The effect of stochastically perturbed parametrisation tendencies (SPPT) on rapidly ascending air streams

Pickl, Moritz ORCIDiD
Lang, Simon T. K. ORCIDiD
Leutbecher, Martin ORCIDiD
Grams, Christian M. ORCIDiD

DOI: https://doi.org/10.1002/qj.4257
Persistent URL: http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/9967
Pickl, Moritz; Lang, Simon T. K.; Leutbecher, Martin; Grams, Christian M., 2022: The effect of stochastically perturbed parametrisation tendencies (SPPT) on rapidly ascending air streams. In: Quarterly Journal of the Royal Meteorological Society, 148, 744, 1242-1261, DOI: https://doi.org/10.1002/qj.4257. 
 
Lang, Simon T. K.; 2 European Centre for Medium‐Range Weather Forecasts (ECMWF) Reading UK
Leutbecher, Martin; 2 European Centre for Medium‐Range Weather Forecasts (ECMWF) Reading UK
Grams, Christian M.; 1 Institute of Meteorology and Climate Research (IMK–TRO), Department Troposphere Research Karlsruhe Institute of Technology (KIT) Karlsruhe Germany

Abstract

The stochastically perturbed parametrisation tendency (SPPT) scheme is a well‐established technique in ensemble forecasting to address model uncertainty by introducing perturbations into the tendencies provided by the physics parametrisations. The magnitude of the perturbations scales with the local net parametrisation tendency, resulting in large perturbations where diabatic processes are active. Rapidly ascending air streams, such as warm conveyor belts (WCBs) and organized tropical convection, are often driven by cloud diabatic processes and are therefore prone to such perturbations. This study investigates the effects of SPPT and initial condition perturbations on rapidly ascending air streams by computing trajectories in sensitivity experiments with the European Centre for Medium‐Range Weather Forecasts (ECMWF) ensemble prediction system, which are set up to disentangle the effects of initial conditions and physics perturbations. The results demonstrate that SPPT systematically increases the frequency of rapidly ascending air streams. The effect is observed globally, but is enhanced in regions where the latent heating along the trajectories is larger. Despite the frequency changes, there are only minor modifications to the physical properties of the trajectories due to SPPT. In contrast to SPPT, initial condition perturbations do not affect WCBs and tropical convection systematically. An Eulerian perspective on vertical velocities reveals that SPPT increases the frequency of strong upward motions compared with experiments with unperturbed model physics. Consistent with the altered vertical motions, precipitation rates are also affected by the model physics perturbations. The unperturbed control member shows the same characteristics as the experiments without SPPT regarding rapidly ascending air streams. We make use of this to corroborate the findings from the sensitivity experiments by analyzing the differences between perturbed and unperturbed members in operational ensemble forecasts of ECMWF. Finally, we give an explanation of how symmetric, zero‐mean perturbations can lead to a unidirectional response when applied in a nonlinear system.


The stochastically perturbed parametrisation tendencies (SPPT) scheme is used at ECMWF to perturb the model physics and introduces state‐dependent perturbations into the parametrisation tendencies. The frequency of rapidly ascending air streams is systematically enhanced when SPPT is active. This effect is stronger when the latent heating is large (panel a), and is therefore more pronounced in the Tropics than in the Extratropics. In contrast, the impact of SPPT on the physical properties of the air streams, such as the latent heat release, is very small (panel b).