• 文献检索
  • 文档翻译
  • 深度研究
  • 学术资讯
  • Suppr Zotero 插件Zotero 插件
  • 邀请有礼
  • 套餐&价格
  • 历史记录
应用&插件
Suppr Zotero 插件Zotero 插件浏览器插件Mac 客户端Windows 客户端微信小程序
定价
高级版会员购买积分包购买API积分包
服务
文献检索文档翻译深度研究API 文档MCP 服务
关于我们
关于 Suppr公司介绍联系我们用户协议隐私条款
关注我们

Suppr 超能文献

核心技术专利:CN118964589B侵权必究
粤ICP备2023148730 号-1Suppr @ 2026

文献检索

告别复杂PubMed语法,用中文像聊天一样搜索,搜遍4000万医学文献。AI智能推荐,让科研检索更轻松。

立即免费搜索

文件翻译

保留排版,准确专业,支持PDF/Word/PPT等文件格式,支持 12+语言互译。

免费翻译文档

深度研究

AI帮你快速写综述,25分钟生成高质量综述,智能提取关键信息,辅助科研写作。

立即免费体验

2022年1月15日洪阿哈阿帕伊岛火山喷发引发的海啸对哥斯达黎加的影响。

Impact of the tsunami caused by the Hunga Tonga-Hunga Ha'apai eruption in Costa Rica on 15 January 2022.

作者信息

Chacón-Barrantes Silvia, Rivera-Cerdas Fabio, Murillo-Gutiérrez Anthony

机构信息

SINAMOT Program, National University Costa Rica, Heredia, Costa Rica.

出版信息

Bull Volcanol. 2023;85(6):36. doi: 10.1007/s00445-023-01648-x. Epub 2023 May 12.

DOI:10.1007/s00445-023-01648-x
PMID:37200554
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC10176287/
Abstract

UNLABELLED

Hunga Tonga-Hunga Ha'apai had a large eruption (VEI 5-6) on 15 January 2022, which caused a tsunami recorded in all ocean basins. Costa Rica has made many advances in tsunami preparation over the past 9 years since the creation of SINAMOT (, National Tsunami Monitoring System), both on watch and warning protocols and on community preparedness. For the Hunga Tonga-Hunga Ha'apai event, the government declared a low-threat warning, suspending all in-water activities, even though the country did not receive any official warning from PTWC (Pacific Tsunami Warning Center) due to the lack of procedures for tsunamis generated by volcanoes. The tsunami was observed at 24 locations on both the Pacific and Caribbean coasts of Costa Rica, becoming the second most recorded tsunami in the country, after the 1991 Limon tsunami along the Caribbean coast. At 22 of those locations along the continental Pacific coast, observations were made by eyewitnesses, including one collocated with the sea level station at Quepos, which registered the tsunami. At Cocos Island (~ 500 km southwest of the continental Costa Rica, in the Pacific Ocean), several eyewitnesses reported the tsunami at two locations, and it was recorded at the sea level station. The tsunami was also recorded at the sea level station on the Caribbean coast. The tsunami effects reported were a combination of sea level fluctuations, strong currents, and coastal erosion, proving that the response actions were adequate for the size of the tsunami. Tsunami preparedness and the largest waves arriving during a dry season Saturday afternoon allowed the large number of eyewitness reports. This event then increased tsunami awareness in the country and tested protocols and procedures. Still, many people along the coast were not informed of the tsunami during the alert due to their remote location, the short notice of the warning, and a lack of procedures for some communities. There is thus still much work to do, particularly about warning dissemination, a direction in which communities should take an active role.

SUPPLEMENTARY INFORMATION

The online version contains supplementary material available at 10.1007/s00445-023-01648-x.

摘要

未标注

2022年1月15日,洪阿哈阿帕伊岛发生了一次大规模火山喷发(火山爆发指数5 - 6级),引发了一场在所有大洋盆地都有记录的海啸。自国家海啸监测系统(SINAMOT)创建以来的过去9年里,哥斯达黎加在海啸防备方面取得了许多进展,涵盖监测与预警协议以及社区防备等方面。对于洪阿哈阿帕伊岛事件,尽管由于缺乏针对火山引发海啸的相关程序,该国未收到太平洋海啸预警中心(PTWC)的任何官方预警,但政府仍发布了低威胁预警,暂停了所有水上活动。在哥斯达黎加太平洋和加勒比海岸的24个地点观测到了此次海啸,使其成为该国记录次数第二多的海啸,仅次于1991年加勒比海岸的利蒙海啸。在太平洋沿岸大陆的22个地点,有目击者进行了观测,其中一处与克波斯的海平面监测站同址,该监测站记录到了海啸。在科科斯岛(位于哥斯达黎加大陆西南约500公里处的太平洋海域),有几名目击者在两个地点报告了海啸情况,并且在海平面监测站也有记录。加勒比海岸的海平面监测站也记录到了此次海啸。所报告的海啸影响包括海平面波动、强流和海岸侵蚀,这证明应对行动对于此次海啸的规模是足够的。海啸防备措施以及在旱季周六下午到来的最大海浪使得出现了大量目击者报告。此次事件提高了该国对海啸的认识,并对相关协议和程序进行了检验。然而,由于沿海许多地区位置偏远、预警通知时间短以及一些社区缺乏相关程序,在警报期间仍有许多人未被告知海啸情况。因此仍有许多工作要做,特别是在警报传播方面,社区应在这方面发挥积极作用。

补充信息

在线版本包含可在10.1007/s00445 - 023 - 01648 - x获取的补充材料。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/b634357f433c/445_2023_1648_Fig12_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/fbd93476a1f9/445_2023_1648_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/d37b5ffa1e1c/445_2023_1648_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/512793a48e08/445_2023_1648_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/183248619349/445_2023_1648_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/73ffe89e65d5/445_2023_1648_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/43a694ac27a1/445_2023_1648_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/d8b4ad8a15a0/445_2023_1648_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/372b67bc4590/445_2023_1648_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/833d68cb630e/445_2023_1648_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/f6ca254ea17a/445_2023_1648_Fig10_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/77e7b7f1f3ab/445_2023_1648_Fig11_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/b634357f433c/445_2023_1648_Fig12_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/fbd93476a1f9/445_2023_1648_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/d37b5ffa1e1c/445_2023_1648_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/512793a48e08/445_2023_1648_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/183248619349/445_2023_1648_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/73ffe89e65d5/445_2023_1648_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/43a694ac27a1/445_2023_1648_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/d8b4ad8a15a0/445_2023_1648_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/372b67bc4590/445_2023_1648_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/833d68cb630e/445_2023_1648_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/f6ca254ea17a/445_2023_1648_Fig10_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/77e7b7f1f3ab/445_2023_1648_Fig11_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/bab9/10176287/b634357f433c/445_2023_1648_Fig12_HTML.jpg

相似文献

1
Impact of the tsunami caused by the Hunga Tonga-Hunga Ha'apai eruption in Costa Rica on 15 January 2022.2022年1月15日洪阿哈阿帕伊岛火山喷发引发的海啸对哥斯达黎加的影响。
Bull Volcanol. 2023;85(6):36. doi: 10.1007/s00445-023-01648-x. Epub 2023 May 12.
2
Tsunami Effects on the Coast of Mexico by the Hunga Tonga-Hunga Ha'apai Volcano Eruption, Tonga.汤加洪阿哈阿帕伊火山喷发对墨西哥海岸的海啸影响
Pure Appl Geophys. 2022;179(4):1117-1137. doi: 10.1007/s00024-022-03017-9. Epub 2022 Apr 11.
3
Tsunami Runup and Inundation in Tonga from the January 2022 Eruption of Hunga Volcano.2022年1月洪阿火山喷发引发的汤加海啸爬高与淹没情况
Pure Appl Geophys. 2023;180(1):1-22. doi: 10.1007/s00024-022-03215-5. Epub 2022 Dec 28.
4
The near-field tsunami generated by the 15 January 2022 eruption of the Hunga Tonga-Hunga Ha'apai volcano and its impact on Tongatapu, Tonga.2022年1月15日汤加洪阿哈阿帕伊岛火山喷发引发的近场海啸及其对汤加汤加塔布岛的影响。
Sci Rep. 2022 Sep 7;12(1):15187. doi: 10.1038/s41598-022-19486-w.
5
Diverse tsunamigenesis triggered by the Hunga Tonga-Hunga Ha'apai eruption.多种成因引发洪阿哈阿帕伊火山喷发海啸。
Nature. 2022 Sep;609(7928):728-733. doi: 10.1038/s41586-022-05170-6. Epub 2022 Aug 8.
6
Resonance characteristics of tsunami in bay of Japan by the Hunga Tonga-Hunga Ha'apai volcano eruption on 15th January 2022.2022年1月15日汤加洪阿哈阿帕伊岛火山喷发引发的日本海湾海啸共振特征
Sci Rep. 2023 Oct 26;13(1):18385. doi: 10.1038/s41598-023-45601-6.
7
Tonga national emergency medical team response to the 2022 Hunga Tonga-Hunga Ha'apai volcanic eruption and tsunami: the first deployment of the Tonga Emergency Medical Assistance Team (TEMAT).汤加国家紧急医疗救援队对 2022 年洪加汤加-洪加哈派火山喷发和海啸的反应:汤加应急医疗队(TEMAT)的首次部署。
Western Pac Surveill Response J. 2023 May 18;14(6 Spec edition):1-6. doi: 10.5365/wpsar.2023.14.6.1026. eCollection 2023.
8
Australian atmospheric pressure and sea level data during the 2022 Hunga-Tonga Hunga-Ha'apai volcano tsunami.2022 年汤加洪阿哈阿帕伊海底火山喷发海啸期间的澳大利亚气压和海平面数据。
Sci Data. 2024 Jan 23;11(1):114. doi: 10.1038/s41597-024-02949-2.
9
Observational study of the heterogeneous global meteotsunami generated after the Hunga Tonga-Hunga Ha'apai Volcano eruption.观测研究洪加汤加-洪加哈派火山喷发后产生的全球不均匀大气潮涌。
Sci Rep. 2023 May 27;13(1):8649. doi: 10.1038/s41598-023-35800-6.
10
Global fast-traveling tsunamis driven by atmospheric Lamb waves on the 2022 Tonga eruption.由 2022 年汤加火山喷发驱动的大气 Lamb 波引发的全球快速移动海啸。
Science. 2022 Jul;377(6601):91-94. doi: 10.1126/science.abo4364. Epub 2022 May 12.

本文引用的文献

1
Diverse tsunamigenesis triggered by the Hunga Tonga-Hunga Ha'apai eruption.多种成因引发洪阿哈阿帕伊火山喷发海啸。
Nature. 2022 Sep;609(7928):728-733. doi: 10.1038/s41586-022-05170-6. Epub 2022 Aug 8.
2
Global Tonga tsunami explained by a fast-moving atmospheric source.全球汤加海啸由快速移动的大气源引发。
Nature. 2022 Sep;609(7928):734-740. doi: 10.1038/s41586-022-04926-4. Epub 2022 Jun 13.
3
Global fast-traveling tsunamis driven by atmospheric Lamb waves on the 2022 Tonga eruption.由 2022 年汤加火山喷发驱动的大气 Lamb 波引发的全球快速移动海啸。
Science. 2022 Jul;377(6601):91-94. doi: 10.1126/science.abo4364. Epub 2022 May 12.