One hundred plus years of recomputed surface wave magnitude of shallow global earthquakes

<p>Among the multitude of magnitude scales developed to measure the size of an earthquake, the surface wave magnitude <span class="inline-formula"><i>M</i><sub>s</sub></span> is the only magnitude type that can be computed since the dawn of modern...

Full description

Bibliographic Details
Main Authors: D. Di Giacomo, D. A. Storchak
Format: Article
Language:English
Published: Copernicus Publications 2022-02-01
Series:Earth System Science Data
Online Access:https://essd.copernicus.org/articles/14/393/2022/essd-14-393-2022.pdf
_version_ 1828142147377823744
author D. Di Giacomo
D. A. Storchak
author_facet D. Di Giacomo
D. A. Storchak
author_sort D. Di Giacomo
collection DOAJ
description <p>Among the multitude of magnitude scales developed to measure the size of an earthquake, the surface wave magnitude <span class="inline-formula"><i>M</i><sub>s</sub></span> is the only magnitude type that can be computed since the dawn of modern observational seismology (beginning of the 20th century) for most shallow earthquakes worldwide. This is possible thanks to the work of station operators, analysts and researchers that performed measurements of surface wave amplitudes and periods on analogue instruments well before the development of recent digital seismological practice. As a result of a monumental undertaking to digitize such pre-1971 measurements from printed bulletins and integrate them in parametric data form into the database of the International Seismological Centre (ISC, <span class="uri">http://www.isc.ac.uk</span>, last access: August 2021), we are able to recompute <span class="inline-formula"><i>M</i><sub>s</sub></span> using a large set of stations and obtain it for the first time for several hundred earthquakes. We summarize the work started at the ISC in 2010 which aims to provide the seismological and broader geoscience community with a revised <span class="inline-formula"><i>M</i><sub>s</sub></span> dataset (i.e., catalogue as well as the underlying station data) starting from December 1904 up to the last complete year reviewed by the ISC (currently 2018). This <span class="inline-formula"><i>M</i><sub>s</sub></span> dataset is available at the ISC Dataset Repository at <a href="https://doi.org/10.31905/0N4HOS2D">https://doi.org/10.31905/0N4HOS2D</a> <span class="cit" id="xref_paren.1">(<a href="#bib1.bibx34">International Seismological Centre</a>, <a href="#bib1.bibx34">2021</a><a href="#bib1.bibx34">d</a>)</span>.</p>
first_indexed 2024-04-11T19:37:03Z
format Article
id doaj.art-285584893d16442db2002cc7d0c3058e
institution Directory Open Access Journal
issn 1866-3508
1866-3516
language English
last_indexed 2024-04-11T19:37:03Z
publishDate 2022-02-01
publisher Copernicus Publications
record_format Article
series Earth System Science Data
spelling doaj.art-285584893d16442db2002cc7d0c3058e2022-12-22T04:06:50ZengCopernicus PublicationsEarth System Science Data1866-35081866-35162022-02-011439340910.5194/essd-14-393-2022One hundred plus years of recomputed surface wave magnitude of shallow global earthquakesD. Di GiacomoD. A. Storchak<p>Among the multitude of magnitude scales developed to measure the size of an earthquake, the surface wave magnitude <span class="inline-formula"><i>M</i><sub>s</sub></span> is the only magnitude type that can be computed since the dawn of modern observational seismology (beginning of the 20th century) for most shallow earthquakes worldwide. This is possible thanks to the work of station operators, analysts and researchers that performed measurements of surface wave amplitudes and periods on analogue instruments well before the development of recent digital seismological practice. As a result of a monumental undertaking to digitize such pre-1971 measurements from printed bulletins and integrate them in parametric data form into the database of the International Seismological Centre (ISC, <span class="uri">http://www.isc.ac.uk</span>, last access: August 2021), we are able to recompute <span class="inline-formula"><i>M</i><sub>s</sub></span> using a large set of stations and obtain it for the first time for several hundred earthquakes. We summarize the work started at the ISC in 2010 which aims to provide the seismological and broader geoscience community with a revised <span class="inline-formula"><i>M</i><sub>s</sub></span> dataset (i.e., catalogue as well as the underlying station data) starting from December 1904 up to the last complete year reviewed by the ISC (currently 2018). This <span class="inline-formula"><i>M</i><sub>s</sub></span> dataset is available at the ISC Dataset Repository at <a href="https://doi.org/10.31905/0N4HOS2D">https://doi.org/10.31905/0N4HOS2D</a> <span class="cit" id="xref_paren.1">(<a href="#bib1.bibx34">International Seismological Centre</a>, <a href="#bib1.bibx34">2021</a><a href="#bib1.bibx34">d</a>)</span>.</p>https://essd.copernicus.org/articles/14/393/2022/essd-14-393-2022.pdf
spellingShingle D. Di Giacomo
D. A. Storchak
One hundred plus years of recomputed surface wave magnitude of shallow global earthquakes
Earth System Science Data
title One hundred plus years of recomputed surface wave magnitude of shallow global earthquakes
title_full One hundred plus years of recomputed surface wave magnitude of shallow global earthquakes
title_fullStr One hundred plus years of recomputed surface wave magnitude of shallow global earthquakes
title_full_unstemmed One hundred plus years of recomputed surface wave magnitude of shallow global earthquakes
title_short One hundred plus years of recomputed surface wave magnitude of shallow global earthquakes
title_sort one hundred plus years of recomputed surface wave magnitude of shallow global earthquakes
url https://essd.copernicus.org/articles/14/393/2022/essd-14-393-2022.pdf
work_keys_str_mv AT ddigiacomo onehundredplusyearsofrecomputedsurfacewavemagnitudeofshallowglobalearthquakes
AT dastorchak onehundredplusyearsofrecomputedsurfacewavemagnitudeofshallowglobalearthquakes