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@ARTICLE{Genthe:614384,
      author       = {Genthe, Erik and Czwalinna, Marie Kristin and
                      Lautenschlager, Bjoern and Schlarb, Holger and Hadziioannou,
                      Celine and Gerberding, Oliver and Isleif, Katharina-Sophie},
      title        = {{S}eismic {N}oise {C}ontributions to {E}u{XFEL} {B}unch
                      {A}rrival {T}ime {J}itter from {O}cean-{G}enerated
                      {M}icroseism},
      journal      = {High power laser science and engineering},
      volume       = {13},
      issn         = {2095-4719},
      address      = {Cambridge},
      publisher    = {Cambridge Univ. Press},
      reportid     = {PUBDB-2024-05851},
      pages        = {e52},
      year         = {2025},
      note         = {Title has changed to: Seismic Noise Contributions to EuXFEL
                      Bunch Arrival Time Jitter from Ocean-Generated Microseism},
      abstract     = {Measurements of the bunch arrival times at the European
                      XFEL show noise contributions in the spectral rangebetween
                      0.05 Hz and 0.5 Hz with peak-to-peak jitter of up to 25 fs.
                      Correlation with Distributed Acoustic Sensing(DAS)
                      measurements confirms the seismic origin. The seismic noise
                      in this frequency band is known to be ocean-generated
                      microseism. Both primary and secondary ocean-generated
                      microseism were identified using seismometersand a numerical
                      ocean wave model. Whereas secondary microseism has a strong
                      impact on the bunch arrival time,primary microseism has no
                      notable effect. Rayleigh waves cause the effect, while Love
                      waves have minimal impact.In the presented cases, the noise
                      originates from the North Atlantic and/or the North Sea. The
                      amplitude of the noisedepends on the local weather
                      conditions and is much stronger in winter. Ocean-generated
                      microseism is a significantbottleneck that must be addressed
                      to achieve femtosecond bunch arrival time stability in the
                      sub-Hz regime},
      cin          = {MSK},
      ddc          = {620},
      cid          = {I:(DE-H253)MSK-20120731},
      pnm          = {621 - Accelerator Research and Development (POF4-621) / DFG
                      project G:(GEPRIS)390833306 - EXC 2121: Quantum Universe
                      (390833306)},
      pid          = {G:(DE-HGF)POF4-621 / G:(GEPRIS)390833306},
      experiment   = {EXP:(DE-MLZ)NOSPEC-20140101 /
                      EXP:(DE-H253)XFEL-Exp-20150101},
      typ          = {PUB:(DE-HGF)16},
      doi          = {10.1017/hpl.2025.40},
      url          = {https://bib-pubdb1.desy.de/record/614384},
}