Predictability of isotropic turbulence by massive ensemble forecasting

Turbulent flows are difficult to predict due to chaos, which amplifies any uncertainty in the initial conditions. The way this uncertainty grows and propagates is key to understanding the emergence of complexity in turbulence and to assessing the reliability of turbulence forecasts. In this Letter, a novel approach based on massive ensembles of simulations reveals that uncertainty propagates in isotropic turbulence following a simple law that depends only on the average properties of the flow. This result opens avenues to improve current forecasting techniques by efficiently and accurately modeling uncertainty propagation.

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Publication Details

Journal
Physical Review Fluids
Published
2024-12-04
DOI
https://doi.org/10.1103/physrevfluids.9.l122601
Citations
1
Primary Topic
Meteorological Phenomena and Simulations
Type
article
Field-Weighted Citation Impact
0.38
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article

Predictability of isotropic turbulence by massive ensemble forecasting

Alberto Vela-Martín
1 citations
Physical Review Fluids
Meteorological Phenomena and Simulations
0.38
article

Predictability of isotropic turbulence by massive ensemble forecasting

Alberto Vela-Martín
article en
1 citations

Abstract

Turbulent flows are difficult to predict due to chaos, which amplifies any uncertainty in the initial conditions. The way this uncertainty grows and propagates is key to understanding the emergence of complexity in turbulence and to assessing the reliability of turbulence forecasts. In this Letter, a novel approach based on massive ensembles of simulations reveals that uncertainty propagates in isotropic turbulence following a simple law that depends only on the average properties of the flow. This result opens avenues to improve current forecasting techniques by efficiently and accurately modeling uncertainty propagation.

Physical Review FluidsVol. 9(12)
Universidad Carlos III de Madrid (ES)
Climate action
Openalex Percentile: Top 38%
Meteorological Phenomena and Simulations
0.38
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