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Chunlong Huang, Kunde Yang, Hui Li and Yukun Zhang
The flow noise of a sonar platform is one of the main background interferences for sonar applications. This paper focuses on the flow noise of an axisymmetric body in a complex oceanic environment. Under the condition of a constant stream velocity which ...
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Xinguang Wang, Le Wang and Shengmei Zhao
In this paper, we use two methods to research the propagation characteristics of a Hypergeometric-Gaussian (HyGG) vortex beam under oceanic turbulence. One is numerical calculation based on the Rytov approximation theory, where the theoretical detection ...
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Rodrigo Duran, Lucy Romeo, Jonathan Whiting, Jason Vielma, Kelly Rose, Amoret Bunn and Jennifer Bauer
The Department of Energy?s (DOE?s) National Energy Technology Laboratory?s (NETL?s) Blowout and Spill Occurrence Model (BLOSOM), and the National Oceanic and Atmospheric Administration?s (NOAA?s) General NOAA Operational Modeling Environment (GNOME) are ...
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Rodrigo Duran, Lucy Romeo, Jonathan Whiting, Jason Vielma, Kelly Rose, Amoret Bunn and Jennifer Bauer
The Department of Energy’s (DOE’s) National Energy Technology Laboratory’s (NETL’s) Blowout and Spill Occurrence Model (BLOSOM), and the National Oceanic and Atmospheric Administration’s (NOAA’s) General NOAA Operation...
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Rodrigo Duran, Lucy Romeo, Jonathan Whiting, Jason Vielma, Kelly Rose, Amoret Bunn and Jennifer Bauer
The Department of Energy’s (DOE’s) National Energy Technology Laboratory’s (NETL’s) Blowout and Spill Occurrence Model (BLOSOM), and the National Oceanic and Atmospheric Administration’s (NOAA’s) General NOAA Operation...
ver más
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Hans Niemeyer
Pág. 163 - 181
RESUMEN. El complejo Igneo-Sedimentario del Cordon de Lila, de probable edad ordovicica, esta formado por 3.000 m de lavas y volcanoclastitas basicas, intermedias y acidas con intercalaciones de limolitas y grauwacas turbiditicas. Las lavas presentan un ...
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Hans Niemeyer
Pág. 163 - 181
RESUMEN. El complejo Igneo-Sedimentario del Cordon de Lila, de probable edad ordovicica, esta formado por 3.000 m de lavas y volcanoclastitas basicas, intermedias y acidas con intercalaciones de limolitas y grauwacas turbiditicas. Las lavas presentan un ...
ver más
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