南中国海TOPEX/POSEIDON轨迹交叉点测高数据的潮汐调和分析

讨论了由卫星测高数据进行潮汐分析的混叠问题和分潮的可分辨性;用ＴＯＰＥＸ／ＰＯ－ＳＥＩＤＯＮ海面重复轨迹交叉点测高数据计算南中国海１２个分潮（Ｓａ,Ｓｓａ,Ｍｍ,Ｍｆ,Ｑ１,Ｏ１,Ｐ１,Ｋ１,Ｎ２,Ｍ２,Ｓ２,Ｋ２）的调和常数;用不同方法验证了计算结果的精度,分析表明,分潮的振幅精度和潮高精度已达到±２ｃｍ,四个较大分潮（Ｏ１,Ｐ１,Ｋ１,Ｍ２）的迟角误差不超过±７°。其中Ｏ１,Ｋ１,和Ｍ２与验潮站实测值的最大偏差小于７°;给出了最大的全日和半日分潮（Ｋ１,Ｍ２）的潮波图。     

Geomatics and Information Science of Wuhan University TOTAL CONTENTS (Vol.2 6No .1-6 ,2 0 0 1)

Ｎｏ .1ＴｈｅＴｅｃｈｎｉｑｕｅＩｎｔｅｇｒａｔｉｏｎｏｆｔｈｅＳｐａｔｉａｌＩｎｆｏｒｍａｔｉｏｎａｎｄＣｏｍｍｕｎｉｃａｔｉｏｎＬＩＤｅｒｅｎ　ＬＩＱｉｎｇｑｕａｎ( 1)……………………ＴｈｅＤｅｓｉｇｎａｎｄＩｍｐｌｅｍｅｎｔａｔｉｏｎｏｆＣｙｂｅｒＣｉｔｙＧＩＳＺＨＵＱｉｎｇ　ＬＩＤｅｒｅｎ　ＧＯＮＧＪｉａｎｙａ　ＸＩＯＮＧＨａｎｊｉａｎｇ( 8)ＬｏｏｋＤｉｒｅｃｔｉｏｎＥｒｒｏｒａｎｄＩｔｓＣｏｒｒｅｃｔｉｏｎｏｎＡｉｒｂｏｒｎｅＩｍａｇｉｎｇＳｃａｎｎｅｒＩｍａｇｅ ＹＥＺｅｔｉａｎ　ＨＥ…     

用T／P测高数据确定中国海域及其邻海的海面高及海面地形

描述了利用Ｔ／Ｐ卫星测高数据确定中国海域及其邻海的海面地形。处理了Ｔ／Ｐ５９～８２周（Ｃｙｃｌｅ）１９９４年第８３ｄ～３１１ｄ的数据，将５９～８２周数据分成两部分分别估计海面高，并分析了海面高变化。结果与Ｂａｓｉｃ和Ｒａｐｐ１９９２年确定的海面高作了比较。利用Ｓｈｅｐａｒｄ曲面拟合方法给出了３０′×３０′平均海面高结果，分别以ＯＳＵ９１和ＷＤＭ９４地球重力场模型作为参考重力场，计算了相应的３０′×３０′平均海面地形。     

全站仪与计算机数据通讯

本文介绍徕卡（ＬＥＩＣＡ）、日本尼康（ＮＩＫＯＮ）、索佳（ＳＯＫＫＩＡ）、拓普康（ＴＯＰＣＯＮ）、宾得（ＰＥＮＴＡＸ）、瑞典捷创力（ＧＥＯＤＩＭＥＴＥＲ）全站仪与ＰＣ—Ｅ５００袖珍计算机、惠普ＨＰ１００／ＨＰ２００掌上机、ＩＢＭ台式计算机联机使用，介绍了全站仪的数据格式、通讯程序和使用方法。     

地图信息识别与提取技术的研究与实践

地图信息识别与提取技术的研究与实践ＴＨＥＳＴＵＤＹＡＮＤＰＲＡＣＴＩＳＥＯＮＴＨＥＴＥＣＨＮＩＣＯＦＲＥＣＯＧＮＩＴＩＯＮＡＮＤＥＸＴＲＡＣＴＩＯＮＯＦＭＡＰＩＮＦＯＲＭＡＴＩＯＮ郝向阳（郑州测绘学院,郑州,４５００５２）在建立地理信息系统和各种地图...     

规划GIS基础信息录入探讨

本文就ＧＥＮＡＭＡＰ对基础信息（地形图）的处理方法加以分析与探讨,提出用ＡＵＴＯＣＡＤ１２．０进行１：５０００的形图数字化,输出ＤＸＦ格式文件,然后再转换到ＧＥＮＡＭＡＰ中去,在数字化操作和软件编制时应注意的几个事项。     

利用MIVIS数据进行遥感图像模拟的研究

本文研究利用机载ＭＩＶＩＳ超光谱成像系统数据,运用光谱模拟,大气改正的方法,定量模拟了ＳＰＯＴ－ＨＲＶ ＸＳ１、ＸＳ２、ＸＳ３的地面反射率图像,并将模拟结果与相应的地面反射率实测值进行了对比。同时对成像系统ＭＴＦ的影响也进行了定量模拟分析。试验结果显示,ＳＰＯＴ图像的模拟值与地面实测值相一致。     

卫星高度计反演海面风速——模式函数与应用实例

对迄今为止国际上公开发表的１４ 种卫星高度计反演海面风速的模式函数进行了系统的分析和比较。在此基础上提出了一种“折中”模式函数,用于ＴＯＰＥＸ 资料海面风速反演效果良好。文中对高度计获取的全球海面风速分布特征进行了分析,最后探讨了改善海面风速模式函数反演精度的途径。     

利用TOPEX/Poseidon卫星测高资料监测全球海平面变化

本文利用１９９３年１月至１９９９年５月的ＴＯＰＥＸ／Ｐｏｓｅｉｄｏｎ卫星测高数据计算了全球海平变化。海平面模型误差和不恰当的加权方法都会影响全球海平面序列的周年变化,潮汐模型误差对于季节性变化有明显的影响。利用两个高度计算的海平面变化存在周年变化存在明显的差异,利用ＴＯＰＥＸ高度计和Ｐｏｓｅｉｄｏｎ高度计得到的该时段全球平均海平面的变化率分别为２．０ｍｍ／ａ和－０．５ｍｍ／ａ。与南方涛动指数的比较     

PC—E500机系统盘介绍及应用初探

本文对ＰＣ－Ｅ５００袖珍机未公开的系统盘Ｓ１和Ｓ２及系统管理文件作了详细介绍；公开了两个未公开命令ＢＴＥＸＴ＄和ＢＤＡＴＡ＄的用法；对系统盘Ｓ１和Ｓ２的开发应用作了初步探讨，结合Ｓ１和Ｓ２的特性，给出了一种保护内存程序的简易方法。     

以相邻点海面高度差为观测量的沿迹调和分析新方法

采用TOPEX/POSEIDON卫星轨迹上相邻点的海面高差作为观测量,在交叉点分析结果的控制下构成同一弧段上观测量在两相邻交叉点间的综合观测方程,以轨迹上纬差0.1°的正常点的潮汐参数构成总体待估参数系列,实施最小二乘综合解算。分析结果表明,这种差分模式可以基本消除非潮汐因素的影响,提高潮汐参数估计的精度和可靠性,可比一般沿迹逐点分析给出更为平滑的沿迹参数分布,更符合海洋潮汐运动的物理背景。     

由ERS-2和TOPEX卫星测高数据推算的海面高异常的主成分分析

利用1995~2003年间的TOPEX/POSEIDON和ERS-2卫星测高数据,尽量采用相同的改正模型对TOPEX和ERS-2卫星测高数据分别进行改正,然后由共线分析法分别推算了全球1°×1°的35 d的海面高异常时间序列,并采用主成分分析法分别对这两个海面高异常时间序列进行了分析。     

Comparison between the harmonic and response methods of tidal analysis using TOPEX/POSEIDON altimetry

Three years of TOPEX/POSEIDON altimeter data have been processed at Delft Institute for Earth-Oriented Space Research (DEOS) to solve the major diurnal and semi-diurnal constituents of the global ocean tide using the two classical methods of tidal analysis, i.e. the harmonic and response analyses. Some experiments with the parameters in the response formalism show that the tidal admittance in both the diurnal and semi-diurnal band can be adequately described with a lag interval of 2 days and a number of lags of three. Results of both methods are evaluated from the differences with the most recent Grenoble hydrodynamic model (FES95.2) and from the fit with the harmonic constants of a globally distributed set of tide gauges. It was found that the solutions of the two methods differ at the millimeter level and are thus fully equivalent, which is confirmed by the tide gauges and the differences with FES95.2. From the comparisons with the Grenoble model it was found that the M ₂ and S ₂ solutions of that model likely contain bathymetric errors which are of the order of 1–2 cm for M ₂ and 0.5 cm for S ₂. Received: 18 December 1996 / Accepted: 12 May 1997     

Analysis of the bias between TOPEX and GPS vTEC determinations

The TOPEX/Poseidon satellite was jointly developed and deployed by the National Aeronautics and Space Administration (NASA), USA, and the Centre National d’Etudes Spatiales (CNES), France (for details see Chelton et al. In: Fu L-L, Cazenave A (eds) International geophysics series, vol 69, ISBN 0-12-269545-3, Academic Press, CA, pp 1–131, 2001), with the main scientific goal of sea surface height monitoring. The process that ends with the TOPEX main observable (the range between the satellite and the sea surface) involves the measurement of several parameters of the radar pulses reflected by the sea surface and the computation of several other corrections. After several calibration campaigns performed by the Calibration/Validation team of the mission, it was found that TOPEX range determinations were systematically shorter than expected and it was decided to add an empirical correction of +15 mm to the TOPEX range-computation algorithm. As a by-product, TOPEX provides vertical total electron content (vTEC) determinations which have turned out to be a very important data source for the ionospheric research community. Since TOPEX vTEC measurements became available, several comparison studies have detected a constant bias, from +2 to +5 TECu, when TOPEX is compared to other vTEC sources, e.g., Global Positioning System (GPS), Doppler Orbitography and Radio-positioning Integrated by Satellite (DORIS), (TOPEX always greater than the others). In this work, we show that miscalibration of the corrections used in the TOPEX processing algorithm can cause the shortening effect of TOPEX ranges and at the same time the constant bias on the TOPEX vTEC values. It is also shown that changes on TOPEX System Biases of less than 10 mm for the Ku-band and between 40 and 70 mm for the C-band, can make both effects disappear. The analyzed hypothesis is supported by theoretical considerations and data analysis available in the specialized literature. On behalf of the authors of the contribution ‘Analysis of the bias between TOPEX and GPS vTEC determinations’, I declare that the paper has not been, nor is in the process of being published in any other publication.     

TOPEX/Poseidon卫星监测博斯腾湖水位变化及其与NINO3 SST的相关性分析

利用TOPEX/Poseidon(T/P)卫星10年（1992~2002）监测博斯腾湖水位变化的GDR数据,经过数据的地球物理改正、编辑、约化和滤波后,分别采用小波分析和傅里叶分析得到了博斯腾湖水位变化的平均周期为1034d,363d,182d和47d。季节性变化是湖泊水位变化的主项,利用最小二乘法得到了周年振幅为0.7196m,半年振幅为0.5322m,因此季节性变化的主周期是周年,次周期是半年。博斯腾湖水位变化变化趋势为0.2012m/a,说明在全球气候变暖趋势下,博斯腾湖水位在升高。由博斯腾湖月水位变化的时间序列与NINO3 SST进行相关性分析,发现在NINO3 SST 发生6个月后,博斯腾湖月水位变化序列与NINO3 SST数据相关性最大(-0.2784),表明厄尔尼诺事件对我国西部气候影响的具有一定的滞后性。     

卫星激光测高ICESat确定海面高精度分析

讨论了ICESat卫星在大地测量学与海洋学中的应用,利用目前国际上公认的最高精度的测高数据TOPEX,分析了ICESat确定的海平面高以及中尺度的海面异常精度,给出了统计结果。     

Temporal and spatial variability of the bias between TOPEX- and GPS-derived total electron content

Total electron content (TEC) predictions made with the GPS-based la plata ionospheric model (LPIM) and the International Reference Ionosphere (IRI95) model were compared to estimates from the dual-frequency altimeter onboard the TOPEX/Poseidon (T/P) satellite. LPIM and IRI95 were evaluated for the location and time of available T/P data, from January 1997 to December 1998. To investigate temporal and spatial variations of the TEC bias between T/P and each model, the region covered by T/P observations was divided into ten latitude bands. For both models and for all latitudes, the bias was mainly positive (i.e. T/P values were larger); the LPIM bias was lower and less variable than the IRI95 bias. To perform a detailed analysis of temporal and spatial variability of the T/P-LPIM TEC bias, the Earth’s surface was divided into spherical triangles with 9°-sides, and a temporally varying regression model was fitted to every triangle. The highest TEC bias was found over the equatorial anomalies, which is attributed to errors in LPIM. A significant TEC bias was found at 40°N latitude, which is attributed to errors in the T/P Sea State Bias (SSB) correction. To separate systematic errors in the T/P TEC from those caused by LPIM, altimeter range biases estimated by other authors were analysed in connection with the TEC bias. This suggested that LPIM underestimates the TEC, particularly during the Southern Hemisphere summer, while T/P C-band SSB calibration is worse during the Southern Hemisphere winter.     

联合TOPEX/Poseidon与Geosat／ERM建立区域潮汐模型的研究测高资料

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。根据潮汐参数提取的要求,选取了7个主分潮,为了克服混叠影响,将T/P沿迹点处的主要分潮间的5组差比关系引入到Geosat沿迹点处,并利用T/P提供的Sa模型去除Sa对M2的扰动影响。精度估计的结果表明,Geosat/ERM反演的潮汐参数的精度与传统的月分析结果的精度相近;因差比关系的捆绑,整个全日和半日潮族迟角偏差相近,这主要和Geosat/ERM的轨道设计有关。本文的方法可以应用于利用轨道调整后的T/P卫星的测高数据提取潮汐参数。     

联合TOPEX/Poseidon与Geosat/ERM测高资料建立区域潮汐模型的研究

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。根据潮汐参数提取的要求,选取了7个主分潮,为了克服混叠影响,将T/P沿迹点处的主要分潮间的5组差比关系引入到Geosat沿迹点处,并利用T/P提供的Sa模型去除Sa对M2的扰动影响。精度估计的结果表明,Geosat/ERM反演的潮汐参数的精度与传统的月分析结果的精度相近;因差比关系的捆绑,整个全日和半日潮族迟角偏差相近,这主要和Geosat/ERM的轨道设计有关。本文的方法可以应用于利用轨道调整后的T/P卫星的测高数据提取潮汐参数。