Climate Models. 1-D Radiative convective models The atmosphere is divided into several (about 50) vertical layers. Each layer can either represent the.
Svetlana Y. Kotchenova 1, Eric F. Vermote 1,2, Philip A. Farris 1, & Jose G. Roa 1 1 Department of Geography, University of Maryland, USA; 2 NASA/GSFC.
Combining Observations and Models: A Bayesian View Mark Berliner, OSU Stat Dept Bayesian Hierarchical Models Selected Approaches Geophysical Examples Discussion.
Sablefish recruitment off Sitka Island and Mesoscale Circulation by A. Smith, K. Shotwell (NOAA), M. Stachura (UW) and E. Di Lorenzo.
INGV - Istituto Nazionale di Geofisica e Vulcanologia - Italy Basics of numerical coupled modelling Antonio Navarra Istituto Nazionale di Geofisica e.
Seasonal forecasting: status and plans David Anderson Tim Stockdale, Magdalena Balmasda, Arthur Vidard, Alberto Troccoli, Paco Doblas-Reyes, Kristian Morgensen,
Climate Prediction Division Japan Meteorological Agency Developments for Climate Services at Japan Meteorological Agency 1.
4th u3 l1_weathering_erosion
Dispersão de Petroleo
Introduction to parametrization Introduction to Parametrization of Sub-grid Processes Anton Beljaars ([email protected] room 114) What is parametrization?
Introducing ECMWF Anna Ghelli [email protected].
THE NCEP CLIMATE FORECAST SYSTEM Version 2 Implementation Date: 22 Feb 2011 [email protected] THE ENVIRONMENTAL MODELING CENTER NCEP/NWS/NOAA.
