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引用本文:丰海,李建成,李大炜,刘志勇. �µ�������ˮ׼��ģ����ο�����ˮ׼����[J]. 大地测量与地球动力学, 2013, 33(4): 133-136
作者姓名:丰海  李建成  李大炜  刘志勇
作者单位:1. 武汉大学测绘学院,武汉430079 ;北京宇航系统工程研究所,北京100076
2. 武汉大学测绘学院,武汉,430079
摘    要:?????????????????CEGM02????????LRO_LTM02??????????????α?????????????ο??????棬??????????????棬??????λ??W0??=2 822 327.8±16.2 m2 s-2??????????????????????????????????1 737 462 m??????????1/2 579?????????1/6 863??????????-76.8 ″??????ο???????òο??????????????????????????????????????С?60×10-5ms-2??????????????25×10-5ms-2?????????????-325.9 ??389.1 m??

关 键 词:月球大地水准面  参考三轴水准椭球  月球重力场  月球地形  基准

A NEW SELENOID MODEL AND REFERENCE TRIAXIAL LEVEL ELLIPSOID
Feng Hai;Li Jiancheng;Li Dawei;Liu Zhiyong. A NEW SELENOID MODEL AND REFERENCE TRIAXIAL LEVEL ELLIPSOID[J]. Journal of Geodesy and Geodynamics, 2013, 33(4): 133-136
Authors:Feng Hai  Li Jiancheng  Li Dawei  Liu Zhiyong
Affiliation:Feng Hai;Li Jiancheng;Li Dawei;Liu Zhiyong;School of Geodesy and Geomatics,Wuhan University;Beijing Institute of Astronautical Systems Engineering;
Abstract:??A new selenoid (lunar geoid) is derived using the lunar gravity model CEGM02 and topography model LRO_LTM02, which approximates the physical surface as closely as possible. The estimated gravity potential value of this selenoid is 2 822 327.8±16.2 m??2/s??2, denoted as ??W??0?? in usual. A triaxial level ellipsoid whose surface gravity potential equals ??W0?? above is calculated and used as a reference ellipsoid, and its semi??major axis, polar flattening, equator flattening and longitude of semi??major axis are 1 737 462 m, 1/2 579, 1/6 863 and -76.8 ″, respectively. Based on this reference ellipsoid, the gravity decreases about 60×10-5ms-2 from the equator to the poles, while the variation along the equator is about 25×10-5ms-2. The selenoid undulations are in the range of -325.9 m to 389.1 m.
Keywords:selenoid  reference triaxial level ellipsoid  lunar gravity  lunar topography  reference
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