TL;DR
This paper develops and verifies data assimilation methods, especially ensemble Kalman filters, to predict flow reversals in a thermosyphon simulation, demonstrating improved accuracy with adaptive covariance and low-dimensional mode analysis.
Contribution
It introduces adaptive localized covariance in ensemble Kalman filtering and applies Dynamic Mode Decomposition to identify predictive modes of flow reversals.
Findings
Adaptive covariance improves prediction with fewer observations.
DMD identifies modes predictive of flow reversal direction.
ETKF outperforms static covariance in flow reversal prediction.
Abstract
A thermal convection loop is a annular chamber filled with water, heated on the bottom half and cooled on the top half. With sufficiently large forcing of heat, the direction of fluid flow in the loop oscillates chaotically, dynamics analogous to the Earth's weather. As is the case for state-of-the-art weather models, we only observe the statistics over a small region of state space, making prediction difficult. To overcome this challenge, data assimilation (DA) methods, and specifically ensemble methods, use the computational model itself to estimate the uncertainty of the model to optimally combine these observations into an initial condition for predicting the future state. Here, we build and verify four distinct DA methods, and then, we perform a twin model experiment with the computational fluid dynamics simulation of the loop using the Ensemble Transform Kalman Filter (ETKF) to…
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