'Enso' diaporamas de présentation

Mechanisms controlling ENSO: A simple hybrid coupled model study

Mechanisms controlling ENSO: A simple hybrid coupled model study. Cheng-Wei Chang 1 * and Jia-Yuh Yu 2 1. Institute of Geography, Chinese Culture University, Taipei, Taiwan, cwchang@atmos.pccu.edu.tw , +886-2-28610511 ext25705

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ENSO simulation in MIROC: Perspectives toward CMIP5

CLIVAR ENSO WS, Nov 17-19, 2010. ENSO simulation in MIROC: Perspectives toward CMIP5. M. Watanabe 1 , M. Chikira 2 , Y. Imada 1 , M. Kimoto 1 and MIROC modeling team. 1: Atmosphere and Ocean Research Institute (AORI), The Univ. of Tokyo

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Indian Ocean SST Signals in a Tree-Ring Record of Java Drought

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Axel Timmermann F.-F. Jin, J.-S. Kug & S. Lorenz Y. Okumura S.-P. Xie

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Decadal ENSO-like patterns and the modulation of ENSO teelconnections

Decadal ENSO-like patterns and the modulation of ENSO teelconnections. Collaborators. R. Colman, X. Wang, G. Wang, Bureau of Meteorology M. Haylock, Climatic Research Unit, University of East Anglia, U.K. S. McGregor and N. Holbrook, Macquarie University, Sydney.

459 views • 27 slides

ENSO Winter Precipitation (cm/month)

ENSO Winter Precipitation (cm/month). How does ENSO affect Indonesian Precipitation?. ENSO SST anomalies in the eastern and central Tropical Pacific cause an eastward shift in convection from the west Pacific and Indonesia to the central Pacific

475 views • 26 slides

Mike Groenke (Atmospheric Sciences Major)

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The El-Nino Southern Oscillation (ENSO)

The El-Nino Southern Oscillation (ENSO). El Nino Impacts. La Nina Impacts. Outline. History Observed Structure and Evolution What Causes an El-Nino? ENSO Forecasting Global Impacts. ENSO. History In the 1600s, Peruvian fisherman noticed their fish harvests failed

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CO 2 -induced changes in tropical climate as simulated by the GFDL coupled GCMs

CO 2 -induced changes in tropical climate as simulated by the GFDL coupled GCMs. Andrew Wittenberg NOAA/GFDL. CMIP3/AR4 results for future ENSO changes. 1. Enhanced warming of cold tongue - dT/dy change more robust than dT/dx - more stratified ocean & atmosphere

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Presented by Andrew Wittenberg Geophysical Fluid Dynamics Laboratory 17 October 2012

Tropical Climate Change and ENSO. Presented by Andrew Wittenberg Geophysical Fluid Dynamics Laboratory 17 October 2012. NOAA GOES-11 5 Oct 2011 1800 UTC. The Tropics: Firebox of the global circulation. Thompson Higher Education. 2. Projected surface temperature changes.

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Tropical Pacific decadal oscillation driven by the interaction between ENSO and mean state

Tropical Pacific decadal oscillation driven by the interaction between ENSO and mean state. Jung Choi , Soon-Il An Climate Theory Laboratory, Department of Atmospheric Sciences, Yonsei University, Seoul, Korea. Introduction. Fedorov & Philander(2000).

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An Empirical Model of Decadal ENSO Variability

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Coupling of Equatorial Pacific Conditions with Southeast U.S. River Discharge

Coupling of Equatorial Pacific Conditions with Southeast U.S. River Discharge. Lawrence B. Cahoon Dept. of Biology and Marine Biology UNC Wilmington. Correlations – Climate Indices.

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Outline

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ENSO and tropical Pacific metrics for coupled GCMs

ENSO and tropical Pacific metrics for coupled GCMs. Goals : Document the performance of ENSO and tropical simulation in CMIP coupled models. Help better understanding of processes in models and identify new mechanisms

189 views • 7 slides