The California CORS Program
Current State of CORS in California
History of CORS in California
Southern California Integrated GPS Network (SCIGN)
Deformation in California
PPT Slide
Subsidence in California
California also relies on other technologies to monitor crustal motion, but these also depend in some way on CORS. In this example, large areas in the Los Angeles and Orange Counties becomes inflated in April which is consistent with water table measurements and the end of the rainy season. The spatial pattern of the amplitude of the annual signal (solid yellow contours in mm) derived from SCIGN sites is consistent with the shape of the interferometric SAR fringes (black/white image). Each fringe represents about 28 mm of motion in the line of sight to the satellite. Reference: Watson et al., Journal of Geophysical Research, in press, 2002.
Scripps Orbit and Permanent Array Center (http://sopac.ucsd.edu)
SOPAC Archive and RDBMS
SCOUT: SOPAC Coordinates Update Tool (http://sopac.ucsd.edu/cgi-bin/SCOUT.cgi)
UNAVCO GPS Seamless Archive: Map of GPS Data - Western U.S.
History of the CSRC
NGS and CSRC Partnership
CSRC Master Plan
CSRC 2001 Projects Funded by NGS
Some Real-Time CORS Applications
Dam Deformation: Diamond Valley Lake
More Real-Time GPS Networks
Southern California Real-Time GPS Network
Present/Future of CORS in California
Plate Boundary Observatory (PBO)
PBO San Andreas plan
Email: Richard.Snay@noaa.gov
Home Page: http://www.ngs.noaa.gov/