Abstract

Abstract. The current resolution of the operational global models favours the possibility of driving convection-permitting limited-area model (LAM) simulations directly, sparing the necessity for an intermediate step with a coarser-resolution LAM. Though the resolution of global ensemble systems is generally lower than that of deterministic ones, it is also possible to consider this opportunity in the field of ensemble forecasting. The aim of this paper is to investigate the effect of this choice for driving a convection-permitting ensemble based on the COSMO model, for a specific application, namely the forecast of intense autumn precipitation events over Italy. The impact of the direct nesting in the ECMWF global ensemble is compared to a two-step nesting, which makes use of a LAM ensemble system with parametrised convection. Results show that the variability introduced in the geopotential field by the direct nesting is usually contained within the uncertainty described by the standard ensemble, and differences between pairs of members following different nesting approaches are generally smaller than the ensemble error, computed with respect to analysis. The relation between spread and error is even improved by the direct nesting approach. In terms of precipitation, it is found that the forecasts issued by members with different nesting approaches generally have differences at spatial scales between 16 and 180 km, depending on the case, hence not negligible. Nevertheless, the skill of the LAM ensemble precipitation forecasts, evaluated by means of an objective verification, is comparable. Therefore, the overall quality of the 2.8 km ensemble for the specific application is not deteriorated by the provision of lower resolution lateral boundary conditions directly from the global ensemble.

Highlights

  • The current resolution of operational global circulation models (GCM) paves the way towards driving convectionpermitting limited-area model (LAM) integrations directly, with lateral boundary conditions (LBCs) provided by a global model

  • The aim of this paper is to investigate the effect of the provision of LBCs to a LAM ensemble run at a convection-permitting resolution by a global ensemble, compared with providing LBCs from an intermediate LAM ensemble run at coarser resolution

  • 4 Summary and conclusions An analysis has been undertaken of the performance of two different nesting approaches for convection-permitting ensemble forecasting

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Summary

Introduction

The current resolution of operational global circulation models (GCM) paves the way towards driving convectionpermitting limited-area model (LAM) integrations directly, with lateral boundary conditions (LBCs) provided by a global model. The coarser spatial and temporal resolution of the LBCs provided by a global model could introduce errors in the forecast, especially if the LAM domain is small, as is often the case for convection-permitting models. ENS is currently running with an approximate horizontal resolution of 32 km, which is planned to increase to about 20 km in 2015 This may enable direct use of LBCs from ENS members to drive ensemble systems for the convection-permitting scale (2–3 km). In this work, it is studied how the performance of the COSMO-H2-EPS ensemble varies if the 2.8 km runs receive ICs and BCs from the ENS members directly, skipping the intermediate step with COSMO-LEPS at 7 km.

Configuration of the ensemble systems
Analysis of 500 hPa geopotential
Analysis of the precipitation fields
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