USAP-DC

{"dp_type": "Dataset", "free_text": "Earthquakes"}

[{"awards": "1744958 Wei, Yong; 1744856 Bromirski, Peter", "bounds_geometry": ["POLYGON((-155 -62,-146.3 -62,-137.6 -62,-128.9 -62,-120.2 -62,-111.5 -62,-102.80000000000001 -62,-94.10000000000001 -62,-85.4 -62,-76.7 -62,-68 -62,-68 -64.5,-68 -67,-68 -69.5,-68 -72,-68 -74.5,-68 -77,-68 -79.5,-68 -82,-68 -84.5,-68 -87,-76.7 -87,-85.4 -87,-94.1 -87,-102.8 -87,-111.5 -87,-120.19999999999999 -87,-128.89999999999998 -87,-137.6 -87,-146.3 -87,-155 -87,-155 -84.5,-155 -82,-155 -79.5,-155 -77,-155 -74.5,-155 -72,-155 -69.5,-155 -67,-155 -64.5,-155 -62))"], "date_created": "Fri, 04 Apr 2025 00:00:00 GMT", "description": "This dataset includes the bathymetric model grids used to simulate the impact of Pacific-wide and the West Antarctica ice shelf from tsunamis generated by Circum-Pacific-Rim subduction. zone earthquakes.", "east": -68.0, "geometry": ["POINT(-111.5 -74.5)"], "keywords": "Antarctica; Cryosphere; Model Simulation; Pacific Ocean; Subduction Zone Earthquakes; Tsunami; Tsunami impact; West Antarctica Ice Shelf", "locations": "Antarctica; West Antarctica Ice Shelf; Antarctica; Pacific Ocean", "north": -62.0, "nsf_funding_programs": "Antarctic Glaciology; Antarctic Glaciology", "persons": "Wei, Yong", "project_titles": "Collaborative Research: Do Ocean Wave Impacts Pose a Hazard to the Stability of West Antarctic Ice Shelves?", "projects": [{"proj_uid": "p0010320", "repository": "USAP-DC", "title": "Collaborative Research: Do Ocean Wave Impacts Pose a Hazard to the Stability of West Antarctic Ice Shelves?"}], "repo": "USAP-DC", "repositories": "USAP-DC", "science_programs": null, "south": -87.0, "title": "Datasets of bathymetric model grids for model simulations of tsunami Propagation from Circum-Pacific Subduction Zone to West Antarctic Ice Shelves", "uid": "601924", "west": -155.0}, {"awards": "1744958 Wei, Yong; 1744856 Bromirski, Peter", "bounds_geometry": ["POLYGON((-180 62,-168.8 62,-157.6 62,-146.4 62,-135.2 62,-124 62,-112.80000000000001 62,-101.60000000000001 62,-90.4 62,-79.2 62,-68 62,-68 47.1,-68 32.2,-68 17.299999999999997,-68 2.399999999999999,-68 -12.5,-68 -27.400000000000006,-68 -42.3,-68 -57.2,-68 -72.1,-68 -87,-79.2 -87,-90.4 -87,-101.6 -87,-112.8 -87,-124 -87,-135.2 -87,-146.39999999999998 -87,-157.6 -87,-168.8 -87,180 -87,174 -87,168 -87,162 -87,156 -87,150 -87,144 -87,138 -87,132 -87,126 -87,120 -87,120 -72.1,120 -57.2,120 -42.3,120 -27.4,120 -12.5,120 2.400000000000006,120 17.299999999999997,120 32.2,120 47.099999999999994,120 62,126 62,132 62,138 62,144 62,150 62,156 62,162 62,168 62,174 62,-180 62))"], "date_created": "Fri, 04 Apr 2025 00:00:00 GMT", "description": "The dataset includes model simulation results of the Pacific-wide propagation of tsunamis, specifically the time sequence of the water surface elevation of the tsunami, generated by circum-Pacific-Rim subduction zone earthquakes. The simulation scenarios include two historical events, the September 16, 2025 tsunami generated by the Mw 8.3 Illapel, Chile earthquake and the March 11, 2011 tsunami generated by the Mw 9.1 Honshu, Japan earthquake. Also included are six scenarios generated by hypothetical Mw 8.6 earthquakes in the Alaska, Central America, South America, Kermadec, Kuil, and New Zealand-Tonga subduction zones, respectively. These simulation results have been used as boundary conditions to investigate tsunami impact in the West Antarctica ice shelves.", "east": -68.0, "geometry": ["POINT(-154 -12.5)"], "keywords": "Antarctica; Cryosphere; Model Output; Model Simulation; Pacific Ocean; Subduction Zone Earthquakes; Tsunami; Tsunami impact; West Antarctic Ice Sheet", "locations": "West Antarctic Ice Sheet; Antarctica; Pacific Ocean; Pacific Ocean", "north": 62.0, "nsf_funding_programs": "Antarctic Glaciology; Antarctic Glaciology", "persons": "Wei, Yong", "project_titles": "Collaborative Research: Do Ocean Wave Impacts Pose a Hazard to the Stability of West Antarctic Ice Shelves?", "projects": [{"proj_uid": "p0010320", "repository": "USAP-DC", "title": "Collaborative Research: Do Ocean Wave Impacts Pose a Hazard to the Stability of West Antarctic Ice Shelves?"}], "repo": "USAP-DC", "repositories": "USAP-DC", "science_programs": null, "south": -87.0, "title": "Model simulation data of tsunami propagation in the Pacific Ocean", "uid": "601921", "west": 120.0}, {"awards": "1744958 Wei, Yong; 1744856 Bromirski, Peter", "bounds_geometry": ["POLYGON((-155 -65,-148.5 -65,-142 -65,-135.5 -65,-129 -65,-122.5 -65,-116 -65,-109.5 -65,-103 -65,-96.5 -65,-90 -65,-90 -67.1,-90 -69.2,-90 -71.3,-90 -73.4,-90 -75.5,-90 -77.6,-90 -79.7,-90 -81.8,-90 -83.9,-90 -86,-96.5 -86,-103 -86,-109.5 -86,-116 -86,-122.5 -86,-129 -86,-135.5 -86,-142 -86,-148.5 -86,-155 -86,-155 -83.9,-155 -81.8,-155 -79.7,-155 -77.6,-155 -75.5,-155 -73.4,-155 -71.3,-155 -69.2,-155 -67.1,-155 -65))"], "date_created": "Fri, 04 Apr 2025 00:00:00 GMT", "description": "The dataset includes model simulation results of the tsunami impact on the Thwaites Ice Shelf, specifically the time sequence of the water surface elevation of the tsunami, generated by circum-Pacific-Rim subduction zone earthquakes. The model simulations utilized the boundary conditions provided by the Pacific-wide simulations. The simulation scenarios include two historical events, the September 16, 2025 tsunami generated by the Mw 8.3 Illapel, Chile earthquake and the March 11, 2011 tsunami generated by the Mw 9.1 Honshu, Japan earthquake. Also included are four scenarios generated by hypothetical Mw 8.6 earthquakes in the Alaska, Central America, South America, and Kermadec subduction zones, respectively. ", "east": -90.0, "geometry": ["POINT(-122.5 -75.5)"], "keywords": "Antarctica; Cryosphere; Model Simulation; Ross Sea Ice Shelf; Thwaites Region; Tsunami; Tsunami impact; West Antarctica Ice Shelf", "locations": "Antarctica; West Antarctica Ice Shelf; Ross Sea Ice Shelf; Thwaites Region", "north": -65.0, "nsf_funding_programs": "Antarctic Glaciology; Antarctic Glaciology", "persons": "Wei, Yong", "project_titles": "Collaborative Research: Do Ocean Wave Impacts Pose a Hazard to the Stability of West Antarctic Ice Shelves?", "projects": [{"proj_uid": "p0010320", "repository": "USAP-DC", "title": "Collaborative Research: Do Ocean Wave Impacts Pose a Hazard to the Stability of West Antarctic Ice Shelves?"}], "repo": "USAP-DC", "repositories": "USAP-DC", "science_programs": null, "south": -86.0, "title": "Datasets for Model Simulations of Tsunami Propagation from Circum-Pacific Subduction Zone to West Antarctic Ice Shelves (Thwaites)", "uid": "601923", "west": -155.0}, {"awards": "1744958 Wei, Yong", "bounds_geometry": ["POLYGON((-180 -69,-176.25 -69,-172.5 -69,-168.75 -69,-165 -69,-161.25 -69,-157.5 -69,-153.75 -69,-150 -69,-146.25 -69,-142.5 -69,-142.5 -70.7,-142.5 -72.4,-142.5 -74.1,-142.5 -75.8,-142.5 -77.5,-142.5 -79.2,-142.5 -80.9,-142.5 -82.6,-142.5 -84.3,-142.5 -86,-146.25 -86,-150 -86,-153.75 -86,-157.5 -86,-161.25 -86,-165 -86,-168.75 -86,-172.5 -86,-176.25 -86,180 -86,177.5 -86,175 -86,172.5 -86,170 -86,167.5 -86,165 -86,162.5 -86,160 -86,157.5 -86,155 -86,155 -84.3,155 -82.6,155 -80.9,155 -79.2,155 -77.5,155 -75.8,155 -74.1,155 -72.4,155 -70.7,155 -69,157.5 -69,160 -69,162.5 -69,165 -69,167.5 -69,170 -69,172.5 -69,175 -69,177.5 -69,-180 -69))"], "date_created": "Fri, 04 Apr 2025 00:00:00 GMT", "description": "The dataset includes model simulation results of the tsunami impact on the Ross Sea Ice Shelf, specifically the time sequence of the water surface elevation of the tsunami, generated by circum-Pacific-Rim subduction zone earthquakes. The model simulations utilized the boundary conditions provided by the Pacific-wide simulations. The simulation scenarios include two historical events, the September 16, 2025 tsunami generated by the Mw 8.3 Illapel, Chile earthquake and the March 11, 2011 tsunami generated by the Mw 9.1 Honshu, Japan earthquake. Also included are four scenarios generated by hypothetical Mw 8.6 earthquakes in the Alaska, Central America, Kermadec, and New Zealand-Tonga subduction zones, respectively. ", "east": -142.5, "geometry": ["POINT(-173.75 -77.5)"], "keywords": "Antarctica; Cryosphere; Model Simulation; Ross Ice Shelf; Ross Sea Ice Shelf; Subduction Zone Earthquakes; Tsunami; Tsunami impact; West Antarctica Ice Shelf", "locations": "Antarctica; West Antarctica Ice Shelf; Ross Sea Ice Shelf; Ross Ice Shelf", "north": -69.0, "nsf_funding_programs": "Antarctic Glaciology", "persons": "Wei, Yong", "project_titles": "Collaborative Research: Do Ocean Wave Impacts Pose a Hazard to the Stability of West Antarctic Ice Shelves?", "projects": [{"proj_uid": "p0010320", "repository": "USAP-DC", "title": "Collaborative Research: Do Ocean Wave Impacts Pose a Hazard to the Stability of West Antarctic Ice Shelves?"}], "repo": "USAP-DC", "repositories": "USAP-DC", "science_programs": null, "south": -86.0, "title": "Model simulations of tsunami propagation from Circum-Pacific Subduction Zone to West Antarctic Ice Shelves (Ross Sea)", "uid": "601922", "west": 155.0}, {"awards": "2023355 Schmandt, Brandon", "bounds_geometry": ["POLYGON((-180 -60,-144 -60,-108 -60,-72 -60,-36 -60,0 -60,36 -60,72 -60,108 -60,144 -60,180 -60,180 -63,180 -66,180 -69,180 -72,180 -75,180 -78,180 -81,180 -84,180 -87,180 -90,144 -90,108 -90,72 -90,36 -90,0 -90,-36 -90,-72 -90,-108 -90,-144 -90,-180 -90,-180 -87,-180 -84,-180 -81,-180 -78,-180 -75,-180 -72,-180 -69,-180 -66,-180 -63,-180 -60))"], "date_created": "Wed, 26 Jun 2024 00:00:00 GMT", "description": "This catalog/dataset contains 60,006 seismic events between magnitude (Mw) -1.0 and 4.5. It was obtained using publicly available seismic data from 2000 through 2020. The catalog was generated using a workflow that includes new and established software for earthquake detection (Mousavi et al., 2020; Woollam et al., 2022), association (Zhang et al., 2019), location (Lomax et al., 2000, 2009) and magnitude estimation (Satriano, 2022). Events in the catalog are located near volcanoes, outlet glaciers, ice shelves, and within the continental interior. The catalog thus includes events from diverse source processes (cryospheric, volcanic, and tectonic). Preliminary observations include thousands of events near Mount Erebus, Ross Island, and the McMurdo Sound region, repeated seismic events at Ice Streams or large glaciers, and deep long period events in Marie Byrd Land Executive Committee Range. The file contains the latitude, longitude, depth, origin time, Magnitude, errors in the locations and the RMS. More details of the data set and all relevant methods can be found in Pena Castro et al., 2024.", "east": 180.0, "geometry": ["POINT(0 -89.999)"], "keywords": "Antarctica; Cryosphere; Earthquakes; Icequakes; Volcanic Events", "locations": "Antarctica", "north": -60.0, "nsf_funding_programs": "Antarctic Earth Sciences", "persons": "Pena Castro, Andres", "project_titles": "EAGER: Lowering the detection threshold of Antarctic seismicity to reveal undiscovered intraplate deformation", "projects": [{"proj_uid": "p0010450", "repository": "USAP-DC", "title": "EAGER: Lowering the detection threshold of Antarctic seismicity to reveal undiscovered intraplate deformation"}], "repo": "USAP-DC", "repositories": "USAP-DC", "science_programs": null, "south": -90.0, "title": "A seismic catalog for the southernmost continent", "uid": "601805", "west": -180.0}, {"awards": "1643551 Hansen, Samantha", "bounds_geometry": null, "date_created": "Tue, 10 Mar 2020 00:00:00 GMT", "description": "Dataset includes information on all A- and B-ranked earthquakes (see Hansen et al., 2020) recorded by the Antarctic TAMNNET seismic array that were examined for ULVZ evidence. Information on their attenuation (t*) parameter, signal-to-noise ratio, core-mantle boundary bouncepoint location, and average remainder trace standard deviation are also provided. The provided figure indicates where ULVZ evidence has been found and where possible ULVZ evidence may be indicated.", "east": null, "geometry": null, "keywords": "Antarctica; Core-Mantle Boundary; ScP; Southern Hemisphere; Ultra-Low Velocity Zones", "locations": "Antarctica; Antarctica; Southern Hemisphere", "north": null, "nsf_funding_programs": "Antarctic Earth Sciences", "persons": "Hansen, Samantha; Carson, Sarah; Garnero, Edward; Yu, Shule; Rost, Sebastian", "project_titles": "Collaborative Research: Antarctic Seismic Investigations of ULVZ Structure", "projects": [{"proj_uid": "p0010136", "repository": "USAP-DC", "title": "Collaborative Research: Antarctic Seismic Investigations of ULVZ Structure"}], "repo": "USAP-DC", "repositories": "USAP-DC", "science_programs": null, "south": null, "title": "Investigating Ultra-low Velocity Zones (ULVZs) using an Antarctic Dataset", "uid": "601265", "west": null}, {"awards": null, "bounds_geometry": null, "date_created": "Thu, 15 Jun 2006 00:00:00 GMT", "description": "CUB shear velocity model is created from a large data set of the surface wave fundamental model phase and group velocity measurements. Phase velocities in period range between 40 an 150 s are generously donated by Harvard University and Utrecht University. These phase velocity data sets are described by Ekstr\u00f6m et al. (1997) and Trampert and Woodhouse (1995). The group velocity measurements at periods between 16 and 200s are performed at the Center for Imaging the Earth\u0027s Interior in the University of Colorado at Boulder. The group velocities are measured with the frequency-time analysis (Levshin et al., 1989) in which for every waveform a human analyst defines the frequency range of measurements and separate the signal form a variety of noise sources (e.g., overtones, fundamental modes of different types, other earthquakes, multipaths, scattered arrivals). We used broadband waveforms following earthquakes occurred from 1997 to present and recorded at stations from both global networks (GDSN, GSN, GEOSCOPE) as well as temporary regional arrays. At present, the group velocity dataset is composed of about 200000 paths.\n\nData coverage is generally better for Rayleigh waves than for Love waves, is better at intermediate periods than at very short or very long periods, and is better in the northern than in the southern hemisphere. This heterogeneous data coverage is imposed by the distribution of seismic stations and earthquakes. Data coverage optimizes in Eurasia and is currently worst across Africa, the central Pacific, parts of the Indian Ocean, and Antarctica.", "east": null, "geometry": null, "keywords": null, "locations": null, "north": null, "nsf_funding_programs": null, "persons": "Ritzwoller, Michael", "project_titles": null, "projects": null, "repositories": null, "science_programs": null, "south": null, "title": "Upper Mantle Shear Velocity Model", "uid": "600004", "west": null}]

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