[1]
|
Haxby W F,Karner G D,Labrecque J L,et al.Digital Images of Combined Oceanic and ContinentalData Sets and Their Use in Tectonic Studies[J].EOS,Transactions,1983,64:995-1 004[2] Sandwell D T,McAdoo D C.Marine Gravity of theSouthern Ocean and Antarctic Margin from Geosat[J].Journal of Geophysical Research,1990,93(B9):10 389-10 396[3] Li Jiancheng,Ning Jinsheng,Chen Junyong,et al.Determination of Gravity Anomalies over the SouthChina Sea by Combination of TOPEX/Poseidon, ERS2and Geosat Altimeter Data[J].Acta Geodaet-ica et Cartographica Sinca,2001,30(3):197-202(李建成,宁津生,陈俊勇,等.联合 Topex/Posei-don,ERS-2和Geosat卫星测高资料确定中国近海重力异常[J].测绘学报,2001,30(3):197-202)[4] Sarrailh M,Balmino G,Doublet D.The Arctic andAntarctic Oceans Gravity Field from ERS1Altimet-ric Data[C].International Association of GeodesySymposia,Tokyo,Japan,1996[5] Hwang C,Hsu H Y,Deng Xiaoli.Marine GravityAnomaly from Satellite Altimetry:A Comparison ofMethods Over Shallow Waters[C].InternationalAssociation of Geodesy Symposia,Matera,Italy,2003[6] McAdoo D C,Marks K M.Gravity Fields of theSouthern Ocean from Geosat Data[J].Journal ofGeophysical Research,1992,97(B3):3 247-3 260[7] Sandwell D,Smith W H F.Marine Gravity Anoma-ly from Geosat and ERS-1Satellite Altimetry[J].Journal of Geophysical Research,1997,102(B5):10 039-10 054[8] Wang Hubiao,Wang Yong,Lu Yang.High Preci-sion Vertical Deflection over China Marginal Sea andGlobal Sea Derived from Multi-satellite Altimeter [J].Geomatics and Information Science of WuhanUniversity,2007,32(9):770-773(王虎彪,王勇,陆洋.联合多种测高数据确定中国边缘海及全球海域的垂线偏差[J].武汉大学学报·信息科学版,2007,32(9):770-773)[9] Bao Lifeng,Lu Yang,Wang Yong.Improved Re-tracking Algorithm for Oceanic Altimeter Wave-forms[J].Progress in Natural Science,2009,19:195-203[10] Yang Yuande,Hwang C,Hsu Hungjui,et al.ASubwaveform Threshold Retracker for ERS-1Al-timetry:A Case Study in the Antarctic Ocean[J].Computer&Geosciences(2011),doi:10.1016/j.ca-geo.2011.08.017[11] Sandwell D,Smith W H F.Retracking ERS-1Al-timeter Waveforms for Optimal Gravity Field Re-covery[J].Geophysical Journal International,2005,163(1):79-89[12] Hwang C,Guo Jinyun,Deng Xiaoli,et al.CoastalGravity Anomalies from Retracked Geosat GM Al-timetry:Improvement,Limitation and the Role ofAirborne Gravity Data[J].Journal of Geodesy,2006,80(4):204-216[13] Garcia E S,Sandwell D T,Smith W H F.Retrack-ing CryoSat-2,Envisat and Jason-1Radar AltimetryWaveforms for Improved Gravity Field Recovery[J].Geophys.J.Int.(2014),doi:10.1093/gji/ggt469[14] Yang Yuande,E Dongchen,Hwang Cheinwag,etal.Chinese Coastal Gravity Anomalies from Wave-form Retracked Geosat/GM Altimetry[J].Geomat-ics and Information Science of Wuhan University,2008,33(12):1 288-1 291(杨元德,鄂栋臣,黄金维,等.Geosat/GM波形重跟踪反演中国沿海区域重力异常[J].武汉大学学报·信息科学版,2008,33(12):1 288-1 291)[15] Jin Taoyong,Li Jiancheng,Xing Lelin,et al.Re-seach on Datum Unification of Multi-satellite Altim-etric Data[J].Journal of Geodesy and Geodynam-ics,2008,28(3):92-95(金涛勇,李建成,邢乐林,等.多源卫星测高数据基准的统一研究[J].大地测量与地球动力学,2008,28(3):92-95)[16] Olgiati A,Balmino G,Sarrailh M,et al.Gravity A-nomalies from Satellite Altimetry:Comparison Be-tween Computation via Geoid Heights and Via De-flections of the Vertical[J].Bulletin Géodésique,1995,69(4):252-260[17] Hwang C,Hsu H Y,Jang R J.Global Mean SeaSurface and Marine Gravity Anomaly from Multi-satellite Altimetry:Applications of Deflection-geoidand Inverse Vening Meinesz Formulae[J].Journalof Geodesy,2002,76(8):407-418 |