Niño SST Indices are based on the average of SST anomalies across the given regions: Niño 1+2 (0-10S, 90W-80W), Niño 3 (5N-5S, 150W-90W), Niño 3.4 (5N-5S, 170W-120W) and Niño 4 (5N-5S, 160E-150W). These indices are used to monitor the conditions in the Tropical Pacific for the occurrence of El Niño or La Niña.
Below average sea surface temperature anomalies (SSTAs) across the central and eastern equatorial Pacific strengthened (-0.5ºC to -1.5ºC) for the month, however, Niño 4 were near to slightly cooler than average. In the western Pacific near the Maritime continent, near to above average SSTAs were observed (0°C to > 0.5°C).
The Indian Ocean Dipole mode Index (DMI) is defined as the difference between the SST anomalies (ºC) of Western (10ºS-10ºN & 50ºE-70ºE) and Eastern (10ºS-0ºN & 90ºE-110ºE) Equatorial Indian Ocean regions (WEST-EAST). The DMI values represent the intensity of the Indian Ocean Dipole (IOD); DMI values above +0.4 °C is referred as the positive IOD, DMI values below −0.4 °C is referred as the negative IOD and DMI values between +0.4 °C and -0.4 °C is referred as the neutral IOD.
IOD value for the month is at neutral levels, as SSTs in the eastern equatorial Indian Ocean were observed to be slightly warmer than the western equatorial Indian Ocean.