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<article xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:ali="http://www.niso.org/schemas/ali/1.0/" article-type="research-article" dtd-version="1.2" xml:lang="en"><front><journal-meta><journal-id journal-id-type="publisher-id">Vestnik of the Far East Branch of the Russian Academy of Sciences</journal-id><journal-title-group><journal-title xml:lang="en">Vestnik of the Far East Branch of the Russian Academy of Sciences</journal-title><trans-title-group xml:lang="ru"><trans-title>Вестник Дальневосточного отделения Российской академии наук</trans-title></trans-title-group></journal-title-group><issn publication-format="print">0869-7698</issn><publisher><publisher-name xml:lang="en">The Russian Academy of Sciences</publisher-name></publisher></journal-meta><article-meta><article-id pub-id-type="publisher-id">698774</article-id><article-id pub-id-type="doi">10.7868/S3034530825050088</article-id><article-categories><subj-group subj-group-type="toc-heading" xml:lang="en"><subject>Earth and Environment Sciences</subject></subj-group><subj-group subj-group-type="toc-heading" xml:lang="ru"><subject>Науки о Земле и окружающей среде</subject></subj-group><subj-group subj-group-type="article-type"><subject>Research Article</subject></subj-group></article-categories><title-group><article-title xml:lang="en">Calibration and testing of a new magnitude scale: the case study of a strong crustal earthquake on 01.01.2024 in Japan (Mw = 7,5)</article-title><trans-title-group xml:lang="ru"><trans-title>Калибровка и апробация новой магнитудной шкалы на примере сильного корового землетрясения 01.01.2024 в Японии (Mw = 7,5)</trans-title></trans-title-group></title-group><contrib-group><contrib contrib-type="author"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0003-2997-1524</contrib-id><name-alternatives><name xml:lang="en"><surname>Konovalov</surname><given-names>A. V</given-names></name><name xml:lang="ru"><surname>Коновалов</surname><given-names>А. В</given-names></name></name-alternatives><bio xml:lang="en"><p>Candidate of Sciences in Physics and Mathematics, Leading Researcher</p></bio><bio xml:lang="ru"><p>кандидат физико-математических наук, ведущий научный сотрудник</p></bio><email>a.konovalov@geophystech.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><name-alternatives><name xml:lang="en"><surname>Orlin</surname><given-names>I. D</given-names></name><name xml:lang="ru"><surname>Орлин</surname><given-names>И. Д</given-names></name></name-alternatives><bio xml:lang="en"><p>Engineer</p></bio><bio xml:lang="ru"><p>инженер</p></bio><email>office@geophystech.ru</email><xref ref-type="aff" rid="aff1"/></contrib><contrib contrib-type="author"><contrib-id contrib-id-type="orcid">https://orcid.org/0000-0001-5263-5161</contrib-id><name-alternatives><name xml:lang="en"><surname>Stepnova</surname><given-names>Yu. A</given-names></name><name xml:lang="ru"><surname>Степнова</surname><given-names>Ю. А</given-names></name></name-alternatives><bio xml:lang="en"><p>Candidate of Sciences in Geology and Mineralogy, Senior Researcher</p></bio><bio xml:lang="ru"><p>кандидат геолого-минералогических наук, старший научный сотрудник</p></bio><email>stepnova@fegi.ru</email><xref ref-type="aff" rid="aff1"/></contrib></contrib-group><aff-alternatives id="aff1"><aff><institution xml:lang="en">Far East Geological Institute, FEB RAS</institution></aff><aff><institution xml:lang="ru">Дальневосточный геологический институт ДВО РАН</institution></aff></aff-alternatives><pub-date date-type="pub" iso-8601-date="2025-11-15" publication-format="electronic"><day>15</day><month>11</month><year>2025</year></pub-date><issue>5</issue><issue-title xml:lang="en">NO5 (2025)</issue-title><issue-title xml:lang="ru">№5 (2025)</issue-title><fpage>104</fpage><lpage>115</lpage><history><date date-type="received" iso-8601-date="2025-12-16"><day>16</day><month>12</month><year>2025</year></date></history><permissions><copyright-statement xml:lang="en">Copyright ©; 2025, Russian Academy of Sciences</copyright-statement><copyright-statement xml:lang="ru">Copyright ©; 2025, Российская академия наук</copyright-statement><copyright-year>2025</copyright-year><copyright-holder xml:lang="en">Russian Academy of Sciences</copyright-holder><copyright-holder xml:lang="ru">Российская академия наук</copyright-holder><ali:free_to_read xmlns:ali="http://www.niso.org/schemas/ali/1.0/"/></permissions><self-uri xlink:href="https://journals.eco-vector.com/0869-7698/article/view/698774">https://journals.eco-vector.com/0869-7698/article/view/698774</self-uri><abstract xml:lang="en"><p>A crustal earthquake and its aftershocks that occurred in Japan (Mw = 7,5, 01.01.2024) were studied to make measurements and analyze the parameters of strong ground motion, including the Arias intensity. The latter is one of the key physical parameters used in engineering seismology. The level of the Arias intensity is directly connected with the stress drop in an earthquake source. Therefore, developing and calibrating a magnitude scale that would take into account not only fault dimensions, but also the stress drop in an earthquake source is a vital task of seismological observations. In this paper we present our test results of a new magnitude scale (MIa3) based on a modified Arias intensity. The scale was calibrated to medium and moderate earthquakes in the target area (M ~5). The high efficiency of the proposed scale is evidenced by the magnitudes, determined through the new method, that are almost consistent with the moment magnitude (Mw).</p></abstract><trans-abstract xml:lang="ru"><p>На примере корового землетрясения в Японии (Mw = 7,5, 01.01.2024) и его афтершоков проведены измерения и анализ параметров сильных движений грунта, в том числе интенсивности по Ариасу. Интенсивность Ариаса является одной из главных физических метрик, используемых в инженерной сейсмологии. Уровень интенсивности Ариаса непосредственно связан со сброшенным напряжением в очаге землетрясения, поэтому разработка и калибровка магнитудной шкалы, учитывающей не только размеры разрыва, но и сброшенное напряжение в очаге землетрясения, является актуальной задачей сейсмологических наблюдений. В настоящей работе апробирована новая магнитудная шкала (MIa3&gt;), основанная на модифицированной интенсивности Ариаса. Калибровка шкалы выполнена по средним и умеренным землетрясениям в целевом регионе (M ~5). Высокую эффективность предложенной шкалы подтверждают оценки магнитуды, полученные по новой методике, которые близки к моментной магнитуде (Mw).</p></trans-abstract><kwd-group xml:lang="en"><kwd>magnitude</kwd><kwd>earthquake</kwd><kwd>stress drop</kwd><kwd>Arias intensity</kwd><kwd>tectonics</kwd></kwd-group><kwd-group xml:lang="ru"><kwd>магнитуда</kwd><kwd>землетрясение</kwd><kwd>сброшенное напряжение</kwd><kwd>интенсивность по Ариасу</kwd><kwd>тектоника</kwd></kwd-group><funding-group><funding-statement xml:lang="en">The work was carried out within the framework of the state assignment of the Ministry of Science and Higher Education of the Russian Federation for the Far East Geological Institute, FEB RAS.</funding-statement><funding-statement xml:lang="ru">Работа выполнена в рамках государственного задания Минобрнауки России для ДВГИ ДВО РАН.</funding-statement></funding-group></article-meta></front><body></body><back><ref-list><ref id="B1"><label>1.</label><mixed-citation>Kanamori H. 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