Abstract. A 16-month (July 2018–October 2019) dataset of size-resolved aerosol
composition is used to examine the sources and characteristics of five
organic acids (oxalate, succinate, adipate, maleate, phthalate) and
methanesulfonate (MSA) in Metro Manila, Philippines. As one of the most
polluted megacities globally, Metro Manila offers a view of how diverse
sources and meteorology impact the relative amounts and size distributions
of these species. A total of 66 sample sets were collected with a
Micro-Orifice Uniform Deposit Impactor (MOUDI), of which 54 sets were
analyzed for composition. Organic acids and MSA surprisingly were less
abundant than in other global regions that are also densely populated. The
combined species accounted for an average of 0.80 ± 0.66 % of total
gravimetric mass between 0.056 and 18 µm, still leaving 33.74 % of
mass unaccounted for after considering black carbon and water-soluble ions
and elements. The unresolved mass is suggested to consist of
non-water-soluble metals as well as both water-soluble and non-water-soluble
organics. Oxalate was approximately an order of magnitude more abundant than
the other five species (149 ± 94 ng m−3 versus others being
< 10 ng m−3) across the 0.056–18 µm size range. Both
positive matrix factorization (PMF) and correlation analysis are conducted
with tracer species to investigate the possible sources of organic acids
and MSA. Enhanced biomass burning influence in the 2018 southwest monsoon
resulted in especially high levels of submicrometer succinate, MSA, oxalate,
and phthalate. Peculiarly, MSA had negligible contributions from marine
sources but instead was linked to biomass burning and combustion. Enhanced
precipitation during the two monsoon seasons (8 June–4 October 2018 and
14 June–7 October 2019) coincided with a stronger influence from local
emissions rather than long-range transport, leading to notable concentration
enhancements in both the sub- and supermicrometer ranges for some species
(e.g., maleate and phthalate). While secondary formation via gas-to-particle
conversion is consistent with submicrometer peaks for the organic acids and
MSA, several species (i.e., phthalate, adipate, succinate, oxalate)
exhibited a prominent peak in the coarse mode, largely owing to their
association with crustal emissions (i.e., more alkaline aerosol type) rather
than sea salt. Oxalate's strong association with sulfate in the
submicrometer mode supports an aqueous-phase formation pathway for the study
region. However, high concentrations during periods of low rain and high
solar radiation suggest photo-oxidation is an important formation pathway.