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![Comparison between the MALMI catalog and the SeisComP low‐quality catalog. (a) Venn diagram showing the detection capability statistics for the two catalogs. (b) Noncumulative frequency‐magnitude distribution of earthquakes in the MALMI and SeisComP low‐quality catalogs. (c) Earthquake magnitude versus time. The red dots denote events in the MALMI catalog, whereas the black dots represent events in the SeisComP low‐quality catalog. Event size is scaled by magnitude. The red solid line and black dashed line show the cumulative number of events (right Y‐axis) over time for the MALMI and SeisComP low‐quality catalogs, respectively. The green star denotes the occurrence of the largest event (ML 4.5 event at UTC: 30 December 2018 T02:56:20) in the monitoring time period. (d) The mean and standard deviation of the location (in both horizontal and depth directions) and origin time differences for the codetected events in the two catalogs. The color version of this figure is available only in the electronic edition.]()
![IT infrastructure for the MSN. Four dedicated servers run SeisComP, Tsunami Observation and Simulation Terminal (TOAST), website services, and the data archive. SeisComP and TOAST retrieve real‐time data from seismic and sea‐level stations (triangles), respectively, through the corresponding networks (circles). Only the seismic data from the MSN are stored permanently. The color version of this figure is available only in the electronic edition.]()
![Overview of real‐time system. (a) Seismic event list in SeisComP, showing the multiple origins associated with one event. (b) Example of automatic picking on AE sensors. The red vertical lines indicate the automatic P arrival. (c) 3D plot with real‐time double‐difference relocations (blue dots) from TB1 (see Fig. 3). The solid lines show the monitoring boreholes. (d) Real‐time magnitude (Mw*) history plot. The color version of this figure is available only in the electronic edition.]()
![scdetect‐cc workflow and its place within the SeisComP workflow. The detector‐k refers to an origin that corresponds to an earthquake, whereas each template comprises a snippet of continuous waveform from a defined channel stream around a particular phase. The color version of this figure is available only in the electronic edition.]()
![Screenshot of the scdetect‐cc module configuration in the SeisComP configuration graphical user interface (GUI) scconfig. The color version of this figure is available only in the electronic edition.]()
![First thumbnail for: Multiscale Seismic Monitoring in the Bedretto Unde...]()
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![SeisComP Data Structure (SDS) report of the DSEBRA data archive (27 September 2021) created with an extended version of the ObsPy module sds_html_report (Megies et al., 2011). The respective background color indicates the status of a station: Stations for which all checks pass without any errors (green), stations with a data latency longer than one hour (yellow) and longer than one day (red), stations with less than 99.5% data or more than 20 data gaps within the last seven days (dark blue), solar power stations with a current voltage lower than 12.1 V (light blue), number of satellites falls below four (orange). The color version of this figure is available only in the electronic edition.]()
![Screenshots of modules of the SeisComP software: (a) origin locator view (scolv), (b) the picker, (c) screenshot of the WebDC3 software, and (d) schema of the routing service. The color version of this figure is available only in the electronic edition.]()
![Screenshots of modules of the SeisComP software: (a) origin locator view (scolv), (b) the picker, (c) screenshot of the WebDC3 software, and (d) schema of the routing service. The color version of this figure is available only in the electronic edition.]()
![Scatter plot of (a) ML1 versus Mw for all SeisComP (SC) earthquakes; (b) ML1 versus Mw for SC earthquakes with focal depth h>40 km; (c) MLNZ20 versus Mw for all SC earthquakes; and (d) MLNZ20 versus Mw for SC earthquakes with h>40 km. Solid line is line of equality. Dotted curve is smooth local regression fit to data. The color version of this figure is available only in the electronic edition.]()
![Spatial distribution of the relative relocated seismic events in the (a) SeisComP high‐quality catalog and (b) MALMI catalog in the Hengill region from 01 December 2018 to 31 December 2018. (a,b) Events are color coded using event depth (relative to the sea level). Event size is scaled with magnitude. The black circles mark the locations of the two geothermal power plants. Six event clusters are identified and highlighted using black rectangulars. (c) Vertical profiles along the south–north direction for each cluster. The black and red circles indicate the events in the MALMI catalog and the SeisComP high‐quality relative relocated catalog, respectively. The color version of this figure is available only in the electronic edition.]()
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Journal Article
SCDetect: A SeisComP Module for Real‐Time Waveform Cross‐Correlation‐Based Earthquake Detection Available to Purchase
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 12 February 2024
Seismological Research Letters (2024) 95 (3): 1961–1975.
... with the extension module scdetect‐cc is an open‐source SeisComP package written in C++. scdetect‐cc can be used to process both archived waveform data (playback mode), and real‐time data. In the real‐time application, waveforms are fetched through one of the SeisComP RecordStream interfaces, and its output (picks...
FIGURES
Image
Comparison between the MALMI catalog and the SeisComP low‐quality catalog. ... Available to Purchase
in MALMI: An Automated Earthquake Detection and Location Workflow Based on Machine Learning and Waveform Migration
> Seismological Research Letters
Published: 11 May 2022
Figure 6. Comparison between the MALMI catalog and the SeisComP low‐quality catalog. (a) Venn diagram showing the detection capability statistics for the two catalogs. (b) Noncumulative frequency‐magnitude distribution of earthquakes in the MALMI and SeisComP low‐quality catalogs. (c) Earthquake
Image
IT infrastructure for the MSN. Four dedicated servers run SeisComP, Tsunami... Available to Purchase
in A First National Seismic Network for the Maltese Islands—The Malta Seismic Network
> Seismological Research Letters
Published: 31 March 2021
Figure 7. IT infrastructure for the MSN. Four dedicated servers run SeisComP, Tsunami Observation and Simulation Terminal (TOAST), website services, and the data archive. SeisComP and TOAST retrieve real‐time data from seismic and sea‐level stations (triangles), respectively, through
Image
Overview of real‐time system. (a) Seismic event list in SeisComP, showing t... Available to Purchase
in Multiscale Seismic Monitoring in the Bedretto Underground Laboratory for Geosciences and Geoenergies (BULGG)
> Seismological Research Letters
Published: 24 July 2024
Figure 5. Overview of real‐time system. (a) Seismic event list in SeisComP, showing the multiple origins associated with one event. (b) Example of automatic picking on AE sensors. The red vertical lines indicate the automatic P arrival. (c) 3D plot with real‐time double‐difference relocations
Image
scdetect‐cc workflow and its place within the SeisComP workflow. The dete... Available to Purchase
in SCDetect: A SeisComP Module for Real‐Time Waveform Cross‐Correlation‐Based Earthquake Detection
> Seismological Research Letters
Published: 12 February 2024
Figure 1. scdetect‐cc workflow and its place within the SeisComP workflow. The detector‐k refers to an origin that corresponds to an earthquake, whereas each template comprises a snippet of continuous waveform from a defined channel stream around a particular phase. The color version
Image
Screenshot of the scdetect‐cc module configuration in the SeisComP config... Available to Purchase
in SCDetect: A SeisComP Module for Real‐Time Waveform Cross‐Correlation‐Based Earthquake Detection
> Seismological Research Letters
Published: 12 February 2024
Figure 2. Screenshot of the scdetect‐cc module configuration in the SeisComP configuration graphical user interface (GUI) scconfig . The color version of this figure is available only in the electronic edition.
Journal Article
Multiscale Seismic Monitoring in the Bedretto Underground Laboratory for Geosciences and Geoenergies (BULGG) Available to Purchase
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 24 July 2024
Seismological Research Letters (2025) 96 (1): 182–191.
...Figure 5. Overview of real‐time system. (a) Seismic event list in SeisComP, showing the multiple origins associated with one event. (b) Example of automatic picking on AE sensors. The red vertical lines indicate the automatic P arrival. (c) 3D plot with real‐time double‐difference relocations...
FIGURES
Image
SeisComP Data Structure (SDS) report of the DSEBRA data archive (27 Septemb... Available to Purchase
in UNIBRA/DSEBRA: The German Seismological Broadband Array and Its Contribution to AlpArray—Deployment and Performance
> Seismological Research Letters
Published: 25 May 2022
Figure 4. SeisComP Data Structure (SDS) report of the DSEBRA data archive (27 September 2021) created with an extended version of the ObsPy module sds_html_report ( Megies et al. , 2011 ). The respective background color indicates the status of a station: Stations for which all checks pass
Image
Screenshots of modules of the SeisComP software: (a) origin locator view (s... Available to Purchase
Published: 24 February 2021
Figure 6. Screenshots of modules of the SeisComP software: (a) origin locator view (scolv), (b) the picker, (c) screenshot of the WebDC3 software, and (d) schema of the routing service. The color version of this figure is available only in the electronic edition.
Image
Screenshots of modules of the SeisComP software: (a) origin locator view (s... Available to Purchase
Published: 24 February 2021
Figure 6. Screenshots of modules of the SeisComP software: (a) origin locator view (scolv), (b) the picker, (c) screenshot of the WebDC3 software, and (d) schema of the routing service. The color version of this figure is available only in the electronic edition.
Image
Scatter plot of (a) M L 1 versus M w for all SeisComP ... Available to Purchase
in A Depth‐Dependent Local Magnitude Scale for New Zealand Earthquakes Consistent with Moment Magnitude
> Bulletin of the Seismological Society of America
Published: 22 December 2020
Figure 10. Scatter plot of (a) M L 1 versus M w for all SeisComP (SC) earthquakes; (b) M L 1 versus M w for SC earthquakes with focal depth h > 40 km ; (c) M LNZ 20 versus M w for all SC earthquakes; and (d) M LNZ
Image
Spatial distribution of the relative relocated seismic events in the (a) Se... Available to Purchase
in MALMI: An Automated Earthquake Detection and Location Workflow Based on Machine Learning and Waveform Migration
> Seismological Research Letters
Published: 11 May 2022
Figure 7. Spatial distribution of the relative relocated seismic events in the (a) SeisComP high‐quality catalog and (b) MALMI catalog in the Hengill region from 01 December 2018 to 31 December 2018. (a,b) Events are color coded using event depth (relative to the sea level). Event size is scaled
Journal Article
Gisola: A High‐Performance Computing Application for Real‐Time Moment Tensor Inversion Available to Purchase
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 22 December 2021
Seismological Research Letters (2022) 93 (2A): 957–966.
... adjustable MT grid search and multiple data resources interconnection to the International Federation of Digital Seismograph Networks Web Services (FDSNWS), the SeedLink protocol, and the SeisComP Data Structure standard. The new software publishes its results in various formats such as QuakeML and SC3ML...
FIGURES
Journal Article
Standardizing Earthquake Magnitudes for the 2022 Revision of the Aotearoa New Zealand National Seismic Hazard Model Available to Purchase
Publisher: Seismological Society of America
Published: 21 December 2023
Bulletin of the Seismological Society of America (2024) 114 (1): 111–136.
... is a variation of local magnitude M L . In New Zealand, M L is systematically larger than M wNZ over a wide magnitude range. Furthermore, the introduction of the earthquake analysis system SeisComP in 2012 caused step changes in the catalog. We address the problems by converting magnitudes using regressions...
FIGURES
Journal Article
Bridging the Seismic Monitoring Gap around Saba, St. Eustatius, and St. Maarten in the Caribbean Netherlands: The NA Network Available to Purchase
Publisher: Seismological Society of America
Published: 23 November 2022
Bulletin of the Seismological Society of America (2023) 113 (1): 143–156.
..., and to contribute data to regional earthquake and tsunami warning monitoring systems. The network currently comprises 11 broadband seismometers that record data processed in real time at KNMI, using SeisComP and a coincidence trigger. Between January 2017 and April 2022, we detected and located 241 earthquakes...
FIGURES
Journal Article
MALMI: An Automated Earthquake Detection and Location Workflow Based on Machine Learning and Waveform Migration Available to Purchase
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 11 May 2022
Seismological Research Letters (2022) 93 (5): 2467–2483.
...Figure 6. Comparison between the MALMI catalog and the SeisComP low‐quality catalog. (a) Venn diagram showing the detection capability statistics for the two catalogs. (b) Noncumulative frequency‐magnitude distribution of earthquakes in the MALMI and SeisComP low‐quality catalogs. (c) Earthquake...
FIGURES
Includes: Supplemental Content
Journal Article
The Modern Swedish National Seismic Network: Two Decades of Intraplate Microseismic Observation Available to Purchase
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 17 March 2021
Seismological Research Letters (2021) 92 (3): 1747–1758.
... Iceland Lowland (SIL) system as the primary system for automatic detection and event definition. In addition, an in‐house system based on migration and stacking is used for automatic detection of small events, and implementations of SeisComP (SC) and Earthworm are used primarily for rapid detection...
FIGURES
Journal Article
The GEOFON Program in 2020 Available to Purchase
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 24 February 2021
Seismological Research Letters (2021) 92 (3): 1610–1622.
...Figure 6. Screenshots of modules of the SeisComP software: (a) origin locator view (scolv), (b) the picker, (c) screenshot of the WebDC3 software, and (d) schema of the routing service. The color version of this figure is available only in the electronic edition. ...
FIGURES
Journal Article
UiB‐NORSAR EIDA Node: Integration of Seismological Data in Norway Available to Purchase
Journal: Seismological Research Letters
Publisher: Seismological Society of America
Published: 06 January 2021
Seismological Research Letters (2021) 92 (3): 1491–1500.
... that are added in near‐real time, the backfilling of archives from permanent networks and providing access to temporary deployments. The software behind the EIDA node is SeisComP, and access to data and metadata is through standard International Federation of Digital Seismograph Networks (FDSN) and EIDA...
FIGURES
Journal Article
A Depth‐Dependent Local Magnitude Scale for New Zealand Earthquakes Consistent with Moment Magnitude Available to Purchase
Publisher: Seismological Society of America
Published: 22 December 2020
Bulletin of the Seismological Society of America (2021) 111 (2): 1056–1066.
...Figure 10. Scatter plot of (a) M L 1 versus M w for all SeisComP (SC) earthquakes; (b) M L 1 versus M w for SC earthquakes with focal depth h > 40 km ; (c) M LNZ 20 versus M w for all SC earthquakes; and (d) M LNZ...
FIGURES
Includes: Supplemental Content
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