Non-linear forcing singular vector of a two-dimensional quasi-geostrophic model

We propose a non-linear forcing singular vector (NFSV) approach to infer the effect of non-linearity on the predictability associated with model errors. The NFSV is a generalisation of the forcing singular vector (FSV) to non-linear fields and acts as a tendency perturbation that results in a signif...

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Main Authors: Wansuo Duan, Feifan Zhou
Format: Article
Language:English
Published: Taylor & Francis Group 2013-02-01
Series:Tellus: Series A, Dynamic Meteorology and Oceanography
Subjects:
Online Access:http://www.tellusa.net/index.php/tellusa/article/view/18452/pdf_2
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spelling doaj-6e84cf20148849a6975f21d61e651e5f2020-11-24T21:49:56ZengTaylor & Francis GroupTellus: Series A, Dynamic Meteorology and Oceanography0280-64951600-08702013-02-0165012010.3402/tellusa.v65i0.18452Non-linear forcing singular vector of a two-dimensional quasi-geostrophic modelWansuo DuanFeifan ZhouWe propose a non-linear forcing singular vector (NFSV) approach to infer the effect of non-linearity on the predictability associated with model errors. The NFSV is a generalisation of the forcing singular vector (FSV) to non-linear fields and acts as a tendency perturbation that results in a significantly large perturbation growth. In predictability studies, the NFSV, as a tendency error, may provide useful information about model errors that cause severe prediction uncertainties. In this article, a two-dimensional quasi-geostrophic (QG) model is used to study NFSVs and make a comparison between NFSVs and FSVs. We choose two basic flows: the first is a zonal steady flow (Ref-1), and the second is a meridional steady flow (Ref-2). The results demonstrate that the corresponding NFSVs contain a phase where the stream function tends to be contracted around regions of strong velocity shear. Furthermore, the NFSVs for the Ref-1 tend to have a meridional asymmetric spatial structure. Due to the absence of non-linearity, FSVs tend to have a larger spatial extension than NFSVs; in particular, the FSVs for the Ref-1 are almost symmetric in the stream function component. The prediction errors caused by FSVs in the non-linear QG model are generally smaller than those caused by FSVs in the linearised QG model; therefore, the non-linearity in the QG model would significantly saturate the perturbation growth. Nevertheless, the prediction errors caused by NFSVs (especially for the Ref-1) in the non-linear QG model are larger than those caused by FSVs, which further implies that the tendency errors of NFSV structures tend to reduce the damping effect of the non-linearity on the perturbation growth and are more applicable than those of FSV structures to describing the optimal mode of the model errors. The differences between NFSVs and FSVs demonstrate the usefulness of NFSVs in revealing the effects of non-linearity on predictability. The NFSV may be a useful non-linear technique for exploring the predictability problems introduced by model errors.http://www.tellusa.net/index.php/tellusa/article/view/18452/pdf_2weatherclimatepredictabilitymodel erroroptimal perturbation
collection DOAJ
language English
format Article
sources DOAJ
author Wansuo Duan
Feifan Zhou
spellingShingle Wansuo Duan
Feifan Zhou
Non-linear forcing singular vector of a two-dimensional quasi-geostrophic model
Tellus: Series A, Dynamic Meteorology and Oceanography
weather
climate
predictability
model error
optimal perturbation
author_facet Wansuo Duan
Feifan Zhou
author_sort Wansuo Duan
title Non-linear forcing singular vector of a two-dimensional quasi-geostrophic model
title_short Non-linear forcing singular vector of a two-dimensional quasi-geostrophic model
title_full Non-linear forcing singular vector of a two-dimensional quasi-geostrophic model
title_fullStr Non-linear forcing singular vector of a two-dimensional quasi-geostrophic model
title_full_unstemmed Non-linear forcing singular vector of a two-dimensional quasi-geostrophic model
title_sort non-linear forcing singular vector of a two-dimensional quasi-geostrophic model
publisher Taylor & Francis Group
series Tellus: Series A, Dynamic Meteorology and Oceanography
issn 0280-6495
1600-0870
publishDate 2013-02-01
description We propose a non-linear forcing singular vector (NFSV) approach to infer the effect of non-linearity on the predictability associated with model errors. The NFSV is a generalisation of the forcing singular vector (FSV) to non-linear fields and acts as a tendency perturbation that results in a significantly large perturbation growth. In predictability studies, the NFSV, as a tendency error, may provide useful information about model errors that cause severe prediction uncertainties. In this article, a two-dimensional quasi-geostrophic (QG) model is used to study NFSVs and make a comparison between NFSVs and FSVs. We choose two basic flows: the first is a zonal steady flow (Ref-1), and the second is a meridional steady flow (Ref-2). The results demonstrate that the corresponding NFSVs contain a phase where the stream function tends to be contracted around regions of strong velocity shear. Furthermore, the NFSVs for the Ref-1 tend to have a meridional asymmetric spatial structure. Due to the absence of non-linearity, FSVs tend to have a larger spatial extension than NFSVs; in particular, the FSVs for the Ref-1 are almost symmetric in the stream function component. The prediction errors caused by FSVs in the non-linear QG model are generally smaller than those caused by FSVs in the linearised QG model; therefore, the non-linearity in the QG model would significantly saturate the perturbation growth. Nevertheless, the prediction errors caused by NFSVs (especially for the Ref-1) in the non-linear QG model are larger than those caused by FSVs, which further implies that the tendency errors of NFSV structures tend to reduce the damping effect of the non-linearity on the perturbation growth and are more applicable than those of FSV structures to describing the optimal mode of the model errors. The differences between NFSVs and FSVs demonstrate the usefulness of NFSVs in revealing the effects of non-linearity on predictability. The NFSV may be a useful non-linear technique for exploring the predictability problems introduced by model errors.
topic weather
climate
predictability
model error
optimal perturbation
url http://www.tellusa.net/index.php/tellusa/article/view/18452/pdf_2
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