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   altimetry data 的翻译结果: 查询用时:0.199秒
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altimetry data
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  测高资料
     Study on Tidal Model Derived from Satellite Altimetry Data
     由卫星测高资料确定海洋潮汐模型的研究
短句来源
     Free air gravity anomaly, which was derived from satellite altimetry data of Seaset, Geosat, ERS-1 and TOPEX/POSEIDON, is used to calculate Bouguer gravity anomaly of China sea and its adjacent regions combining ETOPO5 global sea floor topographic data. Moho interface depth is inverted by using Bouguer anomaly in this region.
     利用中国海及邻域 2’× 2’由Seaset,Geosat,ERS 1及TOPEX/POSEIDON等卫星测高资料解算的自由空气重力异常 ,结合ETOPO5全球海底地形资料计算了中国海及邻域布格重力异常 ,并反演了得到了中国海及邻域地壳厚度 .
短句来源
     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.
短句来源
     The first 2 years of TOPEX satellite altimetry data have been analyzed t0 the rise rate inglobal mean sea level and in the regional mean sea level near Shanghai coast, which were es timated as 1. 6mm/yr and 2. 1mm/yr, resectively. These results are well consistent with theresults from the tide gauge data, with higher accuracy than the tide gauge results.
     利用头两年的TOPEX卫星测高资料初步测定了全球平均海平面和上海邻近海域海平面上升速率分别为1.6mm/yr和21mm/yr,这与验潮站资料测得的结果相近,而且比后者有更高的精度。
短句来源
     The Application of Satellite Altimetry Data in Ocean Margin Geology and Geophysics Research
     卫星测高资料在边缘海地质与地球物理研究中的应用
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  测高数据
     Airborne laser scanning altimetry data filtering
     机载激光扫描测高数据滤波
短句来源
     Along with the abundance of the earth gravity field model, gravity data in the earth surface, GPS/leveling data, DTM, satellite altimetry data, satellite gravity data (SST, SGG) and other related information of the earth gravity field, the determination of cm order geoid has been provided with necessary condition.
     随着地球重力场模型、地面重力数据、GPS水准数据、数字地面模型(DTM)、卫星测高数据和卫星重力(SST、SGG)数据及其他地球重力场相关信息的丰富,为确定厘米级大地水准面提供了必要条件。
短句来源
     Methods of Multi-Satellite Altimetry Data Processing and Its Application
     近海多卫星测高数据联合处理的方法及应用
短句来源
     Tidal parameters of 9 constituents in South China Sea(8°~23°N,109°~120°E) are estimated from about 10 years of T/P altimetry data. Alias periods and Rayleigh periods of principal tides under Geosat/ERM sampling are calculated. For overcoming the affect of aliasing,the following approach is adopted that only 7 principal constituents are chosen.
     利用近十年的T/P测高数据来反演南海(8°~23°N,109°~120°E)九个主要分潮的潮汐参数,并计算了Geosat/ERM卫星对应的各主分潮的混叠周期及Rayleigh周期。
短句来源
     In the end, as an application of the formula derived in this paper,we estimate the innermost zone effects of the gravity recovery from ERS-1 altimetry data for an area of 6°×6° in North Atlantic,and analyze the results of the estimation.
     最后利用ERS_1卫星测高数据,根据本文提出的方法计算垂线偏差分量,采用本文导出的内区效应公式计算了北大西洋6°×6°区域内区效应对测高重力结果的影响.
短句来源
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  “altimetry data”译为未确定词的双语例句
     The sea level anomaly (SLA) and mesoscale eddies during the period from 1993 through 2004 in the Kuroshio extension region(120oE-170oE, 25oN-45oN) and South China Sea(105oE-121oE, 0oN-25oN) are analyzed using altimetry data from CNES detected by TP/Jason-1 and ERS/ENVISAT.
     本文以CNES提供的12年(1993-2004年)卫星高度计TOPEX/Poseidon、Jason-1和ERS/ENVISAT网格化融合数据SLA,对黑潮延伸区(120oE-170oE,25oN-45oN)和南海海域(105oE-121oE,0oN-25oN)的海平面异常及中尺度涡进行了统计分析分析。
短句来源
     Ensemble Methods and Applications to Altimetry Data Assimilation in the Pacific
     集合同化方法在太平洋海洋高度计资料同化中的应用研究
短句来源
     The characteristics of sea level anomaly(SLA) and mesoscale eddies during 1993~2004 year in the Kuroshio extension region are analyzed using altimetry data detected by TP/Jason-1 and ERS/ENVISAT.
     利用1993~2004年卫星高度计TP/Jason-1和ERS/ENVISAT提供的海平面异常(SLA)融合数据,分析了黑潮延伸区12年来的平均海平面异常的变化特征及中尺度涡的分布规律。
短句来源
     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
短句来源
     Tide separation from the altimetry data using harmonic analysis method
     运用调和分析方法分离卫星高度计资料中的潮汐信息
短句来源
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  altimetry data
Free-Air Anomalies (FAA) for the Norwegian marine area including some parts of the North Sea, the Norwegian Sea and the Barents Sea are computed from satellite altimetry data.
      
Recovery of marine gravity anomalies from ERS1, ERS2 and ENVISAT satellite altimetry data for geoid computations over Norway
      
The first attempt has been made at determining the differences between mean sea-levels, using the recent satellite altimetry data [1].
      
Moreover, in all seasons, the Rim Current reconstructed according to the altimetry data is characterized by a narrower jet almost along the entire its length.
      
Seasonal variability of geostrophic currents in the Atlantic Ocean according to the altimetry data
      
更多          


The first 2 years of TOPEX satellite altimetry data have been analyzed t0 the rise rate inglobal mean sea level and in the regional mean sea level near Shanghai coast, which were es timated as 1. 6mm/yr and 2. 1mm/yr, resectively. These results are well consistent with theresults from the tide gauge data, with higher accuracy than the tide gauge results.

利用头两年的TOPEX卫星测高资料初步测定了全球平均海平面和上海邻近海域海平面上升速率分别为1.6mm/yr和21mm/yr,这与验潮站资料测得的结果相近,而且比后者有更高的精度。

In this paper, the gridding problem of Satellite Altimetry Data is inquired into from selection of gridding space, the struct of the data points and the gridding operator, etc. Meanwhile the authors bring up a new gridding data method in the frequency domain,finally,the authors analyze two cycles Topex/Peseidon Satellite Altimetry Data in accordance with method in this paper,and reach some experiences of the gridding Satellite Altimetry Data.

本文从卫星测高数据处理中网距的选取、数据点的图形结构、网格算子等三个方面加以讨论,提出了频域中数据网格化的方法,最后利用两个周期的Topex/Poseidon卫星测高数据进行计算分析,得出了一些卫星测高数据网格化的经验。

The authors compare the theoretical values predicted by two anelastic models with the recently observed ones of tides and the Earth rotation variations at M 2, M f, M m, Chandler wobble and 18.6 year frequencies. The response of mantle anelasticity at different frequencies is analyzed, and the observed results of space geodesy are used to constrain the theoretical models of anelasticity. The results show that Zschau's model can interpret the observed amplitude of anelastic Love number in the...

The authors compare the theoretical values predicted by two anelastic models with the recently observed ones of tides and the Earth rotation variations at M 2, M f, M m, Chandler wobble and 18.6 year frequencies. The response of mantle anelasticity at different frequencies is analyzed, and the observed results of space geodesy are used to constrain the theoretical models of anelasticity. The results show that Zschau's model can interpret the observed amplitude of anelastic Love number in the regime from the seismic frequency to the 18.6 year frequency. 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.

利用最新的潮汐和地球自转变化在 M2 、Mf、Mm 、Chandler 摆动和18 .6 年频率上的实测值与两种滞弹模型预测的理论值的比较,分析地幔滞弹性在不同频率上的响应,空间测地结果被用来约束理论的滞弹模型.结果表明,Zschau 的理论模型可以解释从地震频段至18 .6 年频率的滞弹勒夫数的观测振幅.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.

 
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