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| Sprache: | en |
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PANGAEA
2023
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| Online-Zugang: | https://doi.org/10.1594/PANGAEA.963465 |
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| _version_ | 1867169157727911936 |
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| author | Fäh, Donat Shynkarenko, Anastasiia Marrios Lontsi, Agostiny Kremer, Katrina Anselmetti, Flavio S Schmidt-Aursch, Mechita |
| author_facet | Fäh, Donat Shynkarenko, Anastasiia Marrios Lontsi, Agostiny Kremer, Katrina Anselmetti, Flavio S Schmidt-Aursch, Mechita |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | The project "Lake Tsunamis: Causes, Controls, and Hazard (Characterization of subaqueous unstable slopes with geophysical and geotechnical measurements.)" was initiated to understand their governing mechanisms of genesis, propagation, frequency, and the related hazard within an interdisciplinary context. Swiss lakes served as a laboratory for this holistic approach. The project was divided into five work packages (WP), where WP1 comprised a large number of geophysical (using amongst other techniques ocean bottom seismometers (OBS)) and geotechnical measurements to characterize the structure and stability of potentially unstable subaqueous lake slopes. To evaluate the potential and applicability of ambient vibration techniques in a shallow-water offshore environment, multiple single-station and array OBS measurements were performed on subaqueous slopes in Lake Lucerne. Eight DEPAS Lobster type broadband OBS from the German Instrument Pool for Amphibian Seismology (DEPAS) and one Nammu type OBS from ETH Zürich were successfully deployed and recovered at more than 170 distinct locations in 2018-2020. In 2020-2023 the single Nammu OBS was deployed several times for supplemental measurements. Surveys with an airgun of 1-inch³ volume were used on top of the deployment locations to determine the misorientation of the horizontal components. In addition, multibeam bathymetric surveys were performed to locate the positions of the OBS on the lake floor with high accuracy. A workflow for passive seismic investigations with OBS in such shallow-water settings was developed. The seismic response and its variability at the measured sites in terms of amplification functions during earthquakes and resonance frequencies was determined. Shear-wave velocity profiles at different morphological types of slopes down to a depth of 100-150 m below the lake floor were resolved and interpreted. Combining geophysical and geotechnical measurements and interpretation, static and dynamic slope-stability analyses were performed. Thresholds for the subaqueous slope-failure triggering in terms of earthquake magnitude and epicentral distance, macroseismic intensity, and ground-motion intensity measures were derived using earthquake ground-motion modelling. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_963465 |
| institution | PANGAEA |
| language | en |
| publishDate | 2023 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Project LAKE TSUNAMIS: ocean-bottom seismometer operations in Lake Lucerne (Switzerland) in 2018-2023 Fäh, Donat Shynkarenko, Anastasiia Marrios Lontsi, Agostiny Kremer, Katrina Anselmetti, Flavio S Schmidt-Aursch, Mechita Binary Object; Clock skew; Code; Comment; Date/time end; Date/time start; ELEVATION; Event label; Hydrophone, serial number; Hydrophone gain; Hydrophone polarity; Hydrophone type; Lake Lucerne, Switzerland; LATITUDE; LONGITUDE; OBS; Ocean bottom seismometer; Principal investigator; Project; Recorder, serial number; Recorder type; Sampling rate; Seismometer, serial number; Seismometer gain; Seismometer type; Station label; XJ_CHA01; XJ_CHA02; XJ_CHA03; XJ_CHA04; XJ_CHA05; XJ_CHA06; XJ_CHA07; XJ_CHA08; XJ_CHA09; XJ_CHB01; XJ_CHB02; XJ_CHB03; XJ_CHB04; XJ_CHB05; XJ_CHB06; XJ_CHB07; XJ_CHB08; XJ_CHB09; XJ_CHC01; XJ_CHC02; XJ_CHC03; XJ_CHC04; XJ_CHC05; XJ_CHC06; XJ_CHC07; XJ_CHC08; XJ_CHC09; XJ_CHS01; XJ_CHS02; XJ_CHS03; XJ_CIA01; XJ_CIA02; XJ_CIA03; XJ_CIA04; XJ_CIA05; XJ_CIA06; XJ_CIA07; XJ_CIA08; XJ_CIA09; XJ_CIS01; XJ_CIS02; XJ_ENA01; XJ_ENA02; XJ_ENA03; XJ_ENA04; XJ_ENA05; XJ_ENA06; XJ_ENA07; XJ_ENA08; XJ_ENA09; XJ_ENB01; XJ_ENB02; XJ_ENB03; XJ_ENB04; XJ_ENB05; XJ_ENB06; XJ_ENB07; XJ_ENB08; XJ_ENB09; XJ_ENS01; XJ_ENS02; XJ_ENS03; XJ_ENS04; XJ_ENS05; XJ_ENS06; XJ_ENS07; XJ_FLS01; XJ_FLS02; XJ_HOS01; XJ_KEA01; XJ_KEA02; XJ_KEA03; XJ_KEA04; XJ_KEA05; XJ_KEA06; XJ_KEA07; XJ_KEA08; XJ_KEA09; XJ_KEB01; XJ_KEB02; XJ_KEB03; XJ_KEB04; XJ_KEB05; XJ_KEB06; XJ_KEB07; XJ_KEB08; XJ_KEB09; XJ_KES01; XJ_KES02; XJ_LUS01; XJ_MUA02; XJ_MUA03; XJ_MUA04; XJ_MUA05; XJ_MUA06; XJ_MUA07; XJ_MUA08; XJ_MUA09; XJ_MUS01; XJ_MUS02; XJ_NAA01; XJ_NAA02; XJ_NAA03; XJ_NAA04; XJ_NAA05; XJ_NAA06; XJ_NAA07; XJ_NAA08; XJ_NAA09; XJ_NAS01; XJ_NAS02; XJ_NIA01; XJ_NIA02; XJ_NIA03; XJ_NIA04; XJ_NIA05; XJ_NIA06; XJ_NIA07; XJ_NIA08; XJ_NIA09; XJ_NIB01; XJ_NIB02; XJ_NIB03; XJ_NIB04; XJ_NIB05; XJ_NIB06; XJ_NIB07; XJ_NIB08; XJ_NIB09; XJ_NIC01; XJ_NIC02; XJ_NIC03; XJ_NIC04; XJ_NIC05; XJ_NIC06; XJ_NIC07; XJ_NIC08; XJ_NIC09; XJ_NIS01; XJ_NIS02; XJ_NIS03; XJ_NIS04; XJ_WEA01; XJ_WEA02; XJ_WEA03; XJ_WEA04; XJ_WEA05; XJ_WEA06; XJ_WEA07; XJ_WEA08; XJ_WEA09; XJ_WEB01; XJ_WEB02; XJ_WEB03; XJ_WEB04; XJ_WEB05; XJ_WEB06; XJ_WEB07; XJ_WEB08; XJ_WEB09; XJ_WEC01; XJ_WEC02; XJ_WEC03; XJ_WEC04; XJ_WEC05; XJ_WEC06; XJ_WEC07; XJ_WEC08; XJ_WEC09; XJ_WED01; XJ_WED02; XJ_WED03; XJ_WED04; XJ_WED05; XJ_WED06; XJ_WED07; XJ_WED08; XJ_WED09; XJ_WES01; XJ_WES02; XJ_WES03 The project "Lake Tsunamis: Causes, Controls, and Hazard (Characterization of subaqueous unstable slopes with geophysical and geotechnical measurements.)" was initiated to understand their governing mechanisms of genesis, propagation, frequency, and the related hazard within an interdisciplinary context. Swiss lakes served as a laboratory for this holistic approach. The project was divided into five work packages (WP), where WP1 comprised a large number of geophysical (using amongst other techniques ocean bottom seismometers (OBS)) and geotechnical measurements to characterize the structure and stability of potentially unstable subaqueous lake slopes. To evaluate the potential and applicability of ambient vibration techniques in a shallow-water offshore environment, multiple single-station and array OBS measurements were performed on subaqueous slopes in Lake Lucerne. Eight DEPAS Lobster type broadband OBS from the German Instrument Pool for Amphibian Seismology (DEPAS) and one Nammu type OBS from ETH Zürich were successfully deployed and recovered at more than 170 distinct locations in 2018-2020. In 2020-2023 the single Nammu OBS was deployed several times for supplemental measurements. Surveys with an airgun of 1-inch³ volume were used on top of the deployment locations to determine the misorientation of the horizontal components. In addition, multibeam bathymetric surveys were performed to locate the positions of the OBS on the lake floor with high accuracy. A workflow for passive seismic investigations with OBS in such shallow-water settings was developed. The seismic response and its variability at the measured sites in terms of amplification functions during earthquakes and resonance frequencies was determined. Shear-wave velocity profiles at different morphological types of slopes down to a depth of 100-150 m below the lake floor were resolved and interpreted. Combining geophysical and geotechnical measurements and interpretation, static and dynamic slope-stability analyses were performed. Thresholds for the subaqueous slope-failure triggering in terms of earthquake magnitude and epicentral distance, macroseismic intensity, and ground-motion intensity measures were derived using earthquake ground-motion modelling. |
| title | Project LAKE TSUNAMIS: ocean-bottom seismometer operations in Lake Lucerne (Switzerland) in 2018-2023 |
| topic | Binary Object; Clock skew; Code; Comment; Date/time end; Date/time start; ELEVATION; Event label; Hydrophone, serial number; Hydrophone gain; Hydrophone polarity; Hydrophone type; Lake Lucerne, Switzerland; LATITUDE; LONGITUDE; OBS; Ocean bottom seismometer; Principal investigator; Project; Recorder, serial number; Recorder type; Sampling rate; Seismometer, serial number; Seismometer gain; Seismometer type; Station label; XJ_CHA01; XJ_CHA02; XJ_CHA03; XJ_CHA04; XJ_CHA05; XJ_CHA06; XJ_CHA07; XJ_CHA08; XJ_CHA09; XJ_CHB01; XJ_CHB02; XJ_CHB03; XJ_CHB04; XJ_CHB05; XJ_CHB06; XJ_CHB07; XJ_CHB08; XJ_CHB09; XJ_CHC01; XJ_CHC02; XJ_CHC03; XJ_CHC04; XJ_CHC05; XJ_CHC06; XJ_CHC07; XJ_CHC08; XJ_CHC09; XJ_CHS01; XJ_CHS02; XJ_CHS03; XJ_CIA01; XJ_CIA02; XJ_CIA03; XJ_CIA04; XJ_CIA05; XJ_CIA06; XJ_CIA07; XJ_CIA08; XJ_CIA09; XJ_CIS01; XJ_CIS02; XJ_ENA01; XJ_ENA02; XJ_ENA03; XJ_ENA04; XJ_ENA05; XJ_ENA06; XJ_ENA07; XJ_ENA08; XJ_ENA09; XJ_ENB01; XJ_ENB02; XJ_ENB03; XJ_ENB04; XJ_ENB05; XJ_ENB06; XJ_ENB07; XJ_ENB08; XJ_ENB09; XJ_ENS01; XJ_ENS02; XJ_ENS03; XJ_ENS04; XJ_ENS05; XJ_ENS06; XJ_ENS07; XJ_FLS01; XJ_FLS02; XJ_HOS01; XJ_KEA01; XJ_KEA02; XJ_KEA03; XJ_KEA04; XJ_KEA05; XJ_KEA06; XJ_KEA07; XJ_KEA08; XJ_KEA09; XJ_KEB01; XJ_KEB02; XJ_KEB03; XJ_KEB04; XJ_KEB05; XJ_KEB06; XJ_KEB07; XJ_KEB08; XJ_KEB09; XJ_KES01; XJ_KES02; XJ_LUS01; XJ_MUA02; XJ_MUA03; XJ_MUA04; XJ_MUA05; XJ_MUA06; XJ_MUA07; XJ_MUA08; XJ_MUA09; XJ_MUS01; XJ_MUS02; XJ_NAA01; XJ_NAA02; XJ_NAA03; XJ_NAA04; XJ_NAA05; XJ_NAA06; XJ_NAA07; XJ_NAA08; XJ_NAA09; XJ_NAS01; XJ_NAS02; XJ_NIA01; XJ_NIA02; XJ_NIA03; XJ_NIA04; XJ_NIA05; XJ_NIA06; XJ_NIA07; XJ_NIA08; XJ_NIA09; XJ_NIB01; XJ_NIB02; XJ_NIB03; XJ_NIB04; XJ_NIB05; XJ_NIB06; XJ_NIB07; XJ_NIB08; XJ_NIB09; XJ_NIC01; XJ_NIC02; XJ_NIC03; XJ_NIC04; XJ_NIC05; XJ_NIC06; XJ_NIC07; XJ_NIC08; XJ_NIC09; XJ_NIS01; XJ_NIS02; XJ_NIS03; XJ_NIS04; XJ_WEA01; XJ_WEA02; XJ_WEA03; XJ_WEA04; XJ_WEA05; XJ_WEA06; XJ_WEA07; XJ_WEA08; XJ_WEA09; XJ_WEB01; XJ_WEB02; XJ_WEB03; XJ_WEB04; XJ_WEB05; XJ_WEB06; XJ_WEB07; XJ_WEB08; XJ_WEB09; XJ_WEC01; XJ_WEC02; XJ_WEC03; XJ_WEC04; XJ_WEC05; XJ_WEC06; XJ_WEC07; XJ_WEC08; XJ_WEC09; XJ_WED01; XJ_WED02; XJ_WED03; XJ_WED04; XJ_WED05; XJ_WED06; XJ_WED07; XJ_WED08; XJ_WED09; XJ_WES01; XJ_WES02; XJ_WES03 |
| url | https://doi.org/10.1594/PANGAEA.963465 |