Abstract

Data assimilation (DA) methods for convective‐scale numerical weather prediction at operational centres are surveyed. The operational methods include variational methods (3D‐Var and 4D‐Var), ensemble methods (LETKF) and hybrids between variational and ensemble methods (3DEnVar and 4DEnVar). At several operational centres, other assimilation algorithms, like latent heat nudging, are additionally applied to improve the model initial state, with emphasis on convective scales. It is demonstrated that the quality of forecasts based on initial data from convective‐scale DA is significantly better than the quality of forecasts from simple downscaling of larger‐scale initial data. However, the duration of positive impact depends on the weather situation, the size of the computational domain and the data that are assimilated. Furthermore it is shown that more advanced methods applied at convective scales provide improvements over simpler methods. This motivates continued research and development in convective‐scale DA.Challenges in research and development for improvements of convective‐scale DA are also reviewed and discussed. The difficulty of handling the wide range of spatial and temporal scales makes development of multi‐scale assimilation methods and space–time covariance localization techniques important. Improved utilization of observations is also important. In order to extract more information from existing observing systems of convective‐scale phenomena (e.g. weather radar data and satellite image data), it is necessary to provide improved statistical descriptions of the observation errors associated with these observations.

Highlights

  • Development of data assimilation (DA) methods for global numerical weather prediction (NWP) models started with simple horizontal interpolation methods (Eliassen, 1954) which gradually developed to become three-dimensional and to include multivariate relationships (Lorenc, 1981)

  • DF blending is implemented in spectral space and consists of several steps: (i) first global and Limited-Area Model (LAM) spectra are truncated to a cut-off wavelength given by an empirical formula (Derkovaand Bellus, 2007); (ii) this is followed by filtering with a non-recursive Dolph–Chebyshev digital filter (Lynch et al, 1997); (iii) at the end the ALADIN background is incremented with the difference between the filtered models’ spectra interpolated back to high resolution

  • DA methods for convective-scale NWP at operational centres are surveyed in this article

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Summary

Introduction

Development of data assimilation (DA) methods for global numerical weather prediction (NWP) models started with simple horizontal interpolation methods (Eliassen, 1954) which gradually developed to become three-dimensional and to include multivariate relationships (Lorenc, 1981). It is an open question, to what extent these techniques will be completely satisfactory for convective-scale DA, or whether fully nonlinear DA techniques like particle filters (van Leeuwen, 2009) will be required, or if modifications to hybrid and ensemble methods to deal with non-Gaussianity, as suggested in Janjicet al. Only the acronym will be used in the text

Description of operational methods
Formulation of the different DA methods
Incremental 3D-Var and incremental 4D-Var
Multi-incremental 4D-Var
The hybrid 3DEnVar and the hybrid 4DEnVar
Method
Surface and soil assimilation
Meteo-France and the HIRLAM and ALADIN consortia
Basic 3D-Var
Radar DA algorithms
HARMONIE-AROME DA
Met Office 3D-Var
Cloud analysis and radar-derived latent heating
Radar data QC
Japan Meteorological Agency – Operational limited-area DA systems
Impact of DA and observations at convective scales
Downscaling versus convective-scale DA – KENDA and AROME-France
Internationally collected radar data
Mode-S EHS and the IMPACT experiment
Strong convective precipitation
Challenges
Frontal rainband over the Netherlands
Treatment of correlated observation errors
International collection of radar data
Use of dual polarimetric radars
JMA advances in assimilation of radar and satellite observations
HARMONIE-AROME 4D-Var developments
Met Office 4D-Var
HARMONIE hybrid 3DEnVar and 4DEnVar
EnVars at Meteo-France
Rapid update NWP for severe weather warnings at NOAA
Findings
Discussion and concluding remarks
Full Text
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