PC34B:
El Niño–Southern Oscillation (ENSO) Diversity in a Changing Climate III Posters


Session ID#: 11498

Session Description:
ENSO events differ in amplitude, spatial pattern, and temporal evolution. These event-to-event variations are difficult to predict and can result in markedly different global impacts. Moreover, tropical Pacific interannual variability appears to undergo decadal/interdecadal variations, which may obscure the detection of possible ENSO changes associated with global warming. In this session we welcome contributions that target the US CLIVAR goal of advancing our understanding of the origin, dynamics, impacts, and predictability of all aspects of ENSO diversity in a changing climate, using observations, theory, model simulations, as well as paleoclimate reconstructions. The unusual evolution of the 2014-2015 El Niño is a recent example of this diversity, and studies aimed at elucidating the physical processes underlying that event are strongly encouraged. We also welcome studies that clarify how model biases contribute to the diversity of ENSO representation among model simulations of past, present, and future climates, as well as research into how to reduce or otherwise cope with those biases.
Primary Chair:  Antonietta Capotondi, NOAA /ESRL, Physical Sciences Division, Boulder, CO, United States; University of Colorado, CIRES, Boulder, CO, United States
Chairs:  Michael J McPhaden, NOAA Seattle, Seattle, WA, United States and Andrew Thorne Wittenberg, NOAA Princeton, Princeton, NJ, United States
Moderators:  Andrew Thorne Wittenberg, Geophysical Fluid Dynamics Laboratory, Princeton, NJ, United States, Antonietta Capotondi, NOAA /ESRL, Physical Sciences Division, Boulder, CO, United States and Michael J McPhaden, NOAA Seattle, Seattle, WA, United States
Student Paper Review Liaisons:  Antonietta Capotondi, NOAA /ESRL, Physical Sciences Division, Boulder, CO, United States and Andrew Thorne Wittenberg, Geophysical Fluid Dynamics Laboratory, Princeton, NJ, United States
Index Terms:

1616 Climate variability [GLOBAL CHANGE]
4522 ENSO [OCEANOGRAPHY: PHYSICAL]
Co-Sponsor(s):
  • A - Air-sea Interactions and Upper Ocean Processes
  • HI - Human Use and Impacts
  • PO - Physical Oceanography/Ocean Circulation
  • TE - Tropical and Equatorial Environments

Abstracts Submitted to this Session:

 
Spatial Correlation Analysis of Niño3.4 SST with Western North America Hydroclimate (86989)
Joshua Paul Heyer1, Simon Brewer2, Jacqueline J Shinker3 and Andrea Brunelle1, (1)University of Utah, Geography, Salt Lake City, UT, United States, (2)University of Utah, Department of Geography, Salt Lake City, UT, United States, (3)Universty of Wyoming, Geography, Laramie, WY, United States
 
PREDICTABILITY OF EAST AFRICAN RAINFALL BASED ON EL NĨNO-SOUTHERN OSCILLATION (91954)
Joshua Ndiwa Ngaina1, Bethwel Kipkoech Mutai1, Hussein Gadain2 and Nzioka Muthama1, (1)University of Nairobi, Meteorology, Nairobi, Kenya, (2)Food and Agriculture Organization of the United Nations, Somalia Water and Land Information Management, Nairobi, Kenya
 
Different Responses of Sea Surface Temperature in the South China Sea to Various El Niño Events during Boreal Autumn (88808)
Xin Wang, SCSIO South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou, China, Wei Tan, First Institute of Oceanography, State Oceanic Administration, Guangzhou, China, Weiqiang Wang, South China Sea Institute of Oceanology, Chinese Academy of Sciences, State Key Laboratory of Tropical Oceanography, Guangzhou 510301, China and Chunzai Wang, NOAA Miami, Miami, FL, United States
 
The Atlantic as a Driver of the Multidecadal ENSO-Tropical Pacific Annual Cycle Relationship (89163)
Aaron F Z Levine, NOAA Pacific Marine Environmental Laboratory, Seattle, WA, United States and Michael J McPhaden, NOAA Seattle, Seattle, WA, United States
 
Global Warming Attenuates the Tropical Atlantic-Pacific Teleconnection (87581)
Fan Jia, CSIRO, Oceans and Atmosphere Flagship, Aspendale, Australia; Institute of Oceanology, Chinese Academy of Sciences, Key Laboratory of Ocean Circulation and Wave, Qingdao, China
 
Interannual Variability in the Global Meridional Overturning Circulation Dominated by Pacific Variability: Possible Implications for ENSO Variability (93736)
Neil F Tandon, University of Toronto, Department of Physics, Toronto, ON, Canada, Paul J Kushner, University of Toronto, Toronto, ON, Canada, Mark A Cane, Lamont -Doherty Earth Observatory, Palisades, NY, United States and Oleg Saenko, Canadian Centre for Climate Modelling and Analysis, Victoria, BC, Canada
 
Salinity Variations in the Equatorial Pacific during the 2014-15 El Niño (87055)
Caroline Mary Corbett and Subrahmanyam Bulusu, University of South Carolina Columbia, Columbia, SC, United States
 
Impact of Lateral Mixing in the Ocean on El Nino in Fully Coupled Climate Models (89833)
Alexandria Russell1, Anand Gnanadesikan1, Marie-Aude Sabine Pradal2 and Ryan P Abernathey3, (1)Johns Hopkins University, Earth and Planetary Sciences, Baltimore, MD, United States, (2)Johns Hopkins University, Baltimore, MD, United States, (3)Lamont -Doherty Earth Observatory of Columbia University, Palisades, NY, United States
 
Response of the Tropical Pacific Ocean to El Niño versus Global Warming (89200)
Fukai Liu, Ocean University of China, Qingdao, China, Yiyong Luo, Ocean University of China, Physical Oceanography Laboratory/CIMST, Qingdao, China and Jian Lu, Pacific Northwest National Laboratory, Richland, WA, United States
 
Rectification of the intraseasonal wind forcing on ENSO and the interannual long equatorial waves (88594)
Xia Zhao1, Dongliang Yuan2, Jing Wang1 and Hailong Liu3, (1)Institute of Oceanology, Chinese Academy of Sciences, Qingdao, China, (2)Institute of Oceanography, Chinese Academy of Sciences, China, (3)IAP, CAS, Beijing, China
 
The Role of Reversed Equatorial Zonal Transport in Terminating an ENSO Event (90069)
Han-Ching Chen, University of Hawaii at Manoa, Atmospheric Sciences, Honolulu, HI, United States; George Mason University, AOES, Fairfax, VA, United States, Zeng-Zhen Hu, Climate Prediction Center, NCEP/NOAA, College Park, MD, United States, Bohua Huang, George Mason University, Fairfax, VA, United States and Chung Hsiung Sui, National Taiwan University, Atmospheric Sciences, Taipei, Taiwan
 
Modulation of Bjerknes feedback on the decadal variations in ENSO predictability (90884)
Fei Zheng, Institute of Atmospheric Physics, Beijing, China
 
Modulation of cloud radiative effect on the strength asymmetry in two types of El Niño events (91031)
Xianghui Fang1, Fei Zheng1,2 and Jiang Zhu1, (1)Institute of Atmospheric Physics, Beijing, China, (2)Institute of Atmospheric Physics, International Center for Climate and Environment Sciences, Beijing, China
 
Response of the Equatorial Pacific Ocean to A Uniform Energy Flux Forcing in A Fully Coupled Atmosphere-Ocean GCM (88578)
Yiyong Luo, Ocean University of China, Physical Oceanography Laboratory/CIMST, Qingdao, China, Fukai Liu, Ocean University of China, Qingdao, China and Jian Lu, Pacific Northwest National Laboratory, Richland, WA, United States
 
Assessing the 21st century shift of ENSO variability (87796)
Cong Guan, NOAA Pacific Marine Environmental Laboratory, Seattle, WA, United States; Institute of Oceanology, Chinese Academy of Sciences, Qingdao, China and Michael J McPhaden, NOAA Seattle, Seattle, WA, United States
 
CMIP5 Projections of Two Types of El Niño and Their Related Tropical Precipitation in the 21st Century (88543)
Kang Xu, South China Sea Institute of Oceanology, Chinese Academy of Sciences, State Key Laboratory of Tropical Oceanography, Guangzhou, China, Chi-Yung Tam, The Chinese University of Hong Kong, Earth System Science (ESSC), Hong Kong, Hong Kong, Congwen Zhu, Chinese Academy of Meteorological Sciences, Institute of Climate Systems, Beijing, China and Weiqiang Wang, South China Sea Institute of Oceanology, Chinese Academy of Sciences, State Key Laboratory of Tropical Oceanography, Guangzhou 510301, China