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Table 2 Weighted-mean bottom slopes calculated as \(\sqrt{G_x^2+G_y^2}\)

From: Relationship between pressure variations at the ocean bottom and the acceleration of its motion during a submarine earthquake

Observatory

\(\sqrt{G_x^2+G_y^2}\)

KMA02

0.0178

KMA03

0.0446

KMA04

0.0276

KMB05

0.0238

KMB06

0.0619

KMB08

0.0555

KMC09

0.0710

KMD16

0.0089

KME17

0.0249

KME18

0.0543