'Flux correction' presentation slideshows

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On Climate Predictability of the Summer Monsoon Rainfall Bin Wang

On Climate Predictability of the Summer Monsoon Rainfall Bin Wang

On Climate Predictability of the Summer Monsoon Rainfall Bin Wang Department of Meteorology and IPRC University of Hawaii Acknowledging contribution from Q. H. Ding, X. H. Fu, I.-S. Kang, J.-Y. Lee, K. Jin. JJA precipitation, 850 hPa winds, 200hPa STR. MCZ: BOB-SCS-PS.

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495 views • 35 slides
BMRC coupled modelling :

BMRC coupled modelling :

BMRC coupled modelling : Oscar Alves, Guomin Wang, Neville Smith, Aihong Zhong, Faina Tseitkin, Andrew Marshall BMRC Model Development ( NWP, Lilia Deschamps ) BMRC Climate Dynamics ( Rob Colman ) CSIRO Marine Research (OGCM)

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352 views • 25 slides
THE ECMWF Seasonal Forecasting system

THE ECMWF Seasonal Forecasting system

THE ECMWF Seasonal Forecasting system. Overview. OCEANOBS 09 & EUROBRISA Applications most welcome for the concept of End To End Seasonal Forecasting Systems The ECMWF S4 Better skill in the Equatorial and South Atlantic Mixed results everywhere else (large biases) EUROBRISA PROJECT

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391 views • 22 slides
The monsoon-ENSO teleconnection and different ENSO regimes in a flux corrected future climate

The monsoon-ENSO teleconnection and different ENSO regimes in a flux corrected future climate

IPSL/CGAM workshop on Tropical Climate 26-27 May 2005. The monsoon-ENSO teleconnection and different ENSO regimes in a flux corrected future climate. Andrew Turner, Pete Inness, Julia Slingo. Why flux adjust?.

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328 views • 20 slides
Tropical performance of the CCSR Coupled GCM

Tropical performance of the CCSR Coupled GCM

Tropical performance of the CCSR Coupled GCM. Masahide Kimoto Center for Climate System Research University of Tokyo in collaboration with All the CCSR-family members. CCSR Coupled Model. ????????. Atmosphere CCSR/NIES AGCM v5.6 Nakajima et al. (2000) radiation (2 stream DOM/adding)

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284 views • 17 slides
Selective Monotonicity Preservation for Scalar Advection

Selective Monotonicity Preservation for Scalar Advection

Selective Monotonicity Preservation for Scalar Advection. Global FCT, CFL=1. Selective FCT, CFL=4. Selective FCT only applies flux correction near perceived discontinuities, using WENO-like smoothness indicator.

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126 views • 3 slides

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