Favali P, Beranzoli L. Seefloor observatory science: A review. Ann Geophys, 2006, 49: 515-567 [2] 汪品先. 从海底观察地球——地球系统的第三个观测平台. 自然杂志, 2007, 29: 125-130 [3] Glenn S M.[J].Schofield O M, Chant R, et al. The LEO-15 Coastal Cabled Observatory——Phase II for the Next Evolutionary Decade ofOceanography. SSC06-Scientific Submarine Cable.2006,:- [4] 同济大学海洋地质国家重点实验室. 国际海底观测系统调查报告. 2006, 12 [5] 陈鹰, 杨灿军, 陶春辉, 等. 海底观测系统. 北京: 海洋出版社, 2006 [6] National Science Foundation Cyberinfrastructure Council. Cyberinfrastructure Vision for 21st Century Discovery, 2007 [7] Gao S, Cheng P, Wang Y P, et al. Characteristics of suspended sediment concentrations over the areas adjacent to the Changjiang Riverestuary, the summer of 1998. Marine Sci Bull, 2000, 2: 14-24 [8] Lozovatsky I, Liu Z Y, Wei H, et al. Tides and mixing in the northwestern East China Sea Part I: Rotating and reversing tidal flows. ContShelf Res, 2008, 28: 318-337 [9] 程鹏, 高抒. ADCP 测量悬沙浓度的可行性分析与现场标定. 海洋与湖沼, 2001, 32: 168-176 [10] Wang X H. Tidal-induced sediment resuspension and the bottom boundary layer in an idealized estuary with a muddy bed. J PhysOceanogr, 2002, 32: 3113-3130 [11] Werner S R, Beardsley R C, Lentz S J, et al. Observations and modeling of the tidal bottom boundary layer on the southern flank ofGeorges Bank. J Geophys Res, 2003, 108: 8005, doi:10.1029/2001JC001271 [12] Carayannis G P. The earthquake and tsunami of 27 February 2010 in Chile-Evaluation of source mechanism and of near and far-fieldtsunami effects. Sci Tsunami Hazards, 2010, 29: 96-126 [13] Yu F J, Yuan Y, Zhao L D, et al. Evaluation of potential hazards from teletsunami in China: Tidal observations of a teletsunami generatedby the Chile 8.8 Mw earthquake. Chinese Sci Bull, 2011, 56: 1108-1116
[2]
Favali P, Beranzoli L. Seefloor observatory science: A review. Ann Geophys, 2006, 49: 515-567
Glenn S M.[J].Schofield O M, Chant R, et al. The LEO-15 Coastal Cabled Observatory——Phase II for the Next Evolutionary Decade ofOceanography. SSC06-Scientific Submarine Cable.2006,:-
[5]
同济大学海洋地质国家重点实验室. 国际海底观测系统调查报告. 2006, 12
[6]
陈鹰, 杨灿军, 陶春辉, 等. 海底观测系统. 北京: 海洋出版社, 2006
[7]
National Science Foundation Cyberinfrastructure Council. Cyberinfrastructure Vision for 21st Century Discovery, 2007
[8]
Gao S, Cheng P, Wang Y P, et al. Characteristics of suspended sediment concentrations over the areas adjacent to the Changjiang Riverestuary, the summer of 1998. Marine Sci Bull, 2000, 2: 14-24
[9]
Lozovatsky I, Liu Z Y, Wei H, et al. Tides and mixing in the northwestern East China Sea Part I: Rotating and reversing tidal flows. ContShelf Res, 2008, 28: 318-337
Wang X H. Tidal-induced sediment resuspension and the bottom boundary layer in an idealized estuary with a muddy bed. J PhysOceanogr, 2002, 32: 3113-3130
[12]
Werner S R, Beardsley R C, Lentz S J, et al. Observations and modeling of the tidal bottom boundary layer on the southern flank ofGeorges Bank. J Geophys Res, 2003, 108: 8005, doi:10.1029/2001JC001271
[13]
Carayannis G P. The earthquake and tsunami of 27 February 2010 in Chile-Evaluation of source mechanism and of near and far-fieldtsunami effects. Sci Tsunami Hazards, 2010, 29: 96-126
[14]
Yu F J, Yuan Y, Zhao L D, et al. Evaluation of potential hazards from teletsunami in China: Tidal observations of a teletsunami generatedby the Chile 8.8 Mw earthquake. Chinese Sci Bull, 2011, 56: 1108-1116
