Probabilistic Stability of an Atmospheric Model to Various Amplitude Perturbations

Abstract

Every forecast should include an estimate of its likely accuracy, as a measure of predictability. A new measure, the first passage time (FPT), which is defined as the time period when the model error first exceeds a predetermined criterion (i.e. the tolerance level), is proposed here to estimate model predictability. A theoretical framework is developed to determine the mean and variance of FPT. The low-order Lorenz atmospheric model is taken as an example to show the robustness of using FPT as a quantitative measure for prediction skill. Both linear and nonlinear perspectives of forecast errors are analytically investigated using the self-consistent Nicolis model. The mean and variance of FPT largely depends on the ratio between twice the maximum Lyapunov exponent (sigma) and the intensity of attractor fluctuations (q sq), lambda = 2(sigma)/q sq. Two types of predictability are found: lambda > 1 referring to low predictability and lambda < 1 referring to high predictability. The mean and variance of FPT can be represented by the e-folding timescales in the low-predictability range, but not in the high-predictability range. The transition between the two predictability ranges is caused by the variability of the attractor characteristics along the reference trajectory.

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Document Details

Document Type
Technical Report
Publication Date
Oct 01, 2002
Accession Number
ADA480140

Entities

People

  • Leonid M. Ivanov
  • Oleg V. Melnichenko
  • Peter Cheng Chu
  • Tatyana M. Margolina

Organizations

  • Naval Postgraduate School

Tags

DTIC Thesaurus Topics

  • Abstracts
  • Accuracy
  • Amplitude
  • Atmospheric Sciences
  • Availability
  • Classification
  • Contracts
  • Errors
  • Information Operations
  • Instructions
  • Intensity
  • Monitoring
  • Perturbations
  • Security
  • Standards

Readers

  • Adaptive Control and Estimation with Uncertainty in Dynamic Systems.
  • Ocean-Atmosphere Mesoscale Modeling, Data Assimilation, and Flux Boundary Layers
  • Theoretical Analysis.