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)
 


