测绘学报 ›› 2014, Vol. 43 ›› Issue (11): 1101-1108.doi: 10.13485/j.cnki.11-2089.2014.0174

• 学术论文 •    下一篇

渤海湾航空重力及其在海域大地水准面精化中的应用

孙中苗1,翟振和1,2,肖云1,3   

  1. 1. 西安测绘研究所
    2. 信息工程大学
    3. 地理信息工程国家重点实验室
  • 收稿日期:2013-12-12 修回日期:2014-01-14 出版日期:2014-11-20 发布日期:2014-12-02
  • 通讯作者: 孙中苗 E-mail:sun_szm@sina.com
  • 基金资助:

    基于航空重力的陆海大地水准面拼接方法研究

Airborne Gravimetry in Bohai Bay and Its Role on the Refining of the Regional Marine Geoid

SUN Zhongmiao1,ZHAI Zhenhe2,3,XIAO Yun4,5   

  1. 1. Xi’an Institute of Surveying and Mapping
    2. Information Engineering University
    3. Institute of Surveying and Mapping
    4. State Key Laboratory of Geo-Information Engineering
    5. Xi’an Research Institute of Surveying and Mapping
  • Received:2013-12-12 Revised:2014-01-14 Online:2014-11-20 Published:2014-12-02
  • Contact: SUN Zhongmiao E-mail:sun_szm@sina.com

摘要:

近海航空重力数据在陆海大地水准面统一中起着重要作用。近三年来,利用我国首套航空重力测量系统(CHAGS)完成了渤海湾地区近20万平方千米的5??5?格网平均重力异常数据的获取。本文首先介绍了渤海湾地区航空重力测量的概况,给出了航空重力测量数据的处理要点;然后,详细讨论了航空重力测量的精度评估方法,其中针对该区域的测线布设特点,提出了“重叠格网比较法”以评估格网平均重力异常的内符合精度。结果表明,对于5?的波长分辨率,交叉点重力异常不符值在抗差后的中误差约为1.5mGal,重叠格网法获得的5??5?格网平均重力异常的中误差约为1.6mGal;5??5?格网重力异常与卫星测高和船测重力的比较精度优于3.0mGal;由航空重力测量获得的1??1?格网平均重力异常与GOCE卫星重力位模型的计算值相比较,其系统性差异小于0.5mGal、中误差约为2.7mGal。利用航空重力数据后,渤海湾区域大地水准面的精度由EGM2008模型的约23cm提高到约12cm。

关键词: 航空重力测量, 重叠格网比较法, 海域大地水准面, 卫星测高, 卫星重力

Abstract:

Offshore airborne gravity plays very important role in the unifying of the land geoid and marine geoid. Airborne gravimetry using Chinese airborne gravimetry system is flown in Bohai bay in recently three years, which the surveying area extends about two hundred thousand square kilometers and 5??5? grid mean gravity anomaly has been obtained. The gravimetry is summarized and its key processing method is introduced firstly. Then, we discuss the accuracy estimation methods for the airborne gravity in detail, and introduce so-called grid-overlapping method to appropriately evaluate the internal accuracy of the grid mean gravity anomaly. The results indicate that the standard derivation of the crossover errors is about 1.5mGa1 at the resolution of 5 arcmin, the standard deviation of the 5??5? grid mean gravity anomaly evaluated by grid-overlapping method is about 1.6mGal, and the accuracy of the 5??5? grid mean gravity anomaly are both better than 3.0mGa1 compared with the satellite altimetry gravity data and the seaborne gravity data respectively. The systemic error and the standard deviation of the 1??1? mean airborne gravity compared with the GOCE gravity field model are less than 0.5mGal and about 2.7mGal respectively. The accuracy of the regional geoid using airborne gravity data in the surveying area is improved to 12cm, whereas it is about 23cm computed from EGM2008 model.

Key words: Airborne gravimetry, Grid-overlapping method, Marine geoid, Satellite altimetry, Stellite gravity