Rabinovich A B. Spectral analysis of tsunami waves: Separation of source and topography effects. J Geophys Res, 1997, 102:12663-12676
[2]
Welch, P D. The use of fast Fourier transform for the estimation of power spectra: A method based on time averaging over short, modifiedperiodograms. IEEE Trans Audio Electroacoust, 1967 AU-15: 70-73
[3]
Yuan Y, Wei H, Zhao L, et al. Implications of intermittent turbulent bursts for sediment resuspension in a coastal boundary layer: A fieldstudy in western Yellow Sea, China. Mar Geol, 2009, 263: 87-96
[4]
Liu P L-F, Wang X M, Salisbury A J. Tsunami hazard and early warning system in South China Sea. J Asian Earth Sci, 2009, 36: 2-12
[5]
Dao M H, Tkalich P, Soon C E, et al. Tsunami propagation scenarios in the South China Sea. J Asian Earth Sci, 2009, 36: 67-73
[6]
杨华庭. 海啸及太平洋海啸预报系统. 海洋预报, 1987, 4(增刊): 68-76
[7]
Gao Y, Wang P D, Zheng S H, et al. Temporal changes in shear-wave splitting at an isolated swarm of small earthquakes in 1992 nearDongfang, Hainan Island, southern China. Geophys J Int, 1998, 135: 102-110
[8]
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. 海洋学报, 2001, 23: 30-39 [2] 叶琳, 于福江, 吴玮. 我国海啸灾害及预警现状与建议. 海洋预报, 2005, 22(增刊): 147-157 [3] Intergovernmental Oceanographic Commission (IOC). Tsunami Glossary. IOC Technical Series(85). Paris, UNESCO, 2008 [4] 于福江, 吴玮. 印度洋大海啸及其全球海啸预警系统展望. 中国科技奖励, 2005, 2: 90-91 [5] Merrifield M A, Firing Y L, Aarup T, et al. Tidal gauge observations of the Indian Ocean tsunami, December 26, 2004. Geophys Res Lett,2005, 32: L09603, doi:10.1029/2005GL022610 [6] Nagarajan B, Suresh I, Sundar D, et al. The Great Tsunami of 26 December 2004: A description based on tide-gauge data from the Indiansubcontinent and surrounding areas. Earth Planet Space, 2006, 58: 211-215 [7] Ichinose G A, Anderson J G. The potential hazard from tsunami and Seiche waves generated by large earthquakes within Lake Tahoe,California-Nevada. Geophys Res Lett, 2000, 27: 1203-1206 [8] Rabinovich A B. Spectral analysis of tsunami waves: Separation of source and topography effects. J Geophys Res, 1997, 102:12663-12676 [9] Welch, P D. The use of fast Fourier transform for the estimation of power spectra: A method based on time averaging over short, modifiedperiodograms. IEEE Trans Audio Electroacoust, 1967 AU-15: 70-73 [10] Yuan Y, Wei H, Zhao L, et al. Implications of intermittent turbulent bursts for sediment resuspension in a coastal boundary layer: A fieldstudy in western Yellow Sea, China. Mar Geol, 2009, 263: 87-96 [11] Liu P L-F, Wang X M, Salisbury A J. Tsunami hazard and early warning system in South China Sea. J Asian Earth Sci, 2009, 36: 2-12 [12] Dao M H, Tkalich P, Soon C E, et al. Tsunami propagation scenarios in the South China Sea. J Asian Earth Sci, 2009, 36: 67-73 [13] 杨华庭. 海啸及太平洋海啸预报系统. 海洋预报, 1987, 4(增刊): 68-76 [14] Gao Y, Wang P D, Zheng S H, et al. Temporal changes in shear-wave splitting at an isolated swarm of small earthquakes in 1992 nearDongfang, Hainan Island, southern China. Geophys J Int, 1998, 135: 102-110
Merrifield M A, Firing Y L, Aarup T, et al. Tidal gauge observations of the Indian Ocean tsunami, December 26, 2004. Geophys Res Lett,2005, 32: L09603, doi:10.1029/2005GL022610
[14]
Nagarajan B, Suresh I, Sundar D, et al. The Great Tsunami of 26 December 2004: A description based on tide-gauge data from the Indiansubcontinent and surrounding areas. Earth Planet Space, 2006, 58: 211-215
[15]
Ichinose G A, Anderson J G. The potential hazard from tsunami and Seiche waves generated by large earthquakes within Lake Tahoe,California-Nevada. Geophys Res Lett, 2000, 27: 1203-1206
