“…The region, including the maritime continent, South China Sea/East Sea (SCS/ES), and Sulu Sea, is thought to be highly susceptible to aerosol cloud interactions (Rosenfeld, 1999;Hamid et al, 2001;Yuan et al, 2011). Indeed, around the second half of the boreal summer monsoonal period from August to mid-October, the seasonal dry climate allows biomass burning throughout the maritime continent (MC), particularly in warm El Niño-Southern Oscillation phases (e.g, Nichol, 1998;van der Werf et al, 2004;Field and Shen, 2008;Langner and Siegert, 2009;Field et al, 2009;van der Kaars et al, 2010;Reid et al, 2012Reid et al, , 2013. Climatologically, there exists both anecdotal evidence and some station data suggesting an increase in the number of no-rain days in the Philippines (Cruz et al, 2013), yet perhaps an increase in intense events (Cinco et al, 2014).…”