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Calculation of geoid undulations and gravity anomalies in the Northwest Pacific by using the Topex/Poseidon and Geosat altimeter data
作者姓名:Pan Jiayi  Wang Junqin  Wang Yanfeng  Zhang Xinmei  Yuan Yeli  Zheng Quan'an
作者单位:Pan Jiayi; Wang Junqin; Wang Yanfeng; Zhang XinmeiYuan Yeli (First Institute of Oceanography State Oceanic Adminitration,Qingdao 266003 China
摘    要:INTRODUCTIONThegeoidistheiargeopotentials~econfidingmostlywiththemeanseasurfaceandisdenotedastheheightrelativetotheidealelliPSes~eoftheearth.Thegeoidundulationsinglobalaceareupto100m.TheunevenstructureOftheearthgivesrisetotheunevenfeatureofthecitysot...

关 键 词:Geoid  undulations  gravity  anomalies  Northwest  Pacific  Topex/Poseidon  and  Geosat  altimeter  data
收稿时间:1998/6/11 0:00:00
修稿时间:1998/12/15 0:00:00

Calculation of geoid undulations and gravity anomalies in the Northwest Pacific by using the Topex/Poseidon and Geosat altimeter data
Pan Jiayi,Wang Junqin,Wang Yanfeng,Zhang Xinmei,Yuan Yeli,Zheng Quan''an.Calculation of geoid undulations and gravity anomalies in the Northwest Pacific by using the Topex/Poseidon and Geosat altimeter data[J].Acta Oceanologica Sinica,1999,18(4):523-533.
Authors:Pan Jiayi  Wang Junqin  Wang Yanfeng  Zhang Xinmei  Yuan Yeli and Zheng Quan'an
Institution:1.First Institute of Oceanography State Oceanic Adminitration, Qingdao 266003 China2.Center for Rerrnte Sensing, College of Marine Studies, University of Delaware, Newark, DE 19716, USA
Abstract:The geoid undulations in the Northwest Pacific were calculated by using the Topex/Paseidon and Geoeat altirreter data.Firstly the bias between two types of the altimeter data was removed and the geoid undulations in the Northwest Pacific were acquired by a long wave bias diminishing model with a resolution of 30 km and precision of 14 cm.Then an algorithm of inversion of gravity artarrtalies was derived,and the gravity anomalies in the East China Seawere calculated by using the algorithm and the geoid undulationts.The rms of difference between the in situ measurements and the gravity anomalies from altimeter data was 3.8×10-5 m/s2.A method to calculate the gravity artornalies in a larger area was developed which combined gravity anomalies in four subregions overlapping each other into one data set in a larger region.The error analysys shows that the model and result of the inversion of gravity anomalies were reliable.
Keywords:Geoid undulations  gravity anomalies    Northwest Pacific  Topex/Poseidon  and Geosat altimeter data
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