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- W2285492819 abstract "The possibility of improving the estimation of the bottom topography of the Earth’s oceans using gravity data is investigated in two extended test areas. The first area is located in the Mediterranean Sea southwest of the island of Gavdos, Greece and bounded by 33° ≤ o ≤c 35° and 15 ° ≤ λ 25°. The other one is across the Mid Atlantic Ridge bounded by 40° ≤ o ≤ 50° and 330° ≤ λ ≤ 340°. The integrated inversion method of gravity data proposed by Knudsen is used in an attempt to improve our knowledge of the ocean bathyrnetry and its gravity response. The KMS99 satellite altimetry-derived global marine gravity field is used with a-priori statistical characteristics of depths in a least squares collocation procedure to produce new depths. Two different global bathymetry models, namely JGP95E and Sandwell and Smith V9, are used to derive the depth apriori statistical information and to test how the gravity data can improve the depth estimation. Two- and threelayer models are used to represent the Earth’s structure. The improvement in the estimation of the bottom topography is investigated through an RTM reduction of shipbome gravity data and ERS l-GM satellite altimetry SSHs. Throughout this study, the EGM96 geopotential model complete to degree and order 360 is used as a reference field to model the low frequency part of the gravity field spectrum." @default.
- W2285492819 created "2016-06-24" @default.
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- W2285492819 date "2002-01-01" @default.
- W2285492819 modified "2023-09-25" @default.
- W2285492819 title "Improving the Estimation of Bottom Ocean Topography with Altimetry Derived Gravity Data Using the Integrated Inverse Method" @default.
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- W2285492819 doi "https://doi.org/10.1007/978-3-662-04709-5_89" @default.
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