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...
Main Authors: | , , , |
---|---|
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 |
id |
doaj-9734e5ea339c42b0a913d166095a59cd |
---|---|
record_format |
Article |
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 |
work_keys_str_mv |
AT kamerondeckerharris predictingflowreversalsinchaoticnaturalconvectionusingdataassimilation AT elhassanridouane predictingflowreversalsinchaoticnaturalconvectionusingdataassimilation AT darrenlhitt predictingflowreversalsinchaoticnaturalconvectionusingdataassimilation AT christophermdanforth predictingflowreversalsinchaoticnaturalconvectionusingdataassimilation |
_version_ |
1725187466886905856 |