Journal of Tropical Oceanography ›› 2026, Vol. 45 ›› Issue (3): 83-94.doi: 10.11978/2025113CSTR: 32234.14.2025113
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LI Yuzhen1,2(
), MENG Xiangfeng1,2(
)
Received:2025-07-21
Revised:2025-10-19
Online:2026-05-10
Published:2026-05-28
Contact:
MENG Xiangfeng. email: mengxf@ouc.edu.cn
Supported by:CLC Number:
LI Yuzhen, MENG Xiangfeng. Differences in subsurface nonlinear dynamical heating contributions between two types of El Niño under different IPO phases[J].Journal of Tropical Oceanography, 2026, 45(3): 83-94.
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Fig. 1
Spatial modes and time series of the IPO (1980-2020). (a) Spatial mode distribution of the IPO; (b) time series of the IPO index; (c) SSTA distribution during peak months of El Niño events in positive IPO phases; (d) SSTA distribution during peak months of El Niño events in negative IPO phases"
Tab. 1
Classification of spatial types of El Niño events from 1980 to 2017"
| 序号 | 年份 | 方法 | 结果 | ||
|---|---|---|---|---|---|
| NWP/NCT | EMI | Niño3/4 | |||
| 1 | 1982/1983 | EP | EP | EP | EP |
| 2 | 1986/1987 | EP | EP | EP | EP |
| 3 | 1991/1992 | EP | CP | EP | EP |
| 4 | 1994/1995 | CP | CP | CP | CP |
| 5 | 1997/1998 | EP | EP | EP | EP |
| 6 | 2002/2003 | CP | CP | CP | CP |
| 7 | 2004/2005 | CP | CP | CP | CP |
| 8 | 2006/2007 | CP | EP | CP | CP |
| 9 | 2009/2010 | CP | CP | CP | CP |
| 10 | 2015/2016 | EP | EP | EP | EP |
Fig. 2
Spatial modes and time series of EP-type and CP-type El Niño events. (a, c) Spatial distributions of SSTA for EP-type and CP-type El Niño events, respectively; (b, d) time series of the E-index and C-index, where the black line represents the E-index and C-index, the blue line denotes the IPO index, and the red line shows the 5-year moving average of the E-index and C-index"
Fig. 3
Hovmöller diagrams of SSTA, thermocline depth anomalies, and sea surface zonal current anomalies. (a, b) Hovmöller diagrams of SSTA during El Niño events; (c, d) Hovmöller diagrams of thermocline depth anomalies during El Niño events; (e, f) Hovmöller diagrams of sea surface zonal current anomalies during El Niño events. (a, c, e) show composite results for El Niño events during positive IPO phases; (b, d, f) show composite results for El Niño events during negative IPO phases"
Fig. 4
Heat budget analysis for the mixed layer and subsurface layer in the Niño4 and Niño3 regions. (a, b) Heat budget terms for the mixed layer and subsurface layer in the Niño4 region; (c, d) heat budget terms for the mixed layer and subsurface layer in the Niño3 region. Red bars represent CP-type El Niño events, and blue bars denote EP-type El Niño events. The three bars correspond to the mean values for the 3 months preceding the peak month, the peak month itself, and the 3 months following the peak month; In the horizontal coordinate, EP and CP represent EP-type El Niño events and CP-type El Niño events respectively while -TH, -ZA, and -NDH correspond to the TH feedback, ZA feedback, and NDH feedback within EP-type/CP-type El Niño events"
Fig. 5
Time series of Niño indices and subsurface NDH values from 1980 to 2022. (a) Niño3 index and subsurface NDH values in the Niño3 region; (b) Niño3.4 index and subsurface NDH values in the Niño3.4 region; (c) Niño4 index and subsurface NDH values in the Niño4 region; The corresponding regions are specifically defined as depths from 50 to 200 meters, latitudes from 5°S to 5°N, with longitudes as follows: a: 150°W-90°W, b: 170°W-120°W, c: 160°E-150°W"
Fig. 6
Long-term averages of NDH and its components (NDHX, NDHY, NDHZ) between 1°S and 1°N. (a, b) Vertical profiles of NDH; (c, d) vertical profiles of NDHX; (e, f) vertical profiles of NDHY; (g, h) vertical profiles of NDHZ. (a, c, e, g) show long-term averages for positive IPO phases; (b, d, f, h) show long-term averages for negative IPO phases. Black lines indicate thermocline depths"
Fig. 7
Regression coefficient distributions of the thermocline depth difference (TDD) between the Niño4 and Niño3 regions and SST. (a) Spatial distribution of regression coefficients (1980-2020); (b) time series of the TDD between the Niño4 and Niño3 regions and the Niño3.4 index; (c) spatial distributions of regression coefficients for 1980-1999; (d) spatial distributions of regression coefficients for 2000-2020. Dotted areas pass the significance test at the 90% confidence level (α = 0.1)"
Fig. 8
Vertical profiles of SSTA, zonal current anomalies, and upwelling anomalies during the development phase of El Niño events under different IPO phases. (a, b) Vertical profiles of SSTA; (c, d) vertical profiles of zonal current anomalies; (e, f) vertical profiles of upwelling anomalies. (a, c, e) are mean profiles during the development phase of El Niño events under positive IPO phases; (b, d, f) are mean profiles during the development phase of El Niño events under negative IPO phases"
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