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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Main Authors: ZHAI Zhenhe, SUN Zhongmiao, WANG Xingtao
Format: Article
Language:zho
Published: Surveying and Mapping Press 2015-08-01
Series:Acta Geodaetica et Cartographica Sinica
Subjects:
Online Access:http://html.rhhz.net/CHXB/html/2015-8-827.htm
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spelling 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&#215;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&#215;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
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