• Detection, Analysis, and Removal of Glitches From InSight's Seismic Data From Mars 

      Scholz, John‐Robert; Widmer‐Schnidrig, Rudolf; Davis, Paul; Lognonné, PhilippeORCIDiD; Pinot, Baptiste; Garcia, Raphaël F.ORCIDiD; Hurst, KennethORCIDiD; Pou, LaurentORCIDiD; Nimmo, FrancisORCIDiD; Barkaoui, SalmaORCIDiD; de Raucourt, Sébastien; Knapmeyer‐Endrun, BrigitteORCIDiD; Knapmeyer, MartinORCIDiD; Orhand‐Mainsant, Guénolé; Compaire, NicolasORCIDiD; Cuvier, Arthur; Beucler, ÉricORCIDiD; Bonnin, MickaëlORCIDiD; Joshi, RakshitORCIDiD; Sainton, Grégory; Stutzmann, EléonoreORCIDiD; Schimmel, MartinORCIDiD; Horleston, AnnaORCIDiD; Böse, Maren; Ceylan, SavasORCIDiD; Clinton, John; van Driel, Martin; Kawamura, Taichi; Khan, AmirORCIDiD; Stähler, Simon C.ORCIDiD; Giardini, DomenicoORCIDiD; Charalambous, ConstantinosORCIDiD; Stott, Alexander E.ORCIDiD; Pike, William T.; Christensen, Ulrich R.ORCIDiD; Banerdt, W. BruceORCIDiD (Earth and Space Science, 2020-10-30)
      The instrument package SEIS (Seismic Experiment for Internal Structure) with the three very broadband and three short‐period seismic sensors is installed on the surface on Mars as part of NASA's InSight Discovery mission. ...
    • Determination of the lunar body tide from global laser altimetry data 

      Thor, Robin N.ORCIDiD; Kallenbach, Reinald; Christensen, Ulrich R.ORCIDiD; Gläser, PhilippORCIDiD; Stark, AlexanderORCIDiD; Steinbrügge, GregorORCIDiD; Oberst, Jürgen (Journal of Geodesy, 2020-12-23)
      We use global data from the Lunar Orbiter Laser Altimeter (LOLA) to retrieve the lunar tidal Love number h2 and find h2 = 0.0387 ± 0.0025. This result is in agreement with previous estimates from laser altimetry using ...
    • Joint Inversion of Receiver Functions and Apparent Incidence Angles for Sparse Seismic Data 

      Joshi, RakshitORCIDiD; Knapmeyer‐Endrun, BrigitteORCIDiD; Mosegaard, KlausORCIDiD; Igel, HeinerORCIDiD; Christensen, Ulrich R.ORCIDiD (Earth and Space Science, 2021-09-28)
      The estimation of crustal structure and thickness is essential in understanding the formation and evolution of terrestrial planets. Initial planetary missions with seismic instrumentation on board face the additional ...