Détail de la notice
Titre du Document
Earthquake prediction and forecasting
Auteur(s)
JACKSON David D. ; SPARKS Robert Stephen John (Editeur scientifique) ; HAWKESWORTH Christopher John (Editeur scientifique)
Corporation(s) du ou des auteurs
International Union of Geodesy and Geodesics (IUGG) Boulder, CO USA (Commanditaire)
Résumé
Prospects for earthquake prediction and forecasting, and even their definitions, are actively debated. Here, forecasting means estimating the future earthquake rate as a function of location, time, and magnitude. Forecasting becomes prediction when we identify special conditions that make the immediate probability much higher than usual and high enough to justify exceptional action. Proposed precursors run from aeronomy to zoology, but no identified phenomenon consistently precedes earthquakes. The reported prediction of the 1975 Haicheng, China earthquake is often proclaimed as the most successful, but the success is questionable. An earthquake predicted to occur near Parkfield, California in 1988±5 years has not happened. Why is prediction so hard? Earthquakes start in a tiny volume deep within an opaque medium; we do not know their boundary conditions, initial conditions, or material properties well; and earthquake precursors, if any, hide amongst unrelated anomalies. Earthquakes cluster in space and time, and following a quake earthquake probability spikes. Aftershocks illustrate this clustering, and later earthquakes may even surpass earlier ones in size. However, the main shock in a cluster usually comes first and causes the most damage. Specific models help reveal the physics and allow intelligent disaster response. Modeling stresses from past earthquakes may improve forecasts, but this approach has not yet been validated prospectively. Reliable prediction of individu
Editeur
American Geophysical Union
Type du document
Conférence : IUGG 2003 General Assembly of the International Union of Geodesy and Geophysics, 23, Sapporo, JPN, 2003-06-30
Identifiant
ISSN : 0065-8448 CODEN : GPMGAD
Source
Geophysical monograph A. 2004, vol. 150, pp. 335-348 [14 pages] [bibl. : 28 ref.]
Langue
Anglais
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