A continuous GPS array is a very useful tool for monitoring and modeling crustal activity. GPS observation has revealed various unknown aspects of tectonic deformation in Japan and other locations. Quasi-real time data acquisition and dense spatial coverage enable incorporation of GPS data into simulation models for crustal activity forecast, which is similar to data assimilation in weather forecast. For that purpose, it is important to develop new techniques of geodetic inversion and time series analysis
Geodetic measurements obtained with the Global Positioning System (GPS) are increasingly more widely...
Continuously-operating networks of GPS receivers (CGPS) are not capable of determiningthe characteri...
The Geographical Survey Institute published a new geodetic datum (the Japanese Geodetic Datum 2000, ...
Data assimilation is indispensable to numerical simulations of crustal activities if one intends to ...
For the monitoring of crustal movements and the long-term earthquake prediction, GPSobservation syst...
The calculation of invariant deformation parame-ters, entering in the constitutional equations of cr...
The calculation of invariant deformation parame-ters, entering in the constitutional equations of cr...
The calculation of invariant deformation parame-ters, entering in the constitutional equations of cr...
Data assimilation is indispensable to numerical simulations of crustal activities if one intends to ...
The calculation of invariant deformation parame-ters, entering in the constitutional equations of cr...
The calculation of invariant deformation parame-ters, entering in the constitutional equations of cr...
The calculation of invariant deformation parame-ters, entering in the constitutional equations of cr...
Since 1994, crustal deformation in northern Nagano Prefecture, including the Hida mountain range, ha...
Monitoring of crustal deformation provides essential information for seismology and volcanology. For...
Geographical Survey Institute (GSI) established GPS permanent observation station network GEONET cov...
Geodetic measurements obtained with the Global Positioning System (GPS) are increasingly more widely...
Continuously-operating networks of GPS receivers (CGPS) are not capable of determiningthe characteri...
The Geographical Survey Institute published a new geodetic datum (the Japanese Geodetic Datum 2000, ...
Data assimilation is indispensable to numerical simulations of crustal activities if one intends to ...
For the monitoring of crustal movements and the long-term earthquake prediction, GPSobservation syst...
The calculation of invariant deformation parame-ters, entering in the constitutional equations of cr...
The calculation of invariant deformation parame-ters, entering in the constitutional equations of cr...
The calculation of invariant deformation parame-ters, entering in the constitutional equations of cr...
Data assimilation is indispensable to numerical simulations of crustal activities if one intends to ...
The calculation of invariant deformation parame-ters, entering in the constitutional equations of cr...
The calculation of invariant deformation parame-ters, entering in the constitutional equations of cr...
The calculation of invariant deformation parame-ters, entering in the constitutional equations of cr...
Since 1994, crustal deformation in northern Nagano Prefecture, including the Hida mountain range, ha...
Monitoring of crustal deformation provides essential information for seismology and volcanology. For...
Geographical Survey Institute (GSI) established GPS permanent observation station network GEONET cov...
Geodetic measurements obtained with the Global Positioning System (GPS) are increasingly more widely...
Continuously-operating networks of GPS receivers (CGPS) are not capable of determiningthe characteri...
The Geographical Survey Institute published a new geodetic datum (the Japanese Geodetic Datum 2000, ...