Slide 1Putting to rest WISHE-ful misconceptions Roger K. Smith....LMU Munich In collaboration with: Michael Montgomery..NPS Monterey John Persing....NPS Monterey Slide 2…
Slide 1RAMS/BRAMS Basic equations and some numerical issues Slide 2 General equations The equations are the standard non-hydrostatic Reynolds-averaged primitive equations.…
Slide 1Storm-scale pseudo-GLM lightning assimilation and explicit lightning forecast implemented within the WRF- ARW model Alexandre Fierro, Blake Allen (CIMMS/NOAA- The…
Slide 1 Tropical Biases in Next-Generation Climate Models Stefan Tulich 1 and George Kiladis 2 1 CIRES, University of Colorado, Boulder CO, USA 2 NOAA ESRL, Boulder CO, USA…
Slide 1 Office of Coast Survey / CSDL A Hierarchy of Physical Models for Ecological Applications Lyon Lanerolle 1,2, Richard Patchen 1, Richard Stumpf 3, Frank Aikman III…
Slide 1 Rappin et al. (2011) Paper Discussion Patrick Duran 1 of 22 Introduction Asymmetric Env.ConclusionsQuestionsSymmetric Env. The Impact of Outflow Environment on Tropical…
Slide 1An Improved Global Snow Classification Dataset for Hydrologic Applications (Photo by Kenneth G. Libbrecht and Patricia Rasmussen) Glen E. Liston, CSU Matthew Sturm,…
Slide 1 Indian Monsoon, Indian Ocean dipoles and ENSO Pascal Terray LOCEAN/IPSL, France Fabrice Chauvin CNRM/Météo-France, France Sébastien Dominiak LOCEAN/IPSL, France…
Slide 1 Primitive equation models These are the most sophisticated type of ocean circulation model, including more of the physics than the analysis systems and shallow water…