本文選題：衛(wèi)星測(cè)高 + 中國(guó)近海及鄰域　； 參考：《中國(guó)石油大學(xué)（華東）》2013年碩士論文

【摘要】：重力異常由于地球質(zhì)量分布不規(guī)則造成的重力場(chǎng)中各點(diǎn)的重力矢量和正常重力矢量的數(shù)量之差,是研究地球形狀、地球內(nèi)部結(jié)構(gòu)和重力勘探，以及修正空間飛行器的軌道的重要數(shù)據(jù)，被廣泛應(yīng)用于物理海洋學(xué)、地球物理學(xué)等領(lǐng)域的研究。但是長(zhǎng)期以來(lái)探測(cè)方法單一與探測(cè)技術(shù)的落后使得海洋重力資料的嚴(yán)重缺乏,衛(wèi)星測(cè)高技術(shù)可以提供大范圍、高精度、長(zhǎng)時(shí)間序列的海面觀(guān)測(cè)資料，其結(jié)果可以很好地詮釋海洋大地水準(zhǔn)面和重力異常，具有傳統(tǒng)技術(shù)無(wú)可比擬的優(yōu)勢(shì)，逐步成為獲取海洋重力場(chǎng)數(shù)據(jù)的主要手段。 本文聯(lián)合利用Geosat、Geosat、ERS-1、ERS-1、ERS-2、Envisat、T/P、Jason-1和Jason-2多種測(cè)高衛(wèi)星數(shù)據(jù)，對(duì)數(shù)據(jù)進(jìn)行數(shù)據(jù)編輯和共線(xiàn)處理，有效的減小了數(shù)據(jù)容量，再經(jīng)參考橢球和參考框架基準(zhǔn)的統(tǒng)一得到海面高值，采用移去-恢復(fù)方法，基于EGM2008重力場(chǎng)模型和DNSC08海面地形模型，用相鄰測(cè)高點(diǎn)大地水準(zhǔn)面高度的一次差分求沿軌垂線(xiàn)偏差，然后基于最小二乘原理直接解算了中國(guó)近海及其鄰域2′×2′分辨率垂線(xiàn)偏差子午分量和卯酉分量�；谀鎂ening-Meinesz公式，采用不同的殘余垂線(xiàn)偏差范圍和不同的積分半徑分別反演中國(guó)近海及其鄰域重力異常，并與選擇中渤海地球和東海北部地區(qū)船測(cè)重力數(shù)據(jù)進(jìn)行比對(duì)。 根據(jù)上述流程，，剔除殘余垂線(xiàn)偏差絕對(duì)值大于3″的點(diǎn)，以45′為積分半徑，確定了中國(guó)近海及其鄰域2′×2′分辨率重力異常，與船測(cè)重力數(shù)據(jù)進(jìn)行比較，精度在3.92~4.437mGal之間，總體精度為4.154mGal。
[Abstract]:The difference between the number of gravity vectors at each point in the gravity field caused by the irregular distribution of the mass of the earth and the number of normal gravity vectors is the study of the shape of the earth, the internal structure of the earth and gravity exploration. It is widely used in the research of physical oceanography, geophysics and so on. However, for a long time, the singleness of exploration methods and the backwardness of detection techniques have made the marine gravity data seriously lacking. Satellite altimetry technology can provide large range, high precision and long time series sea surface observation data. The results can well interpret the ocean geoid and gravity anomaly, and have the unparalleled advantages of traditional technology, and gradually become the main means to obtain marine gravity field data. In this paper, the data are edited and collinear processed by using geosatine ERS-1 / ERS-1 / ERS-2 / Envisato T / P / Jason-1 and Jason-2 altimetry satellite data. The data capacity is reduced effectively, and then the sea surface height value is obtained by the unification of reference ellipsoid and reference frame datum, and the moving-recovery method is adopted. Based on EGM2008 gravity field model and DNSC08 sea surface terrain model, the vertical line deviation along the orbit is obtained by using the first order difference of geoid height of adjacent high points. Then, based on the least square principle, the meridian and unitary components of the vertical line deviation of 2'脳 2 'resolution in the coastal waters of China and its adjacent areas are directly solved. Based on the inverse Vening-Meinesz formula, different ranges of residual vertical deviations and different integral radii are used to invert the gravity anomalies off the coast of China and its adjacent areas, respectively, and to compare them with the gravity data of ships selected from the Central Bohai Sea and the northern part of the East China Sea. According to the above procedure, the absolute value of residual perpendicular deviation greater than 3 "is excluded, and with 45 'integral radius, the 2' 脳 2'resolution gravity anomaly in the coastal waters of China and its adjacent areas is determined, and the accuracy is between 3.92 and 4.437mGal compared with the ship gravity data. The overall accuracy is 4.154mGal.
【學(xué)位授予單位】：中國(guó)石油大學(xué)（華東）
【學(xué)位級(jí)別】：碩士
【學(xué)位授予年份】：2013
【分類(lèi)號(hào)】：P228.3

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