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...

Full description

Bibliographic Details
Main Authors: Jean-François Mahfouf, Alexandre Boilley
Format: Article
Language:English
Published: Taylor & Francis Group 2012-06-01
Series:Tellus: Series A, Dynamic Meteorology and Oceanography
Subjects:
Online Access:http://www.tellusa.net/index.php/tellusa/article/view/18697/pdf_1
id doaj-1629db47b9824c69930d662c47fcc0a2
record_format Article
spelling 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
_version_ 1724774734345797632