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In May or June as the rain-bearing southerly monsoon winds arrive the flow begins to increase, with an especially rapid increase in the eastern and northern highlands.
The low rainfall is because the southerly monsoon flow is weakened in this season.
The location also subjects the area to the northward and southward oscillation of the inter-tropical convergence zone (ITCZ) and associated southerly monsoon winds (Sultan and Janicot 2000; Molua and Lambi 2006).
An East Asian summer monsoon (EASM) precipitation zone is formed by the convergence of a westerly flow to the north of the Tibetan Plateau and a southerly monsoon flow over eastern China, which gradually moves northward from South China and reaches northern China in late July (Qian and Lee 2000).
Consistent with the associated large-scale pressure gradient that exists between the hot Sahara and cold Atlantic, the flow of the southerly monsoon from the Atlantic Ocean bringing in the moisture-laden air towards land is in the spring and summer seasons (Thorncroft et al. 2011).
The air masses are vertically raised by convective motion and transported horizontally by the upper air southerly monsoon flow to the Himalayas [12].
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In summer the southerly tropical monsoon blows from the North Pacific onto the Asian mainland, causing dense fog when its warm and moist winds blow over the cold currents that prevail over the northern part of the sea at that season.
The CDW extends farther offshore, driven by the southerly and southwesterly monsoons from June to August, and advection of the CDW causes a significant decrease in the sea surface salinity (SSS) of the northern Okinawa Trough (Chang and Isobe 2003; Lee and Chao 2003).
Low-level southerly wind prevailed after the monsoon onset.
Herein, seasonal precipitation patterns, moisture trajectories and precipitation isotopes suggest this region is seasonally dominated by the monsoon in summer and the southerlies (from the Bay of Bengal) or a mix of southerlies and westerlies in spring.
Moist southwesterly wind was induced in the southwestern Philippines after the monsoon onset, and low-level southerly wind intensified after the monsoon onset with sudden moistening in the northern Philippines.
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