The Analytical and Quick Computation Method of Disturbing Gravity in Global and Local Ocean Area
In order to solve the problem of deriving the disturbing gravity from satellite altimetry data, the analytical formula of disturbing gravity computed from geoid and vertical deflection are derived. The analytical formula can be used to get global ocean disturbing gravity by using altimetry data. Con...
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doaj-45fbcec4ad6b47168481cce1b8ef74b62020-11-25T00:55:39ZzhoSurveying and Mapping PressActa Geodaetica et Cartographica Sinica1001-15951001-15952015-08-0144882783210.11947/j.AGCS.2015.2014048220150801The Analytical and Quick Computation Method of Disturbing Gravity in Global and Local Ocean AreaZHAI Zhenhe0SUN Zhongmiao1WANG Xingtao2Institute of Geospatial Information, Information Engineering University, Zhengzhou 450052, China;Xi'an Institute of Surveying and Mapping, Xi'an 710054, ChinaXi'an Institute of Surveying and Mapping, Xi'an 710054, ChinaIn order to solve the problem of deriving the disturbing gravity from satellite altimetry data, the analytical formula of disturbing gravity computed from geoid and vertical deflection are derived. The analytical formula can be used to get global ocean disturbing gravity by using altimetry data. Considering the existing achievements, the two improved quick computation methods which are respectively according to the global and local area are also get based on the one dimensional FFT algorithm. The quick computation methods can get the same results as the analytical computation and improve the computation speed of 20 times. The precise, quick computation methods can avoid the problem of aliasing and edge effects and have the flexible application. The 2.5' resolution of geoid and vertical deflection derived from EGM2008 model are used to compute the global and local ocean disturbing gravity. The results show that the difference between two method is about 0.8×10<sup>-5</sup> m/s<sup>2</sup>, so the disturbing gravity respectively derived from geoid and vertical deflection are consistent. Considering the actual situation, the disturbing gravity derived from vertical deflection still has some advantages.http://html.rhhz.net/CHXB/html/2015-8-827.htmgeodesydisturbing gravitygeoidvertical deflectionquick algorithm |
collection |
DOAJ |
language |
zho |
format |
Article |
sources |
DOAJ |
author |
ZHAI Zhenhe SUN Zhongmiao WANG Xingtao |
spellingShingle |
ZHAI Zhenhe SUN Zhongmiao WANG Xingtao The Analytical and Quick Computation Method of Disturbing Gravity in Global and Local Ocean Area Acta Geodaetica et Cartographica Sinica geodesy disturbing gravity geoid vertical deflection quick algorithm |
author_facet |
ZHAI Zhenhe SUN Zhongmiao WANG Xingtao |
author_sort |
ZHAI Zhenhe |
title |
The Analytical and Quick Computation Method of Disturbing Gravity in Global and Local Ocean Area |
title_short |
The Analytical and Quick Computation Method of Disturbing Gravity in Global and Local Ocean Area |
title_full |
The Analytical and Quick Computation Method of Disturbing Gravity in Global and Local Ocean Area |
title_fullStr |
The Analytical and Quick Computation Method of Disturbing Gravity in Global and Local Ocean Area |
title_full_unstemmed |
The Analytical and Quick Computation Method of Disturbing Gravity in Global and Local Ocean Area |
title_sort |
analytical and quick computation method of disturbing gravity in global and local ocean area |
publisher |
Surveying and Mapping Press |
series |
Acta Geodaetica et Cartographica Sinica |
issn |
1001-1595 1001-1595 |
publishDate |
2015-08-01 |
description |
In order to solve the problem of deriving the disturbing gravity from satellite altimetry data, the analytical formula of disturbing gravity computed from geoid and vertical deflection are derived. The analytical formula can be used to get global ocean disturbing gravity by using altimetry data. Considering the existing achievements, the two improved quick computation methods which are respectively according to the global and local area are also get based on the one dimensional FFT algorithm. The quick computation methods can get the same results as the analytical computation and improve the computation speed of 20 times. The precise, quick computation methods can avoid the problem of aliasing and edge effects and have the flexible application. The 2.5' resolution of geoid and vertical deflection derived from EGM2008 model are used to compute the global and local ocean disturbing gravity. The results show that the difference between two method is about 0.8×10<sup>-5</sup> m/s<sup>2</sup>, so the disturbing gravity respectively derived from geoid and vertical deflection are consistent. Considering the actual situation, the disturbing gravity derived from vertical deflection still has some advantages. |
topic |
geodesy disturbing gravity geoid vertical deflection quick algorithm |
url |
http://html.rhhz.net/CHXB/html/2015-8-827.htm |
work_keys_str_mv |
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