Assimilation of low-level wind in a high-resolution mesoscale model using the back and forth nudging algorithm
The performance of a new data assimilation algorithm called back and forth nudging (BFN) is evaluated using a high-resolution numerical mesoscale model and simulated wind observations in the boundary layer. This new algorithm, of interest for the assimilation of high-frequency observations provided...
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Taylor & Francis Group
2012-06-01
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Online Access: | http://www.tellusa.net/index.php/tellusa/article/view/18697/pdf_1 |
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doaj-1629db47b9824c69930d662c47fcc0a22020-11-25T02:42:11ZengTaylor & Francis GroupTellus: Series A, Dynamic Meteorology and Oceanography0280-64951600-08702012-06-0164011510.3402/tellusa.v64i0.18697Assimilation of low-level wind in a high-resolution mesoscale model using the back and forth nudging algorithmJean-François MahfoufAlexandre BoilleyThe performance of a new data assimilation algorithm called back and forth nudging (BFN) is evaluated using a high-resolution numerical mesoscale model and simulated wind observations in the boundary layer. This new algorithm, of interest for the assimilation of high-frequency observations provided by ground-based active remote-sensing instruments, is straightforward to implement in a realistic atmospheric model. The convergence towards a steady-state profile can be achieved after five iterations of the BFN algorithm, and the algorithm provides an improved solution with respect to direct nudging. It is shown that the contribution of the nudging term does not dominate over other model physical and dynamical tendencies. Moreover, by running backward integrations with an adiabatic version of the model, the nudging coefficients do not need to be increased in order to stabilise the numerical equations. The ability of BFN to produce model changes upstream from the observations, in a similar way to 4-D-Var assimilation systems, is demonstrated. The capacity of the model to adjust to rapid changes in wind direction with the BFN is a first encouraging step, for example, to improve the detection and prediction of low-level wind shear phenomena through high-resolution mesoscale modelling over airports.http://www.tellusa.net/index.php/tellusa/article/view/18697/pdf_1Data assimilationNudgingLow-level wind |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Jean-François Mahfouf Alexandre Boilley |
spellingShingle |
Jean-François Mahfouf Alexandre Boilley Assimilation of low-level wind in a high-resolution mesoscale model using the back and forth nudging algorithm Tellus: Series A, Dynamic Meteorology and Oceanography Data assimilation Nudging Low-level wind |
author_facet |
Jean-François Mahfouf Alexandre Boilley |
author_sort |
Jean-François Mahfouf |
title |
Assimilation of low-level wind in a high-resolution mesoscale model using the back and forth nudging algorithm |
title_short |
Assimilation of low-level wind in a high-resolution mesoscale model using the back and forth nudging algorithm |
title_full |
Assimilation of low-level wind in a high-resolution mesoscale model using the back and forth nudging algorithm |
title_fullStr |
Assimilation of low-level wind in a high-resolution mesoscale model using the back and forth nudging algorithm |
title_full_unstemmed |
Assimilation of low-level wind in a high-resolution mesoscale model using the back and forth nudging algorithm |
title_sort |
assimilation of low-level wind in a high-resolution mesoscale model using the back and forth nudging algorithm |
publisher |
Taylor & Francis Group |
series |
Tellus: Series A, Dynamic Meteorology and Oceanography |
issn |
0280-6495 1600-0870 |
publishDate |
2012-06-01 |
description |
The performance of a new data assimilation algorithm called back and forth nudging (BFN) is evaluated using a high-resolution numerical mesoscale model and simulated wind observations in the boundary layer. This new algorithm, of interest for the assimilation of high-frequency observations provided by ground-based active remote-sensing instruments, is straightforward to implement in a realistic atmospheric model. The convergence towards a steady-state profile can be achieved after five iterations of the BFN algorithm, and the algorithm provides an improved solution with respect to direct nudging. It is shown that the contribution of the nudging term does not dominate over other model physical and dynamical tendencies. Moreover, by running backward integrations with an adiabatic version of the model, the nudging coefficients do not need to be increased in order to stabilise the numerical equations. The ability of BFN to produce model changes upstream from the observations, in a similar way to 4-D-Var assimilation systems, is demonstrated. The capacity of the model to adjust to rapid changes in wind direction with the BFN is a first encouraging step, for example, to improve the detection and prediction of low-level wind shear phenomena through high-resolution mesoscale modelling over airports. |
topic |
Data assimilation Nudging Low-level wind |
url |
http://www.tellusa.net/index.php/tellusa/article/view/18697/pdf_1 |
work_keys_str_mv |
AT jeanfranx00e7oismahfouf assimilationoflowlevelwindinahighresolutionmesoscalemodelusingthebackandforthnudgingalgorithm AT alexandreboilley assimilationoflowlevelwindinahighresolutionmesoscalemodelusingthebackandforthnudgingalgorithm |
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