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Station Overview

Overview Location not available
Picture Gallery details...
Network CH
Station Code SARE
Station Description Arbon, Evangelische Kirche, TG
Latitude (WGS84) 47.51488
Longitude (WGS84) 9.43023
Station altitude (CH1903) 414.0
running from 2014-12-19
...until now
Sensor Types Accelerometer
Geological Unit Silty gravel, sand, silt, partly blocks (moraine)
Site Morphology Class T1
T1: flat; T2: slope; T3: ridge and T4: steep ridge;
following Pessina and Fiorini (2014) A GIS procedure for fast topographic characterization of seismic recording stations, Soil Dynamics and Earthquake Engineering, 63, p248-258
Site Morphology Description Valley edge
Ground type EC8 B
Ground type SIA C
Basin Information Lake Constance basin
Reference
Resonance Frequency (Hz) .86
Uncertainty Factor -
Vs 30 (m/s) 374
Location Map


Federal Office of Topograpy: National Map 1:25‘000
Topography Map


Federal Office of Topograpy: DHM25: Digital Height Model 1:25000
Geology Map

Federal Office of Topograpy: Geological map of Switzerland 1:500‘000

Sensor locations

Location Code (none)
Opening Date 19-12-2014
End Date -
Housing Class Free field
Housing Description SSMNet large pot
sensor depth below station 1.0 m
Distance to Building (m) -

Current Instrumentation

Location code (none)
On date 13-01-2022 12:30:00
Off date -
Sensor model EpiSensor ES-T
Sensor manufacturer Kinemetrics
Digitizer model Centaur
Digitizer manufacturer Nanometrics
Channels HGE , HGN , HGZ
Stream Noise (last week) HGE , HGN , HGZ
Location code (none)
On date 09-10-2015 09:48:00
Off date 2022-01-13 12:30:00
Sensor model EpiSensor ES-T
Sensor manufacturer Kinemetrics
Digitizer model Centaur
Digitizer manufacturer Nanometrics
Channels HGE , HGN , HGZ
Location code (none)
On date 19-12-2014 15:00:00
Off date 2015-10-09 09:48:00
Sensor model EpiSensor ES-T
Sensor manufacturer Kinemetrics
Digitizer model Centaur
Digitizer manufacturer Nanometrics
Channels HGE , HGN , HGZ

Site Characterization

channel group CH.SARE..HG
Empirical Amplification not available

Obtained from spectral modeling of small earthquakes with constant update.

  • Top: Fourier amplification with elastic (dashed line) and anelastic (solid line) amplification functions;
  • Centre: 5% damped response spectra amplification (anelastic);
  • Bottom: Number of recordings used.

See Edwards et al. (2013), Determination of Site Amplification from Regional Seismicity: Application to the Swiss National Seismic Networks. Seismological Research Letters, 84(4), 611–621.

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Authoritative Site Characterization Analysis details...
measurements nearby list...