Simple Responses
Seismic sensor (either seismometers or accelerometers) transfer function can be described in a variety of ways. Many modern sensors have a "flat response" in a certain frequency band, meaning that the number of counts measured can be directly converted to ground movement by dividing by a simple factor, called the gain. The simple response gives this gain, as well as the corner period and damping. From these three values, the a simplified version of the transfer function can be also be calculated as poles and zeros or in other representations.
List of Simple Response Tables, By 2-Letter Network Code
- 3B (Enhanced Geothermal Systems)
- 4B (Enhanced Geothermal Systems)
- 5B (Enhanced Geothermal Systems)
- AZ (ANZA network)
- BG (Enhanced Geothermal Systems, The Geysers)
- BK (Berkeley Digital Seismic Network)
- BP (High Resolution Seismic Network
- CE (Galifornia Geological Survey)
- CI (Caltech)
- GM (USGS Earthquake Science Center)
- GS (US Geological Survey Networks)
- LB
- NC (Northern California Seismic Network)
- NN (Nevada)
- NP (NSMP, National Strong Motion Program)
- PB (Plate Boundary Observatory)
- PG (Diablo Canyon Seismic Network, PG&E)
- SF (San Andreas Fault Observatory at Depth
- SB (UC Santa Barbara Engineering Seismology Network)
- TA (US Array)
- UO
- US (United States National Seismic Network)
- UW
- WR (California Division of Water Resources Seismic Network)