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Continuation of Lecture 1

Continuation of Lecture 1

Continuation of Lecture 1. Corrections/Clarifications from Day 1. 1. Lin-Rood scheme stability comes about because it is equivalent to a Semi-Lagrangian scheme not using implicit differencing. (Thanks to Ravi for pointing this out).

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608 views • 49 slides
Continuation of Lecture 1

Continuation of Lecture 1

Continuation of Lecture 1. Corrections/Clarifications from Day 1. 1. Lin-Rood scheme stability comes about because it is equivalent to a Semi-Lagrangian scheme not using implicit differencing. (Thanks to Ravi for pointing this out).

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492 views • 49 slides
Overview of Seasonal-to-Decadal (s2d) Activities during the Initial 18 Months

Overview of Seasonal-to-Decadal (s2d) Activities during the Initial 18 Months

Overview of Seasonal-to-Decadal (s2d) Activities during the Initial 18 Months. Francisco J. Doblas Reyes European Centre for Medium-Range Weather Forecasts. RT1 activities. RT1: Development of the EPS Aim: assess best method to estimate model uncertainty.

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240 views • 15 slides
Overview of Seasonal-to-Decadal (s2d) Activities during the Initial 18 Months

Overview of Seasonal-to-Decadal (s2d) Activities during the Initial 18 Months

Overview of Seasonal-to-Decadal (s2d) Activities during the Initial 18 Months. Francisco J. Doblas Reyes European Centre for Medium-Range Weather Forecasts. RT1 activities. RT1: Development of the EPS Aim: assess best method to estimate model uncertainty.

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158 views • 15 slides
Decadal climate predictions with the CMCC-CM coupled OAGCM initialized with ocean analyses

Decadal climate predictions with the CMCC-CM coupled OAGCM initialized with ocean analyses

Istituto Nazionale di Geofisica e Vulcanologia. EGU General Assembly 2011,Vienna, April 2011 – CL3.1. Decadal climate predictions with the CMCC-CM coupled OAGCM initialized with ocean analyses A. Bellucci 1 , S. Gualdi 1,2 , E. Scoccimarro 2 , A. Navarra 1,2 , S.Masina 1,2 and A. Storto 1

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103 views • 1 slides

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