System for near real-time crustal deformation monitoring

• US 4,170,776 A
• Filed: 12/21/1977
• Issued: 10/09/1979
• Est. Priority Date: 12/21/1977
• Status: Expired due to Term

• Current Assignee: Frosch Robert A Administrator of The National Aeronautics and Space Administration With Respect To An Invention of, Peter F. Macdoran
• Original Assignee: Frosch Robert A Administrator of The National Aeronautics and Space Administration With Respect To An Invention of, Peter F. Macdoran
• Inventors: Frosch, Robert A. Administrator of the National Aeronautics and Space Administration, with respect to an invention of, MacDoran, Peter F.
• Primary Examiner(s): Blum, Theodore M.
• Application Number:
  US05/863,024
• Time in Patent Office: 657 Days
• Field of Search: 343/112 R, 343/112 D, 343/100 ME
• US Class Current: 342/458
• CPC Class Codes: G01V 1/01 Measuring or predicting earthquakes
• CPC Class Codes: H04B 7/00 Radio transmission systems, i.e. using radiation field H04B10/00, H04B15/00 take precedence

Abstract

A system for use in detecting earth crustal deformation using an RF interferometer technique for such purposes as earthquake predictive research and eventual operational predictions. A lunar based RF transmission or transmissions from earth orbiting satellites are received at two locations on Earth, and a precise time dependent phase measurement is made of the RF signal as received at the two locations to determine two or three spatial parameters of the antenna relative positions. The received data are precisely time tagged and land-line routed to a central station for real-time phase comparison and analysis. By monitoring the antenna relative positions over an extended period of months or years, crustal deformation of the earth can be detected.

Claims

1. In a system for monitoring crustal deformation using long-baseline radio interferometry, the method of receiving at two independent stations a radio signal of limited spectrum from a source at a known location is space, maintaining synchronized clocks at said station, time tagging the radio signal received at each station, transmitting the time-tagged radio signal received at each station to a convenient location for cross correlation using communication channels having a bandwidth sufficient for said limited spectrum, adjusting the transmission delay of one radio signal relative to the other to synchronize time tags prior to cross correlation, and estimating the interferometer delay or delay rate in order to derive baselines for near real-time crustal deformation monitoring.

2. The method of claim 1 wherein said source is an artificial narrow band radio signal, and said communication channels are comprised of telephone lines.

3. The method of claim 2 wherein said source is an S-band transmitter on the moon.

4. The method of claim 2 wherein said source is an L-band signal from a global positioning system satellite.

5. The method defined by claim 4 including rapid simultaneous estimating of baseline using several global positioning system satellites in order to significantly reduce the stability requirements of the time and frequency systems.

6. In a monitoring system, using a pair of antennas at separated stations on earth for receiving a radio signal of limited spectrum from an artificial source at a known location in space and a pair of synchronized clocks, one clock at each station for time tagging the radio signal received, the method of transmitting the time tagged radio signals from the stations to a third station, adjusting the transmission delay time of one radio signal relative to the other to synchronize time tags, and cross correlating the signals thus time synchronized for obtaining fringe frequency observations to be used in near real-time crustal deformation monitoring.