The global reach of the 26 December 2004 Sumatra tsunami

被引：346

作者：

Titov, V

Rabinovich, AB

Mofjeld, HO

Thomson, RE

González, FI

机构：

[1] NOAA, Pacific Marine Environm Lab, Seattle, WA 98115 USA

[2] Dept Fisheries & Oceans Canada, Inst Ocean Sci, Sidney, BC V8L 4B2, Canada

[3] Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow 117997, Russia

来源：

SCIENCE | 2005年 / 309卷 / 5743期

关键词：

D O I：

10.1126/science.1114576

中图分类号：

O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];

学科分类号：

07 ; 0710 ; 09 ;

摘要：

Numerical model simulations, combined with tide-gauge and satellite altimetry data, reveal that wave amplitudes, directionatity, and global propagation patterns of the 26 December 2004 Sumatra tsunami were primarily determined by the orientation and intensity of the offshore seismic line source and subsequently by the trapping effect of mid-ocean ridge topographic waveguides.

引用

页码：2045 / 2048

页数：4

共 15 条

[1] Rupture process of the 2004 Sumatra-Andaman earthquake [J].

Ammon, CJ ;

Ji, C ;

Thio, HK ;

Robinson, D ;

Ni, SD ;

Hjorleifsdottir, V ;

Kanamori, H ;

Lay, T ;

Das, S ;

Helmberger, D ;

Ichinose, G ;

Polet, J ;

Wald, D .

SCIENCE, 2005, 308 (5725) :1133-1139

[2]

[Anonymous], 2005, OCEANOGRAPHY

[3]

[Anonymous], 2005, Eos

[4] A flying start, then a slow slip [J].

Bilham, R .

SCIENCE, 2005, 308 (5725) :1126-1127

[5]

Emery W.J., 2001, DATA ANAL METHODS PH

[6] EDGE WAVE AND NON-TRAPPED MODES OF THE 25 APRIL 1992 CAPE-MENDOCINO TSUNAMI [J].

GONZALEZ, FI ;

SATAKE, K ;

BOSS, EF ;

MOFJELD, HO .

PURE AND APPLIED GEOPHYSICS, 1995, 144 (3-4) :409-426

[7]

HIRATA K, UNPUB

[8]

KOSHIMURA S, 1999, COAST ENG J, V41, P167

[9] Observations by the International Tsunami Survey Team in Sri Lanka [J].

Liu, PLF ;

Lynett, P ;

Fernando, H ;

Jaffe, BE ;

Fritz, H ;

Higman, B ;

Morton, R ;

Goff, J ;

Synolakis, C .

SCIENCE, 2005, 308 (5728) :1595-1595

[10]

MARCHUK AG, 1989, P IUGG IOC INT TSUN, P11

← 1 2 →