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First 848 results for ” JR Hannan”

1. Seismic site response in the Netherlands: impact of the shallow subsurface composition on earthquake ground motion amplification

   Local subsurface compositions can strongly influence the level of amplification of ground motion ...

   Janneke van Ginkel Elmer Ruigrok Rien Herber Läslo Evers | Year: 2022

   Publication

2. Amplification behaviour of compressional waves in unconsolidated sediments

   Similar to horizontal earthquake motions, vertical motions are ampli!ed depedent on the local sit...

   Janneke van Ginkel, Elmer Ruigrok, Rick Wentinck, Rien Herber | Journal: Frontiers of Earth Sciences | Volume: 10 | Year: 2022 | First page: 457 | doi: https://doi.org/10.3389/feart.2022.812658

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3. Systematic recovery of instrumental timing and phase errors using interferometric surface-waves retrieved from large-N seismic arrays

   Instrumental timing and phase errors are a notorious problem in seismic data acquisition and proc...

   Cornelis Weemstra, Janneke I. de Laat, Arie Verdel, Pieter Smets | Journal: Geophysical Journal International | Volume: 224 | Year: 2021 | First page: 1028 | Last page: 1055 | doi: https://doi.org/10.1093/gji/ggaa504

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4. CRAAS: A European Cloud Regime dAtAset Based on the CLAAS-2.1 Climate Data Record

   Given the important role of clouds in our planet’s climate system, it is crucial to further impro...

   Tzallas, V.; Hünerbein, A.; Stengel, M.; Meirink, J.F.; Benas, N.; Trentmann, J.; Macke, A. | Journal: Remote Sensing | Volume: 14 | Year: 2022 | doi: 10.3390/rs14215548

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5. Transdimensional ambient-noise surface wave tomography of the Reykjanes Peninsula, SW Iceland

   Ambient noise seismic tomography has proven to be an effective tool for subsurface imaging, parti...

   Amin Rahimi Dalkhani, Thorbjörg Ágústsdóttir, Égill Arni Gudnason, Gylfi Páll Hersir, Xin Zhang, and Cornelis Weemstra | Journal: Geophysical Journal International | Volume: 236 | Year: 2024 | First page: 621 | Last page: 643 | doi: https://doi.org/10.1093/gji/ggad435

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