Amplitude Pattern Effects on NORSAR P-wave Detectability

Abstract

A detailed mapping of NORSAR P-wave amplitude anomalies as a function of the array's beam locations has been performed. For several regions there is as much as 20 dB amplitude variations across the array. There is, however, usually less than 0.3 dB to gain in signal-to-noise ratio by excluding one or more of the NORSAR subarrays. Moreover, one will have to use very small regions, i.e., one set of weights for each of the Detection Processor beams. This because the amplitude pattern, although stable for events coming in on the same beam, may change very drastically from one beam location to the nearest one.

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Document Details

Document Type
Technical Report
Publication Date
Nov 20, 1974
Accession Number
ADA002496

Entities

People

  • E. S. Husebye
  • K. A. Berteussen

Organizations

  • Royal Norwegian Council for Scientific and Industrial Research

Tags

Communities of Interest

  • Materials and Manufacturing Processes
  • Sensors

DTIC Thesaurus Topics

  • Atlantic Ocean
  • Beam Forming
  • Central America
  • Data Analysis
  • Data Processing
  • Detection
  • Detectors
  • Islands
  • Kurile Islands
  • Models
  • North America
  • North Atlantic Ocean
  • Oceans
  • Pacific Ocean
  • Ridges
  • Seismic Arrays
  • Signal Processing

Fields of Study

  • Physics

Readers

  • Phased Array Antenna Design.
  • Seismology