A MEASUREMENT OF OCEAN-BOTTOM SLOPE

The slope of the deep ocean bottom is calculated by measuring the bottom reverberation from active sonar transmissions. Knowledge of this slope is required to localize a target detected by bottom bounce echo-ranging. The method is based on the fact that reverberation has a space-time coherency; that...

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Bibliographische Detailangaben
1. Verfasser:	Newman,Howard S
Format:	Report
Sprache:	eng
Schlagworte:	Acoustic Detection and Detectors DATA PROCESSING DEEP WATER DEPTH INDICATORS DETECTION ECHO RANGING ERRORS GEOMETRY MEASUREMENT Most Project-2 OCEAN BOTTOM OCEANOGRAPHY OSCILLOGRAPHS Physical and Dynamic Oceanography RECORDING SYSTEMS REFLECTION REVERBERATION SIGNALS SURFACE PROPERTIES TABLES(DATA) TARGETS UNDERWATER SOUND VELOCITY
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