当サイトでは、より良いサービスを提供するため、クッキーを利用しています。クッキーの使用に同意いただける場合は「同意」ボタンをクリックし、クッキーポリシーについては「詳細を見る」をクリックしてください。詳しくは当サイトの サイトポリシー をご確認ください。

詳細を見る...
ログイン サインアップ
言語:

WEKO3

  • トップ
  • ランキング
To

Field does not validate



インデックスリンク

インデックスツリー

  • RootNode

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": "b05dedfa-5b03-485c-be69-e14f5f3e475a"}, "_deposit": {"id": "4050", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "4050"}, "status": "published"}, "_oai": {"id": "oai:nied-repo.bosai.go.jp:00004050", "sets": []}, "author_link": [], "item_10001_biblio_info_7": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "2017-10", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "10", "bibliographicPageEnd": "8002", "bibliographicPageStart": "7987", "bibliographicVolumeNumber": "122", "bibliographic_titles": [{"bibliographic_title": "JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH", "bibliographic_titleLang": "en"}]}]}, "item_10001_description_5": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "Noise-based crustal seismic velocity changes are known to be affected by environmental perturbations, such as rainfall, atmospheric pressure loading, and temperature changes. Similar to geodetic observations, these external perturbations can mask the effects of tectonic and volcanic processes. In this study, we benefit from the dense Hi-net short-period seismic network that covers the entire Japan to measure continuous changes in seismic velocities over a few years, using noise-based seismic monitoring. Some strong seasonal seismic velocity changes are observed in both southern Japan (Kyushu Island) and northern Japan (Hokkaido Island). Decreasing of seismic velocities in summer in southern Japan can be clearly explained by a model of increased crustal fluid pore pressure associated with high rainfall. In northern Japan, it is necessary to adopt a more complex model to explain the observed seismic velocity variations, which takes into account precipitation, snow depth, and sea level changes. Moreover, western and eastern Hokkaido Island show very different responses to these different external perturbations. The models developed are used to remove the seasonal components of the seismic velocity changes. The minimum remaining detectable seismic velocity change reduces to 10(-5), which allows detection of crustal responses to small earthquakes that are previously hidden in the strong seasonal perturbations.", "subitem_description_language": "en", "subitem_description_type": "Other"}]}, "item_10001_publisher_8": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "AMER GEOPHYSICAL UNION", "subitem_publisher_language": "en"}]}, "item_10001_relation_14": {"attribute_name": "DOI", "attribute_value_mlt": [{"subitem_relation_type_id": {"subitem_relation_type_id_text": "10.1002/2017JB014307"}}]}, "item_10001_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "2169-9356", "subitem_source_identifier_type": "EISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Qing-Yu Wang", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Florent Brenguier", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Michel Campillo", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Albanne Lecointre", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Tetsuya Takeda", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Yosuke Aoki", "creatorNameLang": "en"}]}]}, "item_language": {"attribute_name": "言語", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_title": "Seasonal Crustal Seismic Velocity Changes Throughout Japan", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "Seasonal Crustal Seismic Velocity Changes Throughout Japan", "subitem_title_language": "en"}]}, "item_type_id": "40001", "owner": "1", "path": ["1670839190650"], "permalink_uri": "https://nied-repo.bosai.go.jp/records/4050", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2023-04-27"}, "publish_date": "2023-04-27", "publish_status": "0", "recid": "4050", "relation": {}, "relation_version_is_last": true, "title": ["Seasonal Crustal Seismic Velocity Changes Throughout Japan"], "weko_shared_id": -1}
  1. 防災科研関係論文

Seasonal Crustal Seismic Velocity Changes Throughout Japan

https://nied-repo.bosai.go.jp/records/4050
https://nied-repo.bosai.go.jp/records/4050
6b5fa33c-f8e2-42cf-a598-8c0b6518af54
Item type researchmap(1)
公開日 2023-04-27
タイトル
言語 en
タイトル Seasonal Crustal Seismic Velocity Changes Throughout Japan
言語
言語 eng
著者 Qing-Yu Wang

× Qing-Yu Wang

en Qing-Yu Wang

Search repository
Florent Brenguier

× Florent Brenguier

en Florent Brenguier

Search repository
Michel Campillo

× Michel Campillo

en Michel Campillo

Search repository
Albanne Lecointre

× Albanne Lecointre

en Albanne Lecointre

Search repository
Tetsuya Takeda

× Tetsuya Takeda

en Tetsuya Takeda

Search repository
Yosuke Aoki

× Yosuke Aoki

en Yosuke Aoki

Search repository
抄録
内容記述タイプ Other
内容記述 Noise-based crustal seismic velocity changes are known to be affected by environmental perturbations, such as rainfall, atmospheric pressure loading, and temperature changes. Similar to geodetic observations, these external perturbations can mask the effects of tectonic and volcanic processes. In this study, we benefit from the dense Hi-net short-period seismic network that covers the entire Japan to measure continuous changes in seismic velocities over a few years, using noise-based seismic monitoring. Some strong seasonal seismic velocity changes are observed in both southern Japan (Kyushu Island) and northern Japan (Hokkaido Island). Decreasing of seismic velocities in summer in southern Japan can be clearly explained by a model of increased crustal fluid pore pressure associated with high rainfall. In northern Japan, it is necessary to adopt a more complex model to explain the observed seismic velocity variations, which takes into account precipitation, snow depth, and sea level changes. Moreover, western and eastern Hokkaido Island show very different responses to these different external perturbations. The models developed are used to remove the seasonal components of the seismic velocity changes. The minimum remaining detectable seismic velocity change reduces to 10(-5), which allows detection of crustal responses to small earthquakes that are previously hidden in the strong seasonal perturbations.
言語 en
書誌情報 en : JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH

巻 122, 号 10, p. 7987-8002, 発行日 2017-10
出版者
言語 en
出版者 AMER GEOPHYSICAL UNION
ISSN
収録物識別子タイプ EISSN
収録物識別子 2169-9356
DOI
関連識別子 10.1002/2017JB014307
戻る
0
views
See details
Views

Versions

Ver.1 2023-03-31 01:42:51.014788
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