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...
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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 |
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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.
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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 |
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