Aerosols are an important
part of Earth’s atmosphere. They
can absorb, scatter, or reflect the incoming solar radiation, which
results in heating or cooling of Earth, thus impacting its climate.
It affects the health of exposed human population adversely, reduces
visibility, disturbs environmental systems, and causes material damage.
This study summarizes the research carried out to understand the role
of aerosol load and its physicochemical characteristics on occurrence,
frequency, and magnitude of haze and fog events during wintertime
within the Indo Gangetic Plain (IGP) in the past decade. For most
species, the highest concentration was measured during foggy events
at night-time over the winter season. A few species such as water-soluble
organic and inorganic carbon (WSOC and WSIC), K+, SO4
2–, and NO3
–, owing to their hygroscopic nature, were efficiently scavenged,
resulting in their lower concentration within the interstitial aerosol
during fog episodes. Oligomerization with hydroxy and carbonyl functional
groups during AFP (activating fog period) and DFP (dissipating fog
period), respectively, accompanied by acidic aerosol (having catalytic
ability) and high aerosol liquid water content conditions was found
to be significant. Whereas the fragmentation process was dominant
along with functionalization of −RCOOH or carbonyl (aldehyde/ketone)
and −RCOOH moieties during FP (fog period) and PoFP (post-fog
period), respectively. Transition metals play an important role in
aqueous production of secondary organic aerosol (SOA) especially during
the night-time. Crustal sources had the highest scavenging efficiency
along with WSOC playing an important role in nucleation scavenging.
Fine droplets had a higher concentration of species with a larger
fraction of highly oxidized organic matter (OM) as compared to coarse
or medium size droplets. Also, a new approach to calculate absorption
by black carbon (BC) and brown carbon (BrC) was proposed, which found
the water-soluble brown carbon (WSBrC) absorption value in aerosol
to be up to 1.8 times higher than that measured in their corresponding
aqueous extracts. Organic aerosol plays a vital role in facilitating
fog formation and is responsible for the longer residence time in
the ambient atmosphere. Ammonia plays an important role in stabilizing
organic aerosol and aids to this recurring haze–fog–haze
cycle that is dominant during wintertime in the IGP. Therefore, controlling
the major anthropogenic sources of organic aerosol and ammonia should
be our top priority in this part of the world.