Search Results

You are looking at 1 - 2 of 2 items for :

  • Boundary currents x
  • DEEPWAVE: The Deep Propagating Gravity Wave Experiment x
  • Monthly Weather Review x
  • Refine by Access: All Content x
Clear All
Benedikt Ehard, Peggy Achtert, Andreas Dörnbrack, Sonja Gisinger, Jörg Gumbel, Mikhail Khaplanov, Markus Rapp, and Johannes Wagner

higher than 1 hPa were found to become unstable. Currently, we do not know why this is the case but will investigate this issue in the future. The initial and boundary conditions for the WRF Model are supplied by ECMWF operational analysis on 137 model levels with a temporal resolution of 6 h. Further details about the model setup can be found in the appendix . The complete WRF output is available every 60 and 30 min for the outer and inner domain, respectively. In addition, the momentary basic

Full access
Stephen D. Eckermann, Jun Ma, Karl W. Hoppel, David D. Kuhl, Douglas R. Allen, James A. Doyle, Kevin C. Viner, Benjamin C. Ruston, Nancy L. Baker, Steven D. Swadley, Timothy R. Whitcomb, Carolyn A. Reynolds, Liang Xu, N. Kaifler, B. Kaifler, Iain M. Reid, Damian J. Murphy, and Peter T. Love

structured around a global, three-time-level (3TL), semi-implicit, semi-Lagrangian (SISL) dynamical core. In the vertical, the model uses the NEWHYB2 hybrid σ – p coordinate of Eckermann (2009) . For operational NWP at the Fleet Numerical Meteorology and Oceanography Center (FNMOC), 60 vertical layers (L60) are currently adopted with a rigid upper boundary at p top = 0.04 hPa (see Fig. 1 of Eckermann et al. 2014 ). As shown in Fig. 3b , in extending NAVGEM through the MLT, we mirrored those

Full access