ログイン サインアップ
言語:

WEKO3

  • トップ
  • ランキング
To
lat lon distance
To

Field does not validate



インデックスリンク

インデックスツリー

メールアドレスを入力してください。

WEKO

One fine body…

WEKO

One fine body…

アイテム

{"_buckets": {"deposit": "4d31b4a1-907e-4ac4-90eb-3e7f7cb4feac"}, "_deposit": {"id": "5077", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "5077"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00005077", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2019-03"}, "bibliographicVolumeNumber": "71", "bibliographic_titles": [{"bibliographic_title": "EARTH PLANETS AND SPACE", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "Earthquake ruptures cause mass redistribution, which is expected to induce transient gravity perturbations simultaneously at all distances from the source before the arrival of P-waves. A recent research paper reported the detection of such prompt gravity signals from the 2011 Tohoku-Oki earthquake by comparing observed acceleration waveforms and model simulations. The 11 observed waveforms presented in that paper recorded in East Asia shared a similar trend above the background seismic noise and were in good agreement with the simulations. However, the signal detection was less quantitative because the significance of the observed signals was not discussed and the waveforms at other stations in the region were not shown. In this study, similar trends were not observed in most of the data recorded near the stations used in the aforementioned study, suggesting that the reported signals were only local noises. We thus took a different approach to identify the prompt signals. We optimized the multi-channel data recorded by superconducting gravimeters, broadband seismometers, and tiltmeters. Though no signal was identified in the single-trace records, the stacked trace of the broadband seismometer array data in Japan showed a clear signal above the reduced noise level. The signal amplitude was 0.25nm/s(2) for an average distance of 987km from the event hypocenter. This detection was confirmed with a statistical significance of 7 sigma, where sigma is the standard deviation of the amplitude of the background noise. This result provided the first constraint on the amplitude of the observed prompt signals and may serve as a reference in the detection of prompt signals in future earthquakes.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_publisher_8": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "SPRINGEROPEN", "subitem_publisher_language": "en"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.1186/s40623-019-1006-x"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "1880-5981", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Masaya Kimura", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Nobuki Kame", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Shingo Watada", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Makiko Ohtani", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Akito Araya", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Yuichi Imanishi", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Masaki Ando", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Takashi Kunugi", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Earthquake-induced prompt gravity signals identified in dense array data in Japan", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Earthquake-induced prompt gravity signals identified in dense array data in Japan", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/5077", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-03-30"}, "publish_date": "2023-03-30", "publish_status": "0", "recid": "5077", "relation": {}, "relation_version_is_last": true, "title": ["Earthquake-induced prompt gravity signals identified in dense array data in Japan"], "weko_shared_id": -1}
  1. 防災科研関係論文

Earthquake-induced prompt gravity signals identified in dense array data in Japan

https://nied-repo.bosai.go.jp/records/5077
https://nied-repo.bosai.go.jp/records/5077
f818db0d-cd38-4856-a781-2cf0c59533d3
Item type researchmap(1)
公開日 2023-03-30
タイトル
言語 en
タイトル Earthquake-induced prompt gravity signals identified in dense array data in Japan
言語
言語 eng
著者 Masaya Kimura

× Masaya Kimura

en Masaya Kimura

Search repository
Nobuki Kame

× Nobuki Kame

en Nobuki Kame

Search repository
Shingo Watada

× Shingo Watada

en Shingo Watada

Search repository
Makiko Ohtani

× Makiko Ohtani

en Makiko Ohtani

Search repository
Akito Araya

× Akito Araya

en Akito Araya

Search repository
Yuichi Imanishi

× Yuichi Imanishi

en Yuichi Imanishi

Search repository
Masaki Ando

× Masaki Ando

en Masaki Ando

Search repository
Takashi Kunugi

× Takashi Kunugi

en Takashi Kunugi

Search repository
抄録
内容記述タイプ Other
内容記述 Earthquake ruptures cause mass redistribution, which is expected to induce transient gravity perturbations simultaneously at all distances from the source before the arrival of P-waves. A recent research paper reported the detection of such prompt gravity signals from the 2011 Tohoku-Oki earthquake by comparing observed acceleration waveforms and model simulations. The 11 observed waveforms presented in that paper recorded in East Asia shared a similar trend above the background seismic noise and were in good agreement with the simulations. However, the signal detection was less quantitative because the significance of the observed signals was not discussed and the waveforms at other stations in the region were not shown. In this study, similar trends were not observed in most of the data recorded near the stations used in the aforementioned study, suggesting that the reported signals were only local noises. We thus took a different approach to identify the prompt signals. We optimized the multi-channel data recorded by superconducting gravimeters, broadband seismometers, and tiltmeters. Though no signal was identified in the single-trace records, the stacked trace of the broadband seismometer array data in Japan showed a clear signal above the reduced noise level. The signal amplitude was 0.25nm/s(2) for an average distance of 987km from the event hypocenter. This detection was confirmed with a statistical significance of 7 sigma, where sigma is the standard deviation of the amplitude of the background noise. This result provided the first constraint on the amplitude of the observed prompt signals and may serve as a reference in the detection of prompt signals in future earthquakes.
言語 en
書誌情報 en : EARTH PLANETS AND SPACE

巻 71
出版者
言語 en
出版者 SPRINGEROPEN
ISSN
収録物識別子タイプ ISSN
収録物識別子 1880-5981
DOI
関連識別子 10.1186/s40623-019-1006-x
戻る
0
views
See details
Views

Versions

Ver.1 2023-03-31 02:12:10.967123
Show All versions

エクスポート

OAI-PMH
  • OAI-PMH JPCOAR
  • OAI-PMH DublinCore
  • OAI-PMH DDI
Other Formats
  • JSON
  • BIBTEX

Confirm


Powered by WEKO3

Change consent settings


Powered by WEKO3

Change consent settings