Predicting flow reversals in chaotic natural convection using data assimilation

A simplified model of natural convection, similar to the Lorenz system, is compared to computational fluid dynamics simulations of a thermosyphon in order to test data assimilation (DA) methods and better understand the dynamics of convection. The thermosyphon is represented by a long time flow simu...

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Main Authors: Kameron Decker Harris, El Hassan Ridouane, Darren L. Hitt, Christopher M. Danforth
Format: Article
Language:English
Published: Taylor & Francis Group 2012-04-01
Series:Tellus: Series A, Dynamic Meteorology and Oceanography
Subjects:
Online Access:http://www.tellusa.net/index.php/tellusa/article/view/17598/pdf_2
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spelling doaj-9734e5ea339c42b0a913d166095a59cd2020-11-25T01:07:24ZengTaylor & Francis GroupTellus: Series A, Dynamic Meteorology and Oceanography0280-64951600-08702012-04-0164011410.3402/tellusa.v64i0.17598Predicting flow reversals in chaotic natural convection using data assimilationKameron Decker HarrisEl Hassan RidouaneDarren L. HittChristopher M. DanforthA simplified model of natural convection, similar to the Lorenz system, is compared to computational fluid dynamics simulations of a thermosyphon in order to test data assimilation (DA) methods and better understand the dynamics of convection. The thermosyphon is represented by a long time flow simulation, which serves as a reference ‘truth’. Forecasts are then made using the Lorenz-like model and synchronised to noisy and limited observations of the truth using DA. The resulting analysis is observed to infer dynamics absent from the model when using short assimilation windows. Furthermore, chaotic flow reversal occurrence and residency times in each rotational state are forecast using analysis data. Flow reversals have been successfully forecast in the related Lorenz system, as part of a perfect model experiment, but never in the presence of significant model error or unobserved variables. Finally, we provide new details concerning the fluid dynamical processes present in the thermosyphon during these flow reversals.http://www.tellusa.net/index.php/tellusa/article/view/17598/pdf_2chaosdata assimilationforecastingLorenz systemthermosyphon
collection DOAJ
language English
format Article
sources DOAJ
author Kameron Decker Harris
El Hassan Ridouane
Darren L. Hitt
Christopher M. Danforth
spellingShingle Kameron Decker Harris
El Hassan Ridouane
Darren L. Hitt
Christopher M. Danforth
Predicting flow reversals in chaotic natural convection using data assimilation
Tellus: Series A, Dynamic Meteorology and Oceanography
chaos
data assimilation
forecasting
Lorenz system
thermosyphon
author_facet Kameron Decker Harris
El Hassan Ridouane
Darren L. Hitt
Christopher M. Danforth
author_sort Kameron Decker Harris
title Predicting flow reversals in chaotic natural convection using data assimilation
title_short Predicting flow reversals in chaotic natural convection using data assimilation
title_full Predicting flow reversals in chaotic natural convection using data assimilation
title_fullStr Predicting flow reversals in chaotic natural convection using data assimilation
title_full_unstemmed Predicting flow reversals in chaotic natural convection using data assimilation
title_sort predicting flow reversals in chaotic natural convection using data assimilation
publisher Taylor & Francis Group
series Tellus: Series A, Dynamic Meteorology and Oceanography
issn 0280-6495
1600-0870
publishDate 2012-04-01
description A simplified model of natural convection, similar to the Lorenz system, is compared to computational fluid dynamics simulations of a thermosyphon in order to test data assimilation (DA) methods and better understand the dynamics of convection. The thermosyphon is represented by a long time flow simulation, which serves as a reference ‘truth’. Forecasts are then made using the Lorenz-like model and synchronised to noisy and limited observations of the truth using DA. The resulting analysis is observed to infer dynamics absent from the model when using short assimilation windows. Furthermore, chaotic flow reversal occurrence and residency times in each rotational state are forecast using analysis data. Flow reversals have been successfully forecast in the related Lorenz system, as part of a perfect model experiment, but never in the presence of significant model error or unobserved variables. Finally, we provide new details concerning the fluid dynamical processes present in the thermosyphon during these flow reversals.
topic chaos
data assimilation
forecasting
Lorenz system
thermosyphon
url http://www.tellusa.net/index.php/tellusa/article/view/17598/pdf_2
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