The values for P waves () and S waves () for frequencies below 1 Hz reported in Olsen et al. (2018) are in error for two reasons. The first reason is the use of incorrect TJN observations for the 2009 event. The data were retrieved directly from the Korea Institute of Geoscience and Mineral Resources (KIGAM), while an instrument response valid only for TJN data contributed to IRIS since 2013 was used. Data and a compatible instrument response from the Ocean Hemisphere Project Data Management Center (OHPDMC) resolved...
Constraints of Crustal Heterogeneity and Q(f) from Regional (<4 Hz) Wave Propagation for the 2009 North Korea Nuclear Test
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Kim B. Olsen, Michael Begnaud, Scott Phillips, Bo Holm Jacobsen; Constraints of Crustal Heterogeneity and from Regional () Wave Propagation for the 2009 North Korea Nuclear Test. Bulletin of the Seismological Society of America doi: https://doi.org/10.1785/0120200173
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