Data assimilation for moving mesh methods with an application to ice sheet modelling

We develop data assimilation techniques for non-linear dynamical systems modelled by moving mesh methods. Such techniques are valuable for explicitly tracking interfaces and boundaries in evolving systems. The unique aspect of these assimilation techniques is that both the states of the system a...

Full description

Bibliographic Details
Main Authors: B. Bonan, N. K. Nichols, M. J. Baines, D. Partridge
Format: Article
Language:English
Published: Copernicus Publications 2017-09-01
Series:Nonlinear Processes in Geophysics
Online Access:https://www.nonlin-processes-geophys.net/24/515/2017/npg-24-515-2017.pdf
id doaj-750dee1ed19a4b389388ccc2cda5ab67
record_format Article
spelling doaj-750dee1ed19a4b389388ccc2cda5ab672020-11-25T00:55:24ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79462017-09-012451553410.5194/npg-24-515-2017Data assimilation for moving mesh methods with an application to ice sheet modellingB. Bonan0N. K. Nichols1M. J. Baines2D. Partridge3School of Mathematical, Physical and Computational Sciences, University of Reading, Reading, UKSchool of Mathematical, Physical and Computational Sciences, University of Reading, Reading, UKSchool of Mathematical, Physical and Computational Sciences, University of Reading, Reading, UKSchool of Mathematical, Physical and Computational Sciences, University of Reading, Reading, UKWe develop data assimilation techniques for non-linear dynamical systems modelled by moving mesh methods. Such techniques are valuable for explicitly tracking interfaces and boundaries in evolving systems. The unique aspect of these assimilation techniques is that both the states of the system and the positions of the mesh points are updated simultaneously using physical observations. Covariances between states and mesh points are generated either by a correlation structure function in a variational context or by ensemble methods. The application of the techniques is demonstrated on a one-dimensional model of a grounded shallow ice sheet. It is shown, using observations of surface elevation and/or surface ice velocities, that the techniques predict the evolution of the ice sheet margin and the ice thickness accurately and efficiently. This approach also allows the straightforward assimilation of observations of the position of the ice sheet margin.https://www.nonlin-processes-geophys.net/24/515/2017/npg-24-515-2017.pdf
collection DOAJ
language English
format Article
sources DOAJ
author B. Bonan
N. K. Nichols
M. J. Baines
D. Partridge
spellingShingle B. Bonan
N. K. Nichols
M. J. Baines
D. Partridge
Data assimilation for moving mesh methods with an application to ice sheet modelling
Nonlinear Processes in Geophysics
author_facet B. Bonan
N. K. Nichols
M. J. Baines
D. Partridge
author_sort B. Bonan
title Data assimilation for moving mesh methods with an application to ice sheet modelling
title_short Data assimilation for moving mesh methods with an application to ice sheet modelling
title_full Data assimilation for moving mesh methods with an application to ice sheet modelling
title_fullStr Data assimilation for moving mesh methods with an application to ice sheet modelling
title_full_unstemmed Data assimilation for moving mesh methods with an application to ice sheet modelling
title_sort data assimilation for moving mesh methods with an application to ice sheet modelling
publisher Copernicus Publications
series Nonlinear Processes in Geophysics
issn 1023-5809
1607-7946
publishDate 2017-09-01
description We develop data assimilation techniques for non-linear dynamical systems modelled by moving mesh methods. Such techniques are valuable for explicitly tracking interfaces and boundaries in evolving systems. The unique aspect of these assimilation techniques is that both the states of the system and the positions of the mesh points are updated simultaneously using physical observations. Covariances between states and mesh points are generated either by a correlation structure function in a variational context or by ensemble methods. The application of the techniques is demonstrated on a one-dimensional model of a grounded shallow ice sheet. It is shown, using observations of surface elevation and/or surface ice velocities, that the techniques predict the evolution of the ice sheet margin and the ice thickness accurately and efficiently. This approach also allows the straightforward assimilation of observations of the position of the ice sheet margin.
url https://www.nonlin-processes-geophys.net/24/515/2017/npg-24-515-2017.pdf
work_keys_str_mv AT bbonan dataassimilationformovingmeshmethodswithanapplicationtoicesheetmodelling
AT nknichols dataassimilationformovingmeshmethodswithanapplicationtoicesheetmodelling
AT mjbaines dataassimilationformovingmeshmethodswithanapplicationtoicesheetmodelling
AT dpartridge dataassimilationformovingmeshmethodswithanapplicationtoicesheetmodelling
_version_ 1725230359503699968