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Description
A user of our seismic data notified us about the following issue, so opening this as it might be useful for others
copying here the user request, and will add some initial info as a first comment
Dear station operator,
I am a seismology researcher in China. I recently processed LHZ data from the NZ network in New Zealand for the period 2008-2012 and found that the waveform records from several stations had polarity flips. The waveform data and instrument response files we used were downloaded from IRIS.
In the measurement of the relative traveltime of the 10 mHz surface wave, it is found that all the measured values of the problem station have a half-period (50 s) deviation for several years. Since our measurement method is based on a cross-correlation technique, it is presumed that the cause is flipped polarity of the waveform recording. Afterwards, we used the P wave of the teleseismic (Wenchuan M7.9 earthquake in China on May 12, 2008, and the Tokyo M9.1 earthquake in Japan on March 11, 2011) to conduct a test. Compared with other nearby normal stations (IU SNZO, NZ RPZ), the seismic records of station NZ BKZ on the island of New Zealand have opposite polarities. For details, please refer to the attachment.
I recently plan to publish an article about station clock error and polarity reversal, and I hope the station operator can tell me the reason for the polarity reversal of the waveform record of this station. I will thank you in the acknowledgments of the article.
Earthquakes and station locations picked for this example
The first arrival P waves recorded by the three stations, raw data is unprocessed except for filtering (0.01Hz-0.02Hz). The record in the middle shows a clear polarity reversal