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Global climatology of 13 underwater acoustic parameters derived from WOA-2023 (NCEI Accession 0290599)
Acoustics is most effective in undersea detection, localization, and communication. However, there is no global climatology of underwater acoustic parameters. A multiple gradient method is used to analyze the sound speed profile, which is calculated from temperature and salinity profiles using the Thermodynamic Equation of Seawater-2010 (TEOS-10) to get the sonic layer depth (SLD), deep sound channel (DSC) axis depth, and second sound channel (SSC) axis depth from the gridded (0.25 degree, 1 degree, 5 degree) temperature and salinity fields of the National Centers for Environmental Information (NCEI) world ocean atlas 2023. With the given (SLD, DSC axis depth, SSC axis depth), the other acoustic parameters are calculated such as sound speed at the surface, sound speed at the SLD, sound speed at the DSC axis, sound speed at the SSC axis, in-layer gradient, below-layer gradient, surface duct cut-off frequency, deep sound channel strength, critical depth of the DSC, depth excess, and second sound channel strength. Data are in NetCDF.
Complete Metadata
| describedByType | application/octet-steam |
|---|---|
| identifier | gov.noaa.nodc:0290599 |
| issued | 2024-04-01T00:00:00.000+00:00 |
| landingPage | https://www.ncei.noaa.gov/contact |
| language | [] |
| references |
[ "https://doi.org/10.1175/2010jtecho742.1", "https://doi.org/10.1007/s10872-011-0019-2", "https://doi.org/10.1175/2010jtecho804.1", "https://doi.org/10.4031/002533207787442178", "https://doi.org/10.1038/s41597-024-04074-6", "https://doi.org/10.1038/s41597-023-02308-7" ] |
| rights | otherRestrictions |
| spatial | 180.0,-90.0,-180.0,90.0 |
| temporal | 1900-01-01T00:00:00+00:00/2023-12-31T00:00:00+00:00 |
