A systematic method of parameterisation estimation using data assimilation

In numerical weather prediction, parameterisations are used to simulate missing physics in the model. These can be due to a lack of scientific understanding or a lack of computing power available to address all the known physical processes. Parameterisations are sources of large uncertainty in a mod...

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Main Authors: Matthew Lang, Peter Jan Van Leeuwen, Philip Browne
Format: Article
Language:English
Published: Taylor & Francis Group 2016-02-01
Series:Tellus: Series A, Dynamic Meteorology and Oceanography
Subjects:
Online Access:http://www.tellusa.net/index.php/tellusa/article/view/29012/45115
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spelling doaj-eb8f0c193bfa44fa8020841520b6fbf02020-11-24T22:14:29ZengTaylor & Francis GroupTellus: Series A, Dynamic Meteorology and Oceanography1600-08702016-02-0168011010.3402/tellusa.v68.2901229012A systematic method of parameterisation estimation using data assimilationMatthew Lang0Peter Jan Van Leeuwen1Philip Browne2 Department of Meteorology, University of Reading, Reading, UK Department of Meteorology, University of Reading, Reading, UK Department of Meteorology, University of Reading, Reading, UKIn numerical weather prediction, parameterisations are used to simulate missing physics in the model. These can be due to a lack of scientific understanding or a lack of computing power available to address all the known physical processes. Parameterisations are sources of large uncertainty in a model as parameter values used in these parameterisations cannot be measured directly and hence are often not well known; and the parameterisations themselves are also approximations of the processes present in the true atmosphere. Whilst there are many efficient and effective methods for combined state/parameter estimation in data assimilation (DA), such as state augmentation, these are not effective at estimating the structure of parameterisations. A new method of parameterisation estimation is proposed that uses sequential DA methods to estimate errors in the numerical models at each space-time point for each model equation. These errors are then fitted to pre-determined functional forms of missing physics or parameterisations that are based upon prior information. We applied the method to a one-dimensional advection model with additive model error, and it is shown that the method can accurately estimate parameterisations, with consistent error estimates. Furthermore, it is shown how the method depends on the quality of the DA results. The results indicate that this new method is a powerful tool in systematic model improvement.http://www.tellusa.net/index.php/tellusa/article/view/29012/45115data assimilationparameterisation estimationparameter estimation
collection DOAJ
language English
format Article
sources DOAJ
author Matthew Lang
Peter Jan Van Leeuwen
Philip Browne
spellingShingle Matthew Lang
Peter Jan Van Leeuwen
Philip Browne
A systematic method of parameterisation estimation using data assimilation
Tellus: Series A, Dynamic Meteorology and Oceanography
data assimilation
parameterisation estimation
parameter estimation
author_facet Matthew Lang
Peter Jan Van Leeuwen
Philip Browne
author_sort Matthew Lang
title A systematic method of parameterisation estimation using data assimilation
title_short A systematic method of parameterisation estimation using data assimilation
title_full A systematic method of parameterisation estimation using data assimilation
title_fullStr A systematic method of parameterisation estimation using data assimilation
title_full_unstemmed A systematic method of parameterisation estimation using data assimilation
title_sort systematic method of parameterisation estimation using data assimilation
publisher Taylor & Francis Group
series Tellus: Series A, Dynamic Meteorology and Oceanography
issn 1600-0870
publishDate 2016-02-01
description In numerical weather prediction, parameterisations are used to simulate missing physics in the model. These can be due to a lack of scientific understanding or a lack of computing power available to address all the known physical processes. Parameterisations are sources of large uncertainty in a model as parameter values used in these parameterisations cannot be measured directly and hence are often not well known; and the parameterisations themselves are also approximations of the processes present in the true atmosphere. Whilst there are many efficient and effective methods for combined state/parameter estimation in data assimilation (DA), such as state augmentation, these are not effective at estimating the structure of parameterisations. A new method of parameterisation estimation is proposed that uses sequential DA methods to estimate errors in the numerical models at each space-time point for each model equation. These errors are then fitted to pre-determined functional forms of missing physics or parameterisations that are based upon prior information. We applied the method to a one-dimensional advection model with additive model error, and it is shown that the method can accurately estimate parameterisations, with consistent error estimates. Furthermore, it is shown how the method depends on the quality of the DA results. The results indicate that this new method is a powerful tool in systematic model improvement.
topic data assimilation
parameterisation estimation
parameter estimation
url http://www.tellusa.net/index.php/tellusa/article/view/29012/45115
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