Topic 3.3: Targeted observations and data assimilation in track prediction Rapporteur: Chun-Chieh Wu PSA Working Group: Sim Aberson, Brian Etherton, Sharanya.
Training Course 2009 – NWP-PR: Calibration of EPSs 1/42 Calibration of EPSs Renate Hagedorn European Centre for Medium-Range Weather Forecasts.
The role of the stratosphere in extended- range forecasting Thomas Jung Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research Germany.
Prediction of Extreme Rainfall of Typhoon Morakot (2009) with the WRF model: Part II: Ensemble Forecast with a New Probability Matching Scheme Xingqin.
Dusanka Zupanski CIRA/Colorado State University Fort Collins, Colorado A General Ensemble-Based Approach to Data Assimilation Model Error and Parameter.
U.S. Contribution to T-NAWDEX: “DOWNSTREAM” Heather Archambault (NPS), Steven Cavallo (OU), Dan Cziczo (MIT), Chris Davis (NCAR), Pat Harr (NPS), Laura.
A Shared Atmosphere-Ocean Dynamical Core: First Validation (Semi-Implicit Semi-Lagrangian) Pierre Pellerin(2), François Roy(1,3), Claude Girard(2), François.
GSI-based EnKF-Var hybrid data assimilation system: implementation and test for hurricane prediction Xuguang Wang, Xu Lu, Yongzuo Li, Ting Lei University.
1 of 141 [email protected] Sergio Masuelli November 2010 Fortaleza Brasil System Engineer of SAC-D Geophysical Applications for MWR Professor.
Squall Lines Loosely defined: A line of either ordinary cells or supercells of finite length (10- hundreds of km) that may contain a stratiform rain region.
Mesoscale Convective Vortices (MCVs) Chris Davis (NCAR ESSL/MMM and RAL) Stan Trier (NCAR ESSL/MMM) Boulder, Colorado 60-h Radar Composite Animation (00.
1 What constrains spread growth in forecasts initialized from ensemble Kalman filters? Tom Hamill (& Jeff Whitaker) NOAA Earth System Research Lab Boulder,