Abstract:Ocean bottom pressure-gauge (OBP) records play an important role in
seafloor geodesy, but oceanographic fluctuations in OBP data are a major
source of noise in seafloor transient crustal deformation observations,
including slow slip events (SSEs), so it is important to evaluate them
properly. To extract the significant characteristics of the
oceanographic fluctuations, we applied principal component analysis
(PCA) to the 3-year Dense Oceanfloor Network System for Earthquakes and
Tsunamis (DONET) OBP time serie… Show more
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