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Fu, Yuning, Song, Y. Tony, and Gross, Richard S., 2017. Linking Oceanic Tsunamis and Geodetic Gravity Changes of Large Earthquakes. Pure and Applied Geophysics, 174(8):3029–3041, doi:10.1007/s00024-017-1510-5.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2017PApGe.174.3029F,
author = {{Fu}, Yuning and {Song}, Y. Tony and {Gross}, Richard S.},
title = "{Linking Oceanic Tsunamis and Geodetic Gravity Changes of Large Earthquakes}",
journal = {Pure and Applied Geophysics},
keywords = {Tsunami observations, large earthquakes, satellite gravity},
year = 2017,
month = aug,
volume = {174},
number = {8},
pages = {3029-3041},
abstract = "{Large earthquakes at subduction zones usually generate tsunamis and
coseismic gravity changes. These two independent oceanic and
geodetic signatures of earthquakes can be observed individually
by modern geophysical observational networks. The Gravity
Recovery and Climate Experiment twin satellites can detect
gravity changes induced by large earthquakes, while altimetry
satellites and Deep-Ocean Assessment and Reporting of Tsunamis
buoys can observe resultant tsunamis. In this study, we
introduce a method to connect the oceanic tsunami measurements
with the geodetic gravity observations, and apply it to the 2004
Sumatra Mw 9.2 earthquake, the 2010 Maule Mw 8.8 earthquake and
the 2011 Tohoku Mw 9.0 earthquake. Our results indicate
consistent agreement between these two independent measurements.
Since seafloor displacement is still the largest puzzle in
assessing tsunami hazards and its formation mechanism, our study
demonstrates a new approach to utilizing these two kinds of
measurements for better understanding of large earthquakes and
tsunamis.}",
doi = {10.1007/s00024-017-1510-5},
adsurl = {https://ui.adsabs.harvard.edu/abs/2017PApGe.174.3029F},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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