1. Review of Regional Weather Conditions for Second Fortnight of June 2018
1.2 During this period, there were isolated showers over parts of the northern ASEAN region but wetter weather was observed over coastal areas of Myanmar. In southern Myanmar, heavy rains reportedly triggered floods and landslides during the beginning of the second fortnight. Based on climatology, the wet conditions over coastal Myanmar is typical during this period of the season. Most parts of the Mekong sub-region experienced below-normal to near-normal rainfall, while northern and coastal areas of Myanmar, eastern Cambodia and southern Vietnam received above-normal rainfall.
1.3 In the southern ASEAN region, large scale convergence of winds caused by a circulation west of Borneo brought widespread shower activities over the region. Most areas experienced wetter than usual conditions, except for central Sumatra, central Kalimantan and Java where below-normal rainfall were received.
1.4 The rainfall distribution and the percentage of normal rainfall for the second fortnight of June 2018 are shown in Figures 1 and 2.
1.5 During the second fortnight of June 2018, weather in the region was influenced by Tropical Storm “Gaemi” and Typhoon “Prapiroon” as well. Rainbands associated with “Gaemi” brought widespread showers over parts of the northern ASEAN region, and persistent wet weather over Sumatra, Peninsular Malaysia and Singapore in the southern ASEAN region. Toward the end of June 2018, rain bands from “Prapiroon” also brought widespread showers over most parts of the ASEAN region.
1.6 Prevailing winds over the northern ASEAN region and the South China Sea were weaker than usual and blew predominantly from the southwest or west. Over the southern ASEAN region, easterly to southeasterly winds prevailed. Figure 4 shows the average and anomalous winds at 5000 feet.
1.7 The El Niño-Southern Oscillation (ENSO) remained in the neutral state (neither El Niño nor La Niña). The atmospheric and oceanic indicators of ENSO such as sea surface temperature and trade winds were also indicative of neutral conditions, although the sea surface temperatures in the eastern Pacific Ocean have been observed to be warming slowly.
1.8 The Madden Julian Oscillation (MJO) progressed from Phase 1 to Phase 2 before the signal weakened toward the end of the month. Typically, the MJO in Phases 1 and 2 brings less rainfall over the coastal Myanmar region and the South China Sea, and the MJO in Phase 2 would bring slightly enhanced rainfall around Sumatra and Borneo. In the second fortnight of June 2018, an increase in rainfall was observed along the belt between the Equator and 5°S.