Temporal evolution of sea surface temperature anomalies in the central equatorial Pacific (Niño 3.4 region average), illustrating the ENSO-associated variability.
Standard deviation of sea surface temperature anomalies in the central equatorial Pacific (Niño 3.4 region average), representing the amplitude of variability.
Ratio of winter to spring standard deviation of sea surface temperature anomalies in the central equatorial Pacific, illustrating the seasonal timing of SSTA.
Skewness of sea surface temperature anomalies in the central equatorial Pacific, illustrating the expected asymmetry where positive SSTA values should typically be larger than negative SSTA values (usually close to 0).
Temporal evolution of sea surface temperature anomalies in the central equatorial Pacific (Niño 3.4 region average), illustrating the ENSO-associated variability. |
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Ratio of winter to spring standard deviation of sea surface temperature anomalies in the central equatorial Pacific, illustrating the seasonal timing of SSTA. |
download |
references |
extra data citation |
provenance
Skewness of sea surface temperature anomalies in the central equatorial Pacific, illustrating the expected asymmetry where positive SSTA values should typically be larger than negative SSTA values (usually close to 0). |
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references |
extra data citation |
provenance
Width of the zonal location of maximum (minimum) SSTA during all El Niño (La Niña) events, illustrating the 'diversity' of ENSO events. |
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references |
extra data citation |
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Temporal evolution of sea surface temperature anomalies in the central equatorial Pacific (Niño 3.4 region average), illustrating the ENSO-associated variability. |
download |
references |
extra data citation |
provenance
Ratio of winter to spring standard deviation of sea surface temperature anomalies in the central equatorial Pacific, illustrating the seasonal timing of SSTA. |
download |
references |
extra data citation |
provenance
Skewness of sea surface temperature anomalies in the central equatorial Pacific, illustrating the expected asymmetry where positive SSTA values should typically be larger than negative SSTA values (usually close to 0). |
download |
references |
extra data citation |
provenance
Width of the zonal location of maximum (minimum) SSTA during all El Niño (La Niña) events, illustrating the 'diversity' of ENSO events. |
download |
references |
extra data citation |
provenance