Yuanhong Guan (NUIST, Nanjing, China) Bohua Huang (GMU/COLA)

Slides:



Advertisements
Similar presentations
Dynamical Prediction of the Terrestrial Ecosystem and the Global Carbon Cycle: a 25-year Hindcast Experiment Jin-Ho Yoon Dept. Atmospheric and Oceanic.
Advertisements

ROLE OF THE INDIAN AND ATLANTIC OCEANS ON THE CLIMATE VARIABILITY OF EASTERN AFRICA Charles C. Mutai Kenya Meteorological Department P. O. Box 30259,
Part II: Observed Multi-Time Scale Variability in the Tropical Atlantic Part I: Biases in the NCEP CFS in the Tropical Atlantic Diagnosing CGCM bias and.
Analysis of Eastern Indian Ocean Cold and Warm Events: The air-sea interaction under the Indian monsoon background Qin Zhang RSIS, Climate Prediction Center,
Simulation of the Global ENSO-Tropical Cyclone Teleconnection by a High-Resolution Coupled GCM Ray Bell, Kevin Hodges, Pier Luigi Vidale, Jane Strachan.
Ocean Prediction and Predictability with Focus on Atlantic Goal: Understanding ocean’s role in climate predictability from ISI to decadal scales using.
Indian Monsoon, Indian Ocean dipoles and ENSO Pascal Terray LOCEAN/IPSL, France Fabrice Chauvin CNRM/Météo-France, France Sébastien Dominiak LOCEAN/IPSL,
Assessment of CFSv2 hindcast (seasonal mean) CPC/NCEP/NOAA Jan 2011.
The causes of extreme rainfall in East Africa: insights from observed data and GCMs Emily Black, Julia Slingo and Ken Sperber.
Validation of the NCEP CFS forecasts Suranjana Saha Environmental Modeling Center NCEP/NWS/NOAA/DOC.
The Predictive Skill and the Most Predictable Pattern in the Tropical Atlantic: The Effect of ENSO Zeng-Zhen Hu 1 Bohua Huang 1,2 1 Center for Ocean-Land-Atmosphere.
INTRODUCTION Although the forecast skill of the tropical Pacific SST is moderate due to the largest interannual signal associated with ENSO, the forecast.
Opening title page On the Delayed Atmospheric Response to ENSO SST Hui Su **, J. David Neelin ** and Joyce E. Meyerson * Dept. of Atmospheric Sciences.
Response of the Atmosphere to Climate Variability in the Tropical Atlantic By Alfredo Ruiz–Barradas 1, James A. Carton, and Sumant Nigam University of.
Contemporaneous and Antecedent Links of Atlantic and Pacific Circulation Features with North American Hydroclimate: Structure and Interannual Variability.
Objects Basic Research (Hypotheses and Understanding) Applied Research (Applications and Tools) Joint effects of ENSO and SST anomalies in different ocean.
Modes of Pacific Climate Variability: ENSO and the PDO Michael Alexander Earth System Research Lab michael.alexander/publications/
Impact of Sea Surface Temperature and Soil Moisture on Seasonal Rainfall Prediction over the Sahel Wassila M. Thiaw and Kingtse C. Mo Climate Prediction.
Forecasting the MJO with the CFS: Factors affecting forecast skill of the MJO over the Maritime Continent Augustin Vintzileos CPC/NCEP – CICS/ESSIC, University.
THE INDIAN OCEAN DIPOLE AND THE SOUTH AMERICAN MONSOON SYSTEM Anita Drumond and Tércio Ambrizzi University of São Paulo São Paulo, 2007
Air-sea heat fluxes and the dynamics of intraseasonal variability Adam Sobel, Eric Maloney, Gilles Bellon, Dargan Frierson.
The Seasonal Footprinting Mechanism in CFSv2: Simulation and Impact on ENSO Prediction Kathy Pegion University of Colorado/CIRES & NOAA/ESRL/PSD Michael.
Sara Vieira Committee members: Dr. Peter Webster
Interannual Variation in the Seasonal Northward Movement of the Baiu Front in the Western North Pacific Tomohiko Tomita Kumamoto University / FRCGC, JAMSTEC.
1 Global Ocean Monitoring: Recent Evolution, Current Status, and Predictions Prepared by Climate Prediction Center, NCEP September 7, 2007
Consolidated Seasonal Rainfall Guidance for Africa, Jan 2013 Initial Conditions Summary Forecast maps Forecast Background – ENSO update – Current State.
Improved ensemble-mean forecast skills of ENSO events by a zero-mean stochastic model-error model of an intermediate coupled model Jiang Zhu and Fei Zheng.
The Influence of Tropical-Extratropical Interactions on ENSO Variability Michael Alexander NOAA/Earth System Research Lab.
The role of the basic state in the ENSO-monsoon relationship and implications for predictability Andrew Turner, Pete Inness, Julia Slingo.
13 March 20074th C20C Workshop1 Interannual Variability of Atmospheric Circulation in C20C models Simon Grainger 1, Carsten Frederiksen 1 and Xiagou Zheng.
Mechanisms of drought in present and future climate Gerald A. Meehl and Aixue Hu.
1 Daily modes of the South Asian monsoon variability and their relation with SST Deepthi Achuthavarier Work done with V. Krishnamurthy Acknowledgments.
A Stochastic Model of the Madden-Julian Oscillation Charles Jones University of California Santa Barbara 1 Collaboration : Leila Carvalho (USP), A. Matthews.
El Nino, Indian Ocean dynamics and extremely rainy years in East Africa Emily Black, Julia Slingo and Ken Sperber Introduction Rainfall.
Zonal Flow Variability Linking the ENSO/Monsoon Systems Step back to the atmospheric response to El Niño –attempt to interpret the zonal flow variability.
Variations in the Activity of the Madden-Julian Oscillation:
CFSv2 Research at COLA: Understanding the effect of air-sea coupling in Asian-Pacific monsoon prediction and improving sea ice simulation for climate study.
El Niño Forecasting Stephen E. Zebiak International Research Institute for climate prediction The basis for predictability Early predictions New questions.
1 The Impact of Mean Climate on ENSO Simulation and Prediction Xiaohua Pan Bohua Huang J. Shukla George Mason University Center for Ocean-Land-Atmosphere.
Role of the Gulf Stream and Kuroshio-Oyashio Systems in Large- Scale Atmosphere-Ocean Interaction: A Review Young-oh Kwon et al.
1 Opposite phases of the Antarctic Oscillation and Relationships with Intraseasonal to Interannual Activity in the Tropics during the Austral Summer (submitted.
Modes of variability and teleconnections: Part II Hai Lin Meteorological Research Division, Environment Canada Advanced School and Workshop on S2S ICTP,
MJO Research at Environment Canada Meteorological Research Division Environment Canada Hai Lin Trieste, Italy, August 2008.
Persistent Atmospheric and Oceanic Anomalies in the North Atlantic Ocean from Summer 2009 to Summer 2010 Zeng-Zhen Hu and Arun Kumar Climate Prediction.
Advances in Fundamental Climate Dynamics John M. Wallace et al.
Sources of global warming of the upper ocean on decadal period scales Warren B. White 2010/05/18 Pei-yu Chueh.
MICHAEL A. ALEXANDER, ILEANA BLADE, MATTHEW NEWMAN, JOHN R. LANZANTE AND NGAR-CHEUNG LAU, JAMES D. SCOTT Mike Groenke (Atmospheric Sciences Major)
Influence of the state of the Indian Ocean Dipole on the following year’s El Niño Izumo et al., 2010.
1 An Assessment of the CFS real-time forecasts for Wanqiu Wang, Mingyue Chen, and Arun Kumar CPC/NCEP/NOAA.
Influence of Subtropical Air-Sea Interaction on the Multidecadal AMOC Variability in the NCEP CFS Bohua Huang 1, Zeng-Zhen Hu 2, Edwin K. Schneider 1 Zhaohua.
Observed influence of North Pacific SST anomalies on the atmospheric circulation Claude Frankignoul and Nathalie Sennéchael LOCEAN/IPSL, Université Pierre.
Southern Hemisphere extra-tropical forcing: a new paradigm for ENSO Pascal Terray, 2010 R 陳漢卿.
Dynamic Climatology Presentation Speaker : Pei-Yu Chueh Date : 2011/01/10.
1 A review of CFS forecast skill for Wanqiu Wang, Arun Kumar and Yan Xue CPC/NCEP/NOAA.
ESSL Holland, CCSM Workshop 0606 Predicting the Earth System Across Scales: Both Ways Summary:Rationale Approach and Current Focus Improved Simulation.
Equatorial Atlantic Variability: Dynamics, ENSO Impact, and Implications for Model Development M. Latif 1, N. S. Keenlyside 2, and H. Ding 1 1 Leibniz.
Summer Monsoon – Global Ocean Interactions Ben Kirtman George Mason University Center for Ocean-Land-Atmosphere Studies Acknowledgements: Randy Wu and.
Seasonal Forecast of Antarctic Sea Ice
Seasonal Climate Outlook of China in Summer 2017
ENSO Frequency Cascade and Implications for Predictability
The role of mid and high latitude air-sea interactions
Alfredo Ruiz-Barradas, and Sumant Nigam
To infinity and Beyond El Niño Dietmar Dommenget.
Dynamics of ENSO Complexity and Sensitivity
ENSO and its impact on eastern/southern African climate:
The Climate System TOPICS ENSO Impacts Seasonal Climate Forecasts
Predictability of Indian monsoon rainfall variability
Case Studies in Decadal Climate Predictability
ENSO Outlook in spring/summer 2013 Beijing Climate Center/CMA
Ocean/atmosphere variability related to the development of tropical Pacific sea-surface temperature anomalies in the CCSM2.0 and CCSM3.0 Bruce T. Anderson,
Presentation transcript:

Mechanism and Predictability of South Pacific Dipole Mode in NCEP CFSv2 Yuanhong Guan (NUIST, Nanjing, China) Bohua Huang (GMU/COLA) Jieshun Zhu (COLA) Zeng-Zhen Hu (CPC/NCEP/NOAA) James L. Kinter III (GMU/COLA)

References Guan, Y., J. Zhu, B. Huang, Z.-Z. Hu and J. L. Kinter, 2013a: South Pacific Ocean Dipole: A predictable mode on multi-seasonal time scales. J. Climate, accepted. Guan, Y., B. Huang, J. Zhu, Z.-Z. Hu and J. L. Kinter, 2013b: Interannual variability of the South Pacific Ocean in observations and simulated by the NCEP Climate Forecast System, version 2. Climate Dynamics, submitted.

Unique Character of Southern Ocean SSTA Open Ocean Formation CFSv2 reproduces the STD distribution of the observed SSTA Overestimate and shift in South Pacific

South Pacific Dipole (SPD) Southern Subtropical Indian Ocean Dipole (SSID) South Pacific Dipole (SPD) Southern Subtropical Atlantic Dipole (SSAD)

South Pacific Dipole (SPD) Mode SPD is highly coherent with ENSO in both observations and CFSv2

Lifecycle of Composite SPD Event

Regional Air-Sea Feedback Surface Heat Flux, ΔQ Monthly climatological mixed layer depth. In developing phase,

Influence of wind anomalies is significant Regional Air-Sea Feedback Morioka et al. (2010, 2012) Influence of wind anomalies is significant

Where the wind anomalies come from?

Atmospheric Tele-Connection Atmospheric anomalies in South Pacific are characterized by Pacific-South American (PSA) Pattern (Mo and Higgins 1998)

Connection to ENSO Heating Sources

SPD Prediction Skill and Predictability

SPD

SPD

SPD

Summary SPD is the leading SSTA pattern in South Pacific during summer. CFSv2 simulates SPD realistically, including its lifecycle, seasonality and ENSO connection. SPD events are initiated by wind-induced surface latent heat flux anomalies. Persistent mixed layer depth anomalies enhance SPD. ENSO-forced PSA wave train generates wind perturbations over South Pacific for SPD. CFSv2 shows high predictive skill of SPD mode, due to its good prediction of ENSO and its PSA tele-connection. Seasonal dependence: An austral “fall barrier” of prediction skill appears near New Zealand. Extratropical SPD sources need further investigation.