4.5 Article

Stress transfer in earthquakes, hazard estimation and ensemble forecasting: Inferences from numerical simulations

期刊

TECTONOPHYSICS
卷 413, 期 1-2, 页码 109-125

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ELSEVIER
DOI: 10.1016/j.tecto.2005.10.031

关键词

earthquakes; numerical simulations; virtual California

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Observations indicate that earthquake faults occur in topologically complex, multi-scale networks driven by plate tectonic forces. We present realistic numerical simulations, involving data-mining, pattern recognition, theoretical analyses and ensemble forecasting techniques, to understand how the observable space-time earthquake patterns are related to the fundamentally inaccessible and unobservable dynamics. Numerical simulations can also help us to understand how the different scales involved in earthquake physics interact and influence the resulting dynamics. Our simulations indicate that elastic interactions (stress transfer) combined with the nonlinearity in the frictional failure threshold law lead to the self-organization of the statistical dynamics, producing 1) statistical distributions for magnitudes and frequencies of earthquakes that have characteristics similar to those possessed by the Gutenberg-Richter magnitude-frequency distributions observed in nature; and 2) clear examples of stress transfer among fault activity described by stress shadows, in which an earthquake oil one group of faults reduces the Coulomb failure stress oil other faults, thereby delaying activity oil those faults. In this paper, we describe the Current state of modeling and simulation efforts for Virtual California, a model (or all the major active strike slip faults in California. Noting that the Working Group oil California Earthquake Probabilities (WGCEP) uses statistical distributions to produce earthquake forecast probabilities, we demonstrate that Virtual California provides a powerful tool for testing the applicability and reliability of the WGCEP statistical methods. Furthermore, we show how the simulations call be used to develop statistical earthquake forecasting techniques that are complementary to the methods used by the WGCEP, but improve upon those methods in a number of important ways. In doing so, we distinguish between the official, forecasts of the WGCEP, and the research-quality forecasts that we discuss here. Finally, we provide a brief discussion of future problems and issues related to the development of ensemble earthquake hazard estimation and forecasting techniques. (c) 2005 Elsevier B.V. All rights reserved.

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