Earthquakes and relative sealevel changes

Using a spherical model of postseismic deformation, for the first time we have computed the global contribution of large earthquakes to the relative sealevel variations in the twentieth century. We have found that great earthquakes have the overall tendency to produce a sealevel rise, and that they...

Full description

Saved in:
Bibliographic Details
Published inGeophysical research letters Vol. 31; no. 9; pp. L09601 - n/a
Main Authors Melini, D., Piersanti, A., Spada, G., Soldati, G., Casarotti, E., Boschi, E.
Format Journal Article
LanguageEnglish
Published American Geophysical Union 16.05.2004
Blackwell Publishing Ltd
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary:Using a spherical model of postseismic deformation, for the first time we have computed the global contribution of large earthquakes to the relative sealevel variations in the twentieth century. We have found that great earthquakes have the overall tendency to produce a sealevel rise, and that they affect the measurements taken at those tide‐gauge sites that are commonly employed to obtain global estimates of sealevel rise. Though on a global scale most of the signal is associated with thrust events, on a regional scale the effects of great transcurrent earthquakes cannot be neglected. Depending on the viscosity of the asthenosphere, the contribution of earthquakes to the long‐term sealevel changes amounts to at least 0.1 mm/yr. Thus, the climate‐driven long‐term sealevel changes deduced by tide‐gauge observations may be slightly, but not negligibly, overestimated.
Bibliography:istex:4A535475EEC43FD8B5D26F99A6111C76948BC1B7
ArticleID:2003GL019347
ark:/67375/WNG-JGNZNV7T-K
ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ObjectType-Article-2
ObjectType-Feature-1
ISSN:0094-8276
1944-8007
DOI:10.1029/2003GL019347