact on the exchange of heat, water and carbon between the land and the atmosphere. Turbulence theory was, however, developed for homogeneous and flat terrain, with stationary conditions. The theory fails in unsteady flow contexts or with heterogeneous landscapes, but no alternative, viable theory is available. This is not only a source of error in forecasts or climate scenarios, but also a source of model uncertainty which should be characterised and considered when using weather and climate models. The model uncertainty is greatest in cold environments or at nighttime, where the atmospheric boundary layer is stably stratified. Turbulence then coexists with non-turbulent motions from the grey zone between the largest turbulent eddies and smallest mesoscale motions, traditionally specified to be 2km horizontal scale. These non-turbulent motions can include density currents, wave-like motions or two-dimensional modes and represent a non-stationary forcing of turbulence. In this project, measurements of turbulent quantities were analysed in great detail to classify flow regimes occurring in cold or nocturnal environments, to quantify the variability of turbulent fluxes and to understand the physical origin of the variability. A data-driven approach was developed and used to derive a stochastic parameterisation of turbulent fluxes, thereby representing the model uncertainty arising from the incomplete representation of our unsteady atmosphere. The most surprising and promising result is that the uncertainty was found to scale with physical quantities which are available in weather and climate models. The stochastic parameterisation thereby extends conventional models and enables the representation of the resulting unsteady, intermittent fluxes. It could help overcome some of the limitations of weather and climate models to represent mixing in the stable boundary layer.

Publications

 
 

Additional Information

Textvergrößerung und Kontrastanpassung