Calculating steady-state linear response matrix of a two-layer quasi-geostrophic model using the multisine excitation
ID:485 View Protection:ATTENDEE Updated Time:2025-01-04 14:45:17 Hits:776 Poster Presentation

Start Time:2025-01-16 19:35(Asia/Shanghai)

Duration:15min

Session:S35 Session 35-Eddy Variability in the Ocean and Atmosphere: Dynamics, Parameterization and Prediction » S35-PEddy Variability in the Ocean and Atmosphere: Dynamics, Parameterization and Prediction

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Abstract
We calculate the steady-state linear response matrix of a two-layer quasi-geostrophic model (two-layer QG model). We impose the multisine excitation, which can effectively detect the magnitude of nonlinear distortions and attain a high signal-to-noise ratio (SNR). This method has recently been introduced to atmospheric science, but has not been applied to the linearization of the two-layer QG model yet. By considering periodic excitations, this method produces a linearization applicable to a wider range of problems. We will examine the frequency dependence of the linear response matrix to evaluate the memory of the two-layer QG model. We will combine the linear response at different frequencies to give a steady-state linear response matrix. The steady-state linear response matrix can be applied to construct time-invariant forcings to force a specified mean state of the model without directly acting on the eddies, and therefore, help to measure the response of eddies to mean state changes and help to gain a better understanding of wave–mean flow interactions.
Keywords
multisine excitation, two-layer quasi-geostrophic model, system identification
Speaker
Xingfeng Li
Undergraduate Fudan University

Submission Author
Xingfeng Li Fudan University
Pak Wah Chan Fudan University
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Important Date
  • Conference Date

    Jan 13

    2025

    to

    Jan 17

    2025

  • Sep 27 2024

    Draft paper submission deadline

  • Feb 17 2025

    Registration deadline

Sponsored By
State Key Laboratory of Marine Environmental Science, Xiamen University
Organized By
State Key Laboratory of Marine Environmental Science, Xiamen University
Department of Earth Sciences, National Natural Science Foundation of China
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