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106 results for “tsunami”
Figure 5 in Effect of environmental change after the 2011 tsunami on the population dynamics of Japanese tubesnout Aulichthys japonicus (Gasterosteiformes)
Figure 5. – Changes of number of Japanese tubesnouts Aulichthys japonicus and ascidians Halocynthia roretzi from 2007 to 2008 and from 2012 to 2016.
Figure 1 in Effect of environmental change after the 2011 tsunami on the population dynamics of Japanese tubesnout Aulichthys japonicus (Gasterosteiformes)
Figure 1. – Location of study area in Okirai Bay and position of the sampling site in Namiita Beach. The white dotted area shows the seagrass bed's area (m2) in August 2014.
Kinematic and Paleoseismic Investigation of an Upper-Plate Fault on Chirikof Island: A Potential Tsunami-Seismic Hazard Source within the Alaska Subduction Zone
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Data for: A further source of Tokyo earthquakes and Pacific Ocean tsunamis
<p>This data repository contains the location of cores collected as part of this study, the microfossil and radiocarbon results from those cores, and fault parameters used in eleven historical and hypothetical tsunami simulations for Kujukuri, Japan (Boso Peninsula).</p> <p>The work is supported by the Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST) and in part by grants awarded to J.E.P. [National Science Foundation (EAR-1303881 and 1624612), Natural Sciences and Engineering Council of Canada (NSERC), Canada Research Chair (CRC) program, and Japan Society for the Promotion of Science (JSPS) International Research Fellow program at the Geological Survey of Japan (PE14038)]; A.C.P. [Science Foundation Ireland Career Development Award (17/CDA/4695), Investigator Award (16/IA/4520), Marine Research Programme funded by the Irish Government, co-financed by the European Regional Development Fund (Grant-Aid Agreement No. PBA/CC/18/01), European Union’s Horizon 2020 research and innovation programme under grant agreement No 818144, and SFI Research Centre (16/RC/3872 and 12/RC/2289_P2); and B.P.H. [Singapore Ministry of Education Academic Research Fund (MOE2019-T3-1-004), National Research Foundation Singapore, and Singapore Ministry of Education, under the Reseach Centers of Excellence initiative].</p>
Direct comparison of the tsunami-generated magnetic field with sea level change for the 2009 Samoa and 2010 Chile tsunamis
<p>This is the dataset for the paper of</p> <p>“<strong>Direct comparison of the tsunami-generated magnetic field with sea level change for the 2009 Samoa and 2010 Chile tsunamis</strong>”</p> <p>in Journal of Geophysical Research: Solid Earth.</p> <p> </p> <p>This dataset includes three zips:</p> <p><strong>1. Processed Observation Tsunami Data</strong></p> <p>-- In this zip, there have the observation tsunami magnetic field and sea level change data of 2009 Samoa and 2010 Chile earthquakes which extracted from the data of the TIARES experiment (Suetsugu et al., 2012).</p> <p><strong>2. Simulated Tsunami Data</strong></p> <p>-- This is the simulated tsunami sea level change and magnetic field of 2009 Samoa and 2010 Chile earthquakes. The tsunami sea level was simulated by JAGURSv5.2 (Baba et al., 2017) and the tsunami magnetic field was simulated by TMTGEMv1.1 (Minami et al., 2017).</p> <p><strong>3. Converted Tsunami Sea Level Change</strong></p> <p>-- The converted sea level changes were calculated by the 2-D analytical solution of tsunami magnetic field (Minami et al., 2021) using the filtered tsunami magnetic vertical component Bz.</p>
Figs. 37–47 in The Chironomidae Larvae Associated With The Tsunami-Impacted Waterbodies Of The Coastal Plain Of Southwestern Thailand
Figs. 37–47. Thai post-tsunami Chironomidae. Dicrotendipes spp.: dorsal heads: 37, D. pelechloris; 38, D. septemmaculatus; 39, D. sarinae. Mentum and ventromental plate: 40, D. pelechloris; 41, D. septemmaculatus; 42; D. sarinae. Kiefferulus spp., dorsal head sclerites: 43, K. longilobus; 44, K. calligaster; 45, K. barbatitarsis. Mentum, ventromental plate, anterior cardo: 46, K. calligaster, 47, K. barbatitarsis. Abbreviations: cly, clypeus; fen, fenestra; sc1–4, labral sclerites 1–4; vmp, ventromental plate.
Figs. 48–59 in The Chironomidae Larvae Associated With The Tsunami-Impacted Waterbodies Of The Coastal Plain Of Southwestern Thailand
Figs. 48–59. Thai post-tsunami Chironomidae. Polypedilum leei: 48, mentum, ventromental plate; 49, anterior thorax; 50, premandible. Mentum, ventromental plate: 51, Polypedilum 'Thai sp 1'; 52, Polypedilum. nubifer; 53, Polypedilum (Pentapedilum) 'K1'. Antenna: 54, Polypedilum 'Thai 2'; 55, P. nubifer; 56, P. 'K1'. 57, Dorsal head sclerites, P. 'Thai 2'. Mandible; 58, P. 'K1', 59, P. 'Thai 2'. Abbreviations: S3, cephalic seta 3; sc1, labral sclerite 1; vmp, ventromental plate.
Figs. 26–36 in The Chironomidae Larvae Associated With The Tsunami-Impacted Waterbodies Of The Coastal Plain Of Southwestern Thailand
Figs. 26–36. Thai post-tsunami Chironomidae. Zavreliella sp.: 26, posterior body. Conochironomus sp.: 27, mentum; 28, antenna. Parachironomus 'K3': 29, labrum; 30; mentum. Kiefferulus sp.: 31, antenna. Chironomus sp.: 32, mandible. Parachironomus sp.: 33, ventromental plate. Chironomus javanus: 34, epipharynx; 35, premandible. Chironomus sp.: 36, premandible. Abbreviations: ll, labral lamella; LO, Lauterborn organ; pmd, premandible; SI, SII, labral setae I, II; vmp, ventromental plate.
Figs. 13–25 in The Chironomidae Larvae Associated With The Tsunami-Impacted Waterbodies Of The Coastal Plain Of Southwestern Thailand
Figs. 13–25. Thai post-tsunami Chironomidae. Ventral head setae and pit: 13, Monopelopia sp., 14, Larsia sp. Larsia sp.: 15, mentum; 16, pupal thoracic horn. Parakiefferiella sp.: 17, mentum; 18, antenna; 19, mandible. Menta: 20, Tanytarsus formosanus; 21, Zavreliella sp. Antennae: 22, Tanytarsus formosanus; 23, Tanytarsus 'Thai 1'; 24, Tanytarsus 'Thai 2'; 25, Zavreliella sp. Abbreviations: LO, Lauterborn organ; m, mentum; sm, submentum; SSm,seta submenta; S9, S10, cephalic setae 9, 10; vmp, ventromental plate; VP, ventral pit.
Figs. 1–12 in The Chironomidae Larvae Associated With The Tsunami-Impacted Waterbodies Of The Coastal Plain Of Southwestern Thailand
Figs. 1–12. Thai post-tsunami Chironomidae. Clinotanypus sp.: 1, lateral body setal fringe; 2, dorsomentum; 3, ventral head (anterior). Tanypus sp.: 4, ligula. Fittkauimyia sp.: 5, ligula, pecten hypopharyngis; 6, mandible; 7, mentum. Ablabesmyia sp.: 8. maxillary palp. Monopelopia sp.: 9, maxillary palp. Ventral head setae and pit of: 10, Paramerina sp., 11, Ablabesmyia sp. Monopelopia sp.: 12, posterior parapod claw. Abbreviations: ant, antenna; dmt, dorsomentum teeth; fr, fringe; lig, ligula; m, mentum; md, mandible; mp, maxillary palp; ph, pecten hypopharyngis; RO, ring organ of maxilla; SSm, seta submenta; S9, S10, cephalic setae 9, 10; VP, ventral pit.
Fig. 6 in Recovery Of The Freshwater Lentic Insect Fauna In Thailand Following The Tsunami Of 2004
Fig. 6. Cluster analyses based on similarity in the taxonomic composition of the insect fauna as estimated by Jaccard's similarity index. A–D, tsunami-inundated and unaffected ponds within each sampling period separately. Inundated ponds are indicated with a "T" and boldface, site numbers correspond with numbers in Table 1 and Figure 1. E, similarity in taxonomic composition among sampling periods (1–4), with ponds pooled within period. Inundated ponds are indicated with a "T" and boldface.
Fig. 4 in Recovery Of The Freshwater Lentic Insect Fauna In Thailand Following The Tsunami Of 2004
Fig. 4. Discriminant Function Analysis with group contour limits for each of four sampling periods of tsunami-inundated ponds using (A) ordinal and (B) family richness values.
Fig. 3 in Recovery Of The Freshwater Lentic Insect Fauna In Thailand Following The Tsunami Of 2004
Fig. 3. Insect species richness levels over four time periods of tsunami-inundated and unaffected ponds within 1 km of the incursion of seawater.
Fig. 2 in Recovery Of The Freshwater Lentic Insect Fauna In Thailand Following The Tsunami Of 2004
Fig. 2. Mean levels of conductivity (µS) in tsunami-inundated and unaffected ponds from which insect communities were sampled from May 2005 to June 2006.
Fig. 1 in Recovery Of The Freshwater Lentic Insect Fauna In Thailand Following The Tsunami Of 2004
Fig. 1. Map of the Isthmus of Kra showing all collection sites. Site numbers correspond with data in Table 1.
Fig. 5 in Recovery Of The Freshwater Lentic Insect Fauna In Thailand Following The Tsunami Of 2004
Fig. 5. Parsimony dendrogram showing succession of 10 sites (ponds) over 4 sampling periods toward the fauna of unaffected control ponds. Site numbers correspond with numbers in Table 1 and Figure 1. Letters A–D following site numbers refer to sampling periods 1–4.
Tsunami Observation Points Database in Eastern Mediterranean
<p>Knowledge of the tsunami observation points of past tsunamis is of great importance since it may help in studies of several kinds, such as better understanding of the source type, determination of the inundation area, and verification of tsunami simulation results. </p> <p>Plenty of information is available about the Tsunami Observation Points (TOPs) of many historical and modern tsunamis observed in Greece and in other areas of the eastern Mediterranean region. The TOPs Database is a systematic compilation of such kind of information. For a specific tsunami event, the TOPs DB includes the source epicenter, the TOPs names and the corresponding geographical coordinates, the names of the localities, and a characterization of the tsunami intensity level, K, in each TOP. K has been estimated according to the 12-grade tsunami intensity scale by Papadopoulos and Imamura (2001). </p> <p>In its current form the TOPs DB provides information about 61 TOPs related to the 9 July 1956 large seismic tsunami generated in the south Aegean Sea. Information about the TOPs and the impact of the wave in each TOP can be found in the publications by Galanopoulos (1957), Ambraseys (1960), Papadopoulos et al. (2005) and Okal et al. (2009). The tsunami intensities have been estimated by Dr G.A. Papadopoulos and Dr I. Triantafyllou. Earthquake source parameters have been adopted from the ISC-GEM (2023) catalogue. </p> <p>The TOPs DB will be gradually expanded with the aim to finally include all the known tsunami events to have occurred in Greece and in other eastern Mediterranean regions in modern and historical times. </p>
Data Set for Sandanbata et al. (2023: GRL) entitled "Two volcanic tsunami events caused by trapdoor faulting at a submerged caldera near Curtis and Cheeseman Islands in the Kermadec Arc"
<p><strong>Descriptions</strong></p> <p>This dataset contains supplementary materials for the manuscript under revision for Geophysical Research Letters; the preprint has been uploaded to ESS Open Archive:</p> <ul> <li>Sandanbata, O., Watada, S., Satake, K., Kanamori, H., & Rivera, L. (2023). Two volcanic tsunami events caused by trapdoor faulting at a submerged caldera near Curtis and Cheeseman Islands in the Kermadec Arc. <em>Geophysical Research Letters</em>, 50, e2022GL101086. <a href="https://doi.org/10.1029/2022GL101086">https://doi.org/10.1029/2022GL101086</a></li> </ul> <p>We constructed a source model for the 2017 earthquake at Curtis caldera in the Kermadec Arc. The dislocation distributions and source geometries of this source model, presented in Figure 3, are contained in this dataset.</p>
Details on the Available Plugins for Tsunami Security Scanner
<p>CSV file containing data from the Tsunami Security Scanner Plugins.</p>
Tsunami Initial Profile and Maximum Runup through Earthquake Source Parameters
<p>The fitting database for 7840 earthquake (tsunami) source scenarios and corresponding N-wave parameters.</p>
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