1.Observation of mesoscale eddy fields in the sea southwest of Taiwan by TOPEX/POSEIDON altimeter data
用TOPEX/POSEIDON高度计识别台湾西南海域中尺度强涡
2.The harmonic analysis along satellite orbit are used to withdraw tidal wave from TOPEX/POSEIDON satellite altimeter data in the Bohai Sea, Yellow Sea, East China Sea and South China Sea.
文中对Topex/Poseidon高度计资料进行了沿轨调和分析。
3.First of all, research about the accuracy and the coherence of the data compared with TOPEX/POSEIDON has been done in this thesis.
本文首先对JASON-1海洋观测资料的精度及其与TOPEX/POSEIDON数据的一致性进行了研究;
4.Based on anelastic model and ocean tide model determined by Topex/Poseidon satellite altimetry data, the authors also present the theoretical values of the tidal response at M f and M m frequencies in consideration of mantle anelasticity and non equilibrium ocean tide effects.
本文还依据滞弹模型和Topex/Poseidon 卫星测高资料确定的海潮模型,给出顾及地幔滞弹性和非平衡海潮效应的 Mf 和Mm 频率的潮汐响应理论值.
5.The sea surface variability of Antarctic Circumpolar Current (ACC) is investigated from 8 years of merged Topex/Poseidon data (January 1993 to December 2000). The study area is a torus from 40°S to 60°S and covers most of the mean axis of ACC.
采用TOPEX/POSEIDON(T/P)卫星高度计 1 993年 1月— 2 0 0 0年 1 2月海面高度数据 ,研究包含了整个南极绕极流流系 (40°— 6 0°S)的海面高度低频变化。
6.Sea surface height anomaly and geostrophic circulation variations in the South China Sea from TOPEX/POSEIDON altimetry
用TOPEX/POSEIDON资料研究南海海面高度和地转流的季节变化
7.Moreover results of P-Vector is almost accord with the surface layer geostrophic current of the South China Sea that is got by data of TOPEX/POSEIDON satellite remote sensing altimeter. The aestival current field is also found that correspond with the stream function distribution which received by the aestival surveying of South China Sea in 1998 and 2000. Finally, the article discusses the factors that influence calculation and actual measurement current field.
而且该方法与TOPEX/POSEIDON卫星遥感高度计资料得出的冬夏季的南海表层地转流场整体上一致,夏季的流场结构也与1998、2000年夏季南海调查得到的流函数分布基本符合。
8.So the recovered along-track anomalies are almost the same as ship measurements along ship trajectory. The 2′×2′ gravity anomalies with an accuracy of 10×10 -5ms -2 (RMS) limited in South China Sea —— IGG-S are recovered from Geosat/GM, ERS-1/35day and TOPEX/Poseidon altimeter data using the method mentioned above.
据此 ,利用 Geosat/GM、ERS-1 /35天及TOPEX/Poseidon三种测高数据 ,反演了南中国海域 (0°～ 2 5°N,1 0 5°～ 1 2 2°E)的 2′× 2′重力异常—— IGG-S。
9.Tidal adjoint assimilation with the TOPEX/Poseidon altimetry data in the Huanghai and Bohai Seas
黄海、渤海TOPEX/Poseidon高度计资料潮汐伴随同化
10.Geoid determination in China Sea Area is carried out with the marine deflection of the vertical computed from the altimeter data of Topex/Poseidon, ERS?2 and Geosat/GM ERM, in which 2.5′×2.5′ grids for calculation are used.
由Topex/Poseidon,ERS 1/2及Geosat/GM,ERM测高资料求解的垂线偏差计算了我国海域及其邻区大地水准面,其中计算格网为2.5′×2.5′。
