Global marine gravity anomalies from Seasat,Geosat,ERS-1,TOPEX/POSEIDON satellite altimetry

碩士 === 國立交通大學 === 土木工程學系 === 85 === Global marine gravity anomalies at a 2'x2'grid have been determined fromSe asat﹑Geosat﹑ERS-1 and TOPEX/POSEIDON altimeter data. The inverse VeningMeine sz formula with an 1D FFT method was used to compute...

Full description

Bibliographic Details
Main Authors: Kao, Eu-Chi, 高豫
Other Authors: Cheinway Hwang
Format: Others
Language:zh-TW
Online Access:http://ndltd.ncl.edu.tw/handle/65379738807251509118
id ndltd-TW-085NCTU0015040
record_format oai_dc
spelling ndltd-TW-085NCTU00150402015-10-13T17:59:37Z http://ndltd.ncl.edu.tw/handle/65379738807251509118 Global marine gravity anomalies from Seasat,Geosat,ERS-1,TOPEX/POSEIDON satellite altimetry 結合Seasat,Geosat,ERS-1和TOPEX/POSEIDON衛星測高資料計算全球海洋重力異常 Kao, Eu-Chi 高豫 碩士 國立交通大學 土木工程學系 85 Global marine gravity anomalies at a 2'x2'grid have been determined fromSe asat﹑Geosat﹑ERS-1 and TOPEX/POSEIDON altimeter data. The inverse VeningMeine sz formula with an 1D FFT method was used to compute gravity anomaliesfrom gri dded north-south and west-east geoid gradients, in a remove-restoreprocedure w ith the EGM96 gravity model as the reference field. The data coverthe area 0° to 360° in longitude and 72°S to 72°N in latitude. In the 12 test areas where ship gravity and satellite-derived gravitywere compared, rms agreements of 6-10 mgals were obtained and the gravityanomalies derived in this work are 0.5 mgal on average better than thosederived by Sandwell and Smith (1997). Th e gravity anomalies are locatedat an ftp site (ftp://gps.cv.nctu.edu.tw) where an application program isavailable for extracting data in a subarea. Cheinway Hwang 黃金維 --- 學位論文 ; thesis 119 zh-TW
collection NDLTD
language zh-TW
format Others
sources NDLTD
description 碩士 === 國立交通大學 === 土木工程學系 === 85 === Global marine gravity anomalies at a 2'x2'grid have been determined fromSe asat﹑Geosat﹑ERS-1 and TOPEX/POSEIDON altimeter data. The inverse VeningMeine sz formula with an 1D FFT method was used to compute gravity anomaliesfrom gri dded north-south and west-east geoid gradients, in a remove-restoreprocedure w ith the EGM96 gravity model as the reference field. The data coverthe area 0° to 360° in longitude and 72°S to 72°N in latitude. In the 12 test areas where ship gravity and satellite-derived gravitywere compared, rms agreements of 6-10 mgals were obtained and the gravityanomalies derived in this work are 0.5 mgal on average better than thosederived by Sandwell and Smith (1997). Th e gravity anomalies are locatedat an ftp site (ftp://gps.cv.nctu.edu.tw) where an application program isavailable for extracting data in a subarea.
author2 Cheinway Hwang
author_facet Cheinway Hwang
Kao, Eu-Chi
高豫
author Kao, Eu-Chi
高豫
spellingShingle Kao, Eu-Chi
高豫
Global marine gravity anomalies from Seasat,Geosat,ERS-1,TOPEX/POSEIDON satellite altimetry
author_sort Kao, Eu-Chi
title Global marine gravity anomalies from Seasat,Geosat,ERS-1,TOPEX/POSEIDON satellite altimetry
title_short Global marine gravity anomalies from Seasat,Geosat,ERS-1,TOPEX/POSEIDON satellite altimetry
title_full Global marine gravity anomalies from Seasat,Geosat,ERS-1,TOPEX/POSEIDON satellite altimetry
title_fullStr Global marine gravity anomalies from Seasat,Geosat,ERS-1,TOPEX/POSEIDON satellite altimetry
title_full_unstemmed Global marine gravity anomalies from Seasat,Geosat,ERS-1,TOPEX/POSEIDON satellite altimetry
title_sort global marine gravity anomalies from seasat,geosat,ers-1,topex/poseidon satellite altimetry
url http://ndltd.ncl.edu.tw/handle/65379738807251509118
work_keys_str_mv AT kaoeuchi globalmarinegravityanomaliesfromseasatgeosaters1topexposeidonsatellitealtimetry
AT gāoyù globalmarinegravityanomaliesfromseasatgeosaters1topexposeidonsatellitealtimetry
AT kaoeuchi jiéhéseasatgeosaters1hétopexposeidonwèixīngcègāozīliàojìsuànquánqiúhǎiyángzhònglìyìcháng
AT gāoyù jiéhéseasatgeosaters1hétopexposeidonwèixīngcègāozīliàojìsuànquánqiúhǎiyángzhònglìyìcháng
_version_ 1717785800832188416