Changes in the El Nino s spatial structure under global warming. Sang-Wook Yeh Hanyang University, Korea
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1 Changes in the El Nino s spatial structure under global warming Sang-Wook Yeh Hanyang University, Korea
2 Changes in El Nino spatial structure Yeh et al. (2009) McPhaden et al. (2009)
3 Why the spatial structure of El Nino matters? Impact and teleconnections - Central Pacific El Nino and decadal climate change in the North Pacific Ocean (Di Lorenzo et al. 2010, Nature Geoscience) - Influence of El Nino Modoki on spring rainfall over South China (Feng et al. 2011, JGR) - Effects of El Nino Modoki on winter precipitation in Korea (Kim et al. 2012, Climate. Dyn.) - Teleconnections associated with the intensification of the Australia monsoon during the El Nino Modoki events (Taschetto et al. 2010) - Central Pacific El Nino, the Subtropical Bridge and Eurasian Climate (2012, GRL) - On the impact of central Pacific warming events on Atlantic tropical storm activity (Lee et al., 201 0, GRL) - Different El Nino Types and Tropical cyclone landfall in East Asia (Wang et al. 2013, J. Climate)
4 Fundamental question Which mechanisms are responsible for the changes in the spatial structure of El Nino (in climate models)? - Air-sea coupling strengths in the eastern Pacific - Bjerknes feedback in the tropical Pacific - Tropical Pacific mean state
5 Air-sea coupling strengths in the eastern Pacific 1 ERSST ( ) CMIP3 Historical run ( ) CMIP5 Historical run ( )
6 Air-sea coupling strengths in the eastern Pacific 2
7 Air-sea coupling strengths in the eastern Pacific 3 Linear trends of SST in the CMIP 3 MME Linear trends of SST in the CMIP 5 MME
8 Air-sea coupling strengths in the eastern Pacific 4 The SSTA variability in the eastern tropical Pacific can be largely ch anged by air sea coupled processes (Ch oi et al. 2009). A greater amount of warming in the easter n tropical Pacific relative to the western tro pical Pacific in CMIP5 can amplify the SST A variability in the eastern tropical Pacific t hrough enhanced air-sea coupled processes
9 Changes in El Nino spatial structure. An enhancement of air-sea coupling strengths over the eastern P acific may contribute to increase the SSTA variability in the eastern P acific Changes in the air-sea coupli ng strengths over the eastern Pacific CMIP3 Historical run CMIP5 Historical run Changes in the spatial structu re of ENSO
10 Bjerknes feedback in the tropical Pacific 1 There exist physical feedback processes that lead to changes in ENS O amplitude. These processes are associated with the changes in ther mocline feedback and surface zonal advective feedback, which are als o associated with a Bjerknes feedback : Anomalous zonal wind stress over the central Pacific : the east minus west anomalous SST difference.
11 Bjerknes feedback in the tropical Pacific 2 Archive 21 CMIP5 Historical run 21 CMIP3 Historial run Modeling Group CMIP ID Integration period CSIRO-BOM ACCESS year BCCR BCC-CSM year CCCMA CanESM2 156 year NCAR CCSM4 156 year Météo-France CNRM-CM5 156 year CSIRO-QCCCE CSIRO-Mk year LASG FGOALS-g2 110 year NOAA / GFDL GFDL-CM3 145 year NOAA / GFDL GFDL-ESM2G 145 year NOAA / GFDL GFDL-ESM2M 145 year NASA / GISS GISS-E2-R 156 year Hadley Centre / Met Office HadGEM2-CC 145 year Hadley Centre / Met Office HadGEM2-ES 145 year INM INM-CM4 156 year IPSL IPSL-CM5A-LR 156 year IPSL IPSL-CM5A-MR 156 year CCSR, JAMSTEC MIROC5 156 year CCSR, JAMSTEC MIROC-ESM 156 year MPI-M MPI-ESM-LR 156 year MRI MRI-CGCM3 156 year NCC NorESM1-M 156 year BCCR BCCR-BCM year CCCMA CCCMA_CGCM_ year CCCMA CCCMA_CGCM_3.1_t year Météo-France CNRM-CM3 140 year CSIRO-QCCCE CSIRO-Mk year CSIRO-QCCCE CSIRO-Mk year NOAA / GFDL GFDL-CM year NOAA / GFDL GFDL-CM year LASG IAP_FGOALS-g year INGV INGV_ECHAM4 100 year INM INM-CM year IPSL IPSL-CM4 141 year CCSR, JAMSTEC MIROC3.2_HIRES 101 year CCSR, JAMSTEC MIROC3.2_MEDRES 141 year University of Bonn, KMA MIUB_ECHO-G 150 year MRI MRI-CGCM2.3.2a 150 year Hadley Centre / Met Office UKMO-HadCM3 140 year Hadley Centre / Met Office UKMO-HadGEM1 140 year MPI MPI_ECHAM5 140 year NCAR NCAR-CCSM year NCAR NCAR_PCM1 110 year
12 Bjerknes feedback in the tropical Pacific 3 (a) 21 CMIP3 MME Historical run (b) 21 CMIP5 MME Historical run
13 Changes in the Bjerknes feedback in the tropical Pacific 4 Scatter plots between SSTA S.D. in the eastern Pacific and Alpha in the 21 CMIP3 and CMIP5 models, respectively.
14 Changes in the Bjerknes feedback in the tropical Pacific 5 21 CMIP3 MME 21 CMIP5 MME
15 Changes in El Nino spatial structure The Bjerknes feedback plays a role to influence the variability of SST A in the eastern Pacific among CMIP5 CGCMs, but not among CMI P3 CGCMs. Changes in the role of Bjerk nes feedback in the tropical P acific basin CMIP3 Historical run CMIP5 Historical run Changes in the spatial structu re of El Nino
16 Tropical Pacific mean state 1 CMIP5 Historical run: Moderate El Nino Moderate El Nino Strong El Nino Strong El Nino Model # Model 1 CanESM2 2 CCSM4 3 CESM1-CAM5 4 CNRM-CM5 5 CSIRO-Mk GISS-E2-R 7 HadGEM2-ES 8 IPSL-CM5A-LR 9 MPI-ESM-LR 10 NorESM1-M - Historical run: CMIP5 RCP 4.5 run: RCP 4.5 run:
17 Tropical Pacific mean state 2 Changes in the moderate El Nino along with a positive and negative PDO Negative PDO phase in the Histor ical run Positive PDO phase in the Histor ical run Negative PDO phase in the RCP4. 5 run Positive PDO phase in the RCP4. 5 run
18 Tropical Pacific mean state 3 Tropical Pacific mean state under a negative phase of PDO An enhancement of zonal advective feedback processes
19 Changes in El Nino spatial structure. It is found that there exist the changes in spatial structure of El Nino under a negative phase of PDO (mostly due to moderate El Ni no ) from the Historical run to the RCP 4.5 run Tropical Pacific mean state Historical run RCP4.5 run Changes in the spatial structu re of El Nino
20 Hypothesis Global Warming - Air-sea coupling strengths in the eastern Pacific - Bjerknes feedback in the tropical Pacific - Tropical Pacific mean state Changes in El Nino spatial structure
21 Thank you
22 Changes in the air-sea coupling strengths in the eastern Pacific 5 Before the late 1990 After the late 1990 Precipitation Regress ion Coefficient over the NINO3 region wrt NINO3 SST ind ex Before the late After the late
23 Mechanism of frequent occurrence of CP El Nino.. the recent predominance of standing CPW(Central Pacific Warmin g) arises from a dramatic decadal change characterized by a grand La Nina-like background pattern and strong divergence in the central Pa cific atmospheric boundary layer (Xiang et al. 2012)..Mean state change (i.e., a cooling (warming) over tropical eastern (w estern) Pacific) is associated with more frequent occurrence of CP El Nino during A shift to the La Nina-like interdecadal me an state is responsible for more frequent occurrence of CP-type El N ino (Chung and Li, 2013)
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