Journal of Tropical Oceanography ›› 2019, Vol. 38 ›› Issue (2): 32-42.doi: 10.11978/2018061CSTR: 32234.14.2018061
• Marine Meteorology • Previous Articles Next Articles
Zhujun FANG1(), Hai ZHI1, Pengfei LIN2,3(), Xiang WEI1
Received:
2018-06-04
Revised:
2018-07-28
Online:
2019-03-20
Published:
2019-04-15
Supported by:
CLC Number:
Zhujun FANG, Hai ZHI, Pengfei LIN, Xiang WEI. Distinguishing two types of El Niño in the Tropical Pacific using key region sea surface salinity index[J].Journal of Tropical Oceanography, 2019, 38(2): 32-42.
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Fig. 3
Horizontal distributions of lead and lag correlation coefficients between the time series of SSSA on each grid and EMI index. SSSA leading SSTA by four months to one month is shown in (a, b, c, d); the zero lead month of SSSA and SSTA is shown in (e); SSSA lagging SSTA by 1~4 months is shown in (f, g, h, i)"
Fig. 4
Horizontal distributions of lead and lag correlation coefficients between the time series of SSSA on each grid and Ni?o3 index. SSSA leading SSTA by four months to one month is shown in (a, b, c, d); the zero lead month of SSSA and SSTA is shown in (e); SSSA lagging SSTA by 1-4 months is shown in (f, g, h, i)"
Tab. 1
The temporal and spatial correlation coefficients between the CP/EP El Ni?o and SCPI/SEPI index, and the four EOF modes in the tropical Pacific"
类型 | 空间相关 | 时间相关 | ||
---|---|---|---|---|
CP | EP | CP | EP | |
SCPI | 0.73 | 0.15 | 0.70 | 0.17 |
SEPI | 0.15 | 0.50 | 0.11 | 0.69 |
PC1 | 0.30 | 0.56 | 0.31 | 0.31 |
PC2 | 0.08 | 0.76 | 0.22 | 0.43 |
PC3 | 0.69 | 0.34 | 0.58 | 0.09 |
PC4 | 0.29 | -0.10 | 0.17 | -0.14 |
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