@prefix skos: <http://www.w3.org/2004/02/skos/core#> .
@prefix ns0: <http://gcmd.gsfc.nasa.gov/kms#> .

<https://gcmd.earthdata.nasa.gov/kms/concept/b56d53ea-511f-486f-b917-26000794ab51>
  skos:prefLabel "Acoustic Sounders"@en ;
  a skos:Concept ;
  skos:narrower <https://gcmd.earthdata.nasa.gov/kms/concept/5c455392-a50e-44da-9da6-f0038cd28acb> .

<https://gcmd.earthdata.nasa.gov/kms/concept/5c455392-a50e-44da-9da6-f0038cd28acb>
  ns0:altLabel [ ] ;
  skos:definition """The SOund SUrveillance System, or SOSUS, is a fixed component of the
U.S. Navy's Integrated Undersea Surveillance Systems(IUSS) network
used for deep ocean surveillance during the Cold War. Installation
of SOSUS was begun in the mid 1950s by the U.S. Navy for use in
antisubmarine warfare. SOSUS consists of bottom mounted hydrophone
arrays connected by undersea communication cables to facilities on
shore. The individual arrays are installed primarily on continental
slopes and seamounts at locations optimized for undistorted long range
acoustic propagation. The combination of location within the oceanic
sound channel and the sensitivity of large-aperture arrays allows the
system to detect radiated acoustic power of less than a watt at ranges
of several hundred kilometers. In October, 1990, the Navy granted
approval to NOAA/PMEL to access the SOSUS arrays in the North Pacific
to assess their value in ocean environmental monitoring,as part of the
U.S. government's dual-use initiative.

The data collection systems developed by NOAA's VENTS Program have
been in place since August 29, 1991. Acoustic signals from the north
Pacific Ocean are monitored and recorded at the Newport, Oregon facility
of NOAA/PMEL. This is the primary tool for both continuous monitoring of
low-level seismicity around the northeast Pacific Ocean and real-time
detection of volcanic activity along the northeast Pacific spreading
centers in support of the VENTS research program in ocean hydrothermal
systems. Real-time ridge crest monitoring potentially permits the timely
on-site investigation of hydrothermal and magmatic emissions.

Data acquisition is accomplished by combining portions of the Navy's
processing facilities with NOAA-designed systems installed at the U.S.
Naval Ocean Processing Facility (NOPF) at Whidbey Island, Washington.
Analog outputs from each hydrophone element are available either through
direct cabling or remote data linkage. Navy systems perform adaptive beam
forming on digitized hydrophone signals, with the outputs converted back to
analog electrical signals. These analog hydrophone and beam-former outputs
are accessed by the NOAA-supplied systems, where the signals are low-pass
filtered, digitized, and temporarily buffered on hard disk. The digital
data are provided to a wide-area network (WAN) based on Network File System
(NFS) protocol, linking (by encrypted, dedicated telephone line) the
acquisition computer to an analysis system located at NOAA laboratories in
Newport, Oregon.

For more information on U.S. Navy SOund SUrveillance System (SOSUS)see:
"http://newport.pmel.noaa.gov/geophysics/sosus_system.html"

Address inquiries to:
Chris Fox - Principal Investigator
NOAA/PMEL
OSU Hatfield Marine Science Center
2115 S.E. OSU Drive
Newport, Oregon 97365 USA

VOICE: (541) 867-0276
FAX: (541) 867-0356
Email: fox&#64pmel.noaa.gov"""@en ;
  skos:prefLabel "SOSUS"@en ;
  skos:inScheme <https://gcmd.earthdata.nasa.gov/kms/concepts/concept_scheme/instruments> ;
  skos:broader <https://gcmd.earthdata.nasa.gov/kms/concept/b56d53ea-511f-486f-b917-26000794ab51> ;
  a skos:Concept .

