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.
Sea surface temperature anomalies (SSTAs) across the tropical Pacific have weakened during the month (~ -0.5 to -1.0°C). However in the western Pacific, SSTAs were near to warmer than average with 0.5°C to > 2.0 °C anomaly located in the northeastern part of the Maritime Continent, while on the western side, near to slightly below average SSTAs were observed.
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.
The average IOD value for March was slightly positive but still within neutral level as SSTAs across most of the equatorial Indian Ocean were observed to be near average.