引文
[1]于福江,叶琳,王喜年.1994年发生在台湾海峡的一次地震海啸的数值模拟[J].海洋学报,2001,23(6):32-39.
[2]叶琳,于福江,吴玮.我国海啸灾害及预警现状与建议[J].海洋预报,2005,22(S):147-157.
[3]王绍玉.印度洋地震和海啸灾害引发的若干思考[J].国际地震动态,2005,313(1):1-8.
[4]温瑞智,任叶飞.我国地震海啸危险性分析方法研究[J].世界地震工程,2007,23(1):6-11.
[5]潘文亮,王盛安,蔡树群.南海潜在海啸灾害的数值模拟[J].热带海洋学报,2009,28(6):7-14.
[6]Mansinha L,Smylie D E.The displacement fields of inclined faults[J].Bulletin of the Seismological Society of America;1971,61(5):1433-1440.
[7]Okada,Y.,1985,Surface deformation due to shear and tensilefaults in a half-space[J].Bulletin of the Seismological Society ofAmerica,75(4),113-1154.
[8]Titov V V,Gonzalez F I.Implementation and testing of the meth-od of Splitting Tsunami(MOST)model[R].NOAA TechnicalMemorandum ERL,1997.
[9]Titov V V,Numerical modeling of long wave run-up[D].Los An-geles:University of Southern California,1997.
[10]Pelayo A M,Wiens D A.Tsunami earthquakes:slow thrust-fault-ing events in the accretionary wedge[J].J Geophys Res,1992,97(15):321-337.
[11]Todorovska M I,Trifunac M D.Generation of tsunamis by aslowly spreading uplift of the sea floor[J].Soil Dynamics andEarthquake Engineering,2001,21:151-167.
[12]赵曦,王本龙,刘桦.海沟内海底地震激发的表面波[J].力学季刊,2007,28(2):195-202.
[13]祝会兵.海啸模型研究进展(I)[J].宁波大学学报(理工版),2006,19(4):536-541.
[14]Synolakis C E,Bardet J P,Borrero J C.The slump origin of the1998 Papua New Guinea tsunami[J].Proc R SocLond,2002,458:763-789.
[15]张超凡,石耀霖.海啸灾害的数值模拟研究[J].中国科学院研究生院学报,2008,25(3):289-296.
[16]Shuto.Numerical simulation of tsunami Its present and near fu-ture[J].Natural Hazards,1991,(4):171-191.
[17]Lynch D R,Gray W G.Finite element simulation of shallow wa-ter problems with moving boundaries[C].InProc.2d Conf.FiniteElements Water Resource,eds,C.A.Brebbia et al,1978.
[18]Lynch D R,Gray W G.Finite element simulation of flow in de-forming regions[J].J of Comp Phys,1980,36:135-153.
[19]Kawahra M,Hirano H,Tsubota K,Inagaki K,Selective lumpingfinite element method for shallow water flow[J].Int.J.for Nu-merical Methods in Fluids,1982,2:89-112.
[20]Kawahra M,Umetsu T.Finite element method for movingboundary problems in river flow[J].Int.J.for Numerical Meth-ods in Fluids,1986,6:365-386.
[21]孙美仙,丁照东,赵联大等.基于GIS的海啸预警信息系统集成框架[J].海洋学研究,2009,27(4):109-116.
[22]Liu P L,Cho Y S,Yoon S B,et al.Numerical simulation of the1960 Chilean tsunami propagation and inundation at Hilo,Ha-waii[C]//Tsuchiya Y,Shuto N.Tsunami Progress in Prediction,di-saster prevention and warning,Amsterdam:Kluwer AcademiPublisher,1995.
[23]Wang X M,Liu P L.An analysis of 2004 Sumatra earthquakefault plane mechanisms and Indian Ocean tsunami[J].Journal ofHydraulic Engineering and Research,2006,44(2):147-154.
[24]LeVeque R J,George D L.High-resolution finite volume meth-ods for the shallow water equations with topography anddry-states[J].Advances in Coastal and Ocean Engineering,2008,(10):43-73.
[25]Wei G,Kirby J T,Grili S T,et al.A fully nonlinear Boussinesqmodel for surface wave[J].Journal of Fluid Mechanics,1995,294:71-92.
[26]于福江,吴玮,赵联大.基于数值预报技术的新一代海啸预警[J].国际地震动态,2005(1):19-22.
[27]Wei Y,Bernarld E N,Tang L,et al.Real-time expaerimental fore-cast of the Peruvian tsunami of August 2007 for U.S.coastlines[J].Geophys Res Lett,2008,35,L04069.