Tohoku {psd} | R Documentation |
Observations of teleseismic strains from the 2011 Tohoku earthquake.
Description
The M_w 9
Tohoku earthquake happened on March 11, 2011. The seismic
waves were recorded at stations across the globe, including by borehole strainmeters
in the Network of the Americas (NOTA), which was previously
known as the Plate Boundary Observatory (PBO) network.
Format
A dataframe with 16000 observations on the following 15 variables.
Dts
The original datetime string, in UTC.
areal
Areal strains
areal.tide
Tidal correction to the areal strains.
areal.baro
Barometric correction to the areal strains.
gamma1
Engineering differential extensional strain:
\gamma_1
gamma1.tide
Tidal correction for the
\gamma_1
strains.gamma1.baro
Barometric pressure correction to the
\gamma_1
strains.gamma2
Engineering shear strain:
\gamma_2
.
gamma2.tide
Tidal correction for the
\gamma_2
strains.gamma2.baro
Barometric pressure correction to the
\gamma_2
strains.pressure.atm
Atmospheric pressure.
pressure.pore
Pore-fluid pressure.
Dt
The
Dts
information converted to POSIX datetime.Origin.secs
The number of seconds relative to the earthquake-origin time.
epoch
Classification based on predicted P-wave arrival: preseismic or seismic.
and 2 attributes:
units
A list of strings regarding the units of various physical quantities given here.
iasp
A list of source and station characteristics, including the the origin time, predicted traveltimes for P and S waves, and the geodetic information used in the traveltime calculation.
Details
These data are for station B084, which is located approximately 8500 km away from the epicenter. Because this distance is large, the seismic waves didn't arrive at this station for more than 700 seconds after the origin time. So there is a record of pre-seismic noise included, the timeseries extends 6784 seconds prior to the origin time, and 9215 seconds after.
The data are classified with the "epoch"
variable, which separates
the series into pre-seismic and seismic data; this is defined relative
to the predicted P-wave arrival time from a traveltime model.
The original dataset contained NA
values, which were imputed
using zoo::na.locf
, which fills NA
with the last previous observation.
Source
High frequency strain data archive:
http://borehole.unavco.org/bsm/earthquakes/NeartheEastCoastofHonshuJapan_20110311/
References
USGS summary page:
https://earthquake.usgs.gov/earthquakes/eventpage/official20110311054624120_30/executive
See Also
TauP.R
for an R-implementation of the traveltime calculations
Examples
data(Tohoku)
str(Tohoku)