English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/53038
logo share SHARE logo core CORE   Add this article to your Mendeley library MendeleyBASE

Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL | DATACITE
Exportar a otros formatos:


Application of acoustic full waveform inversion to retrieve high-resolution temperature and salinity profiles from synthetic seismic data

AuthorsKormann, Jean ; Biescas, Berta ; Korta, N. ; de la Puente, Josep ; Sallarès, Valentí
Issue DateNov-2011
PublisherAmerican Geophysical Union
CitationJournal of Geophysical Research: Oceans 116(C11): C11039 (2011)
AbstractRecent works show that multichannel seismic (MCS) systems are able to provide detailed information on the oceans' fine structure. The aim of this paper is to analyze whether 1-D full waveform inversion algorithms are suitable to recover the extremely weak acoustic impedance contrasts associated to the oceans' fine structure, as well as their potential to image meso-scale objects such as meddies. We limited our analysis to synthetic, noise-free data, in order to identify some methodological issues related to this approach under idealistic conditions (e.g., 1-D wave propagation, noise-free data, known source wavelet). We first discuss the influence of the starting model in the context of the multi-scale strategy that we have implemented. Then we show that it is possible to retrieve not only sound speed but also salinity and temperature contrasts within reasonable bounds from the seismic data using Neural Network relationships trained with regional oceanographic data sets. Potentially, the vertical resolution of the obtained models, which depends on the maximum frequency inverted, is of the order of 5–10 m, whereas the root mean square error of the inverted properties is shown to be ∼0.5 m/s for sound speed, 0.1°C for temperature, and 0.06 for salinity. To conclude this study, we have inverted synthetic data simulated along an oceanographic transect acquired during the EU-funded Geophysical Oceanography (GO) project. The results demonstrate the applicability of the method for synthetic data, as well as its potential to define oceanographic features along 2-D transects at full ocean depth with excellent lateral resolution
Description14 pages, 14 figures
Publisher version (URL)https://doi.org/10.1029/2011JC007216
Appears in Collections:(UTM) Artículos
(ICM) Artículos
Files in This Item:
File Description SizeFormat 
Kormann_et_al_2011.pdf2,95 MBAdobe PDFThumbnail
Show full item record
Review this work

Related articles:

WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.