The Atmosphere, Climate and Global Warming. Climate Change Central Questions & Key Concepts What is the atmosphere What is the difference between weather.
Characteristics of large scale climate indices Nate Mantua University of Washington Aquatic and Fishery Sciences GLOBEC/PICES/ICES ECOFOR Workshop, Friday.
INGV - Istituto Nazionale di Geofisica e Vulcanologia - Italy Basics of numerical coupled modelling Antonio Navarra Istituto Nazionale di Geofisica e.
User meeting 14-16 June 20061 Monthly and Seasonal forecasts Laura Ferranti and the Seasonal Forecast Section User meeting 14-16 June 2006.
Training Course 2009 – NWP-PR: Initialization and Ensemble Generation in Seasonal Forecasting Initialization and Ensemble generation for Seasonal Forecasting.
Training Course 2009 – NWP-DA: Ocean Data Assimilation 1 Data assimilation in the ocean Magdalena A. Balmaseda.
Bureau of Meteorology Activities as a GPC of Long Range Forecasts Dr David Jones [email protected] Australian Bureau of Meteorology CBS Expert Team on.
Click to edit Master title style Timeseries of dynamical and precipitation indices Black: observations; RGB: ensemble members for each start date case.
3 Reasons for the biennial tendency: The biennial tendency in HadCM3 2xCO 2 is in contrast with observed basinwide El Niño events which are often of 4-5.
Exploiting observations to seek robust responses in global precipitation Richard P. Allan Department of Meteorology, University of Reading Thanks to Brian.
Climate Modeling Inez Fung University of California, Berkeley.
C LIMATE R ESEARCH IN THE C ARIBBEAN Climate Studies Group, Mona (CSGM) Department of Physics University of the West Indies, Mona.