Effects of mountains on aerosols determined by AERONET/DRAGON/J-ALPS
measurements and regional model simulations
Abstract
The NASA/AERONET field campaign DRAGON/J-ALPS (Distributed Regional
Aerosol Gridded Observation Networks/Joint work to the AerosoL
Properties and Process Simulations) was conducted from March 2020 to May
2021 in Nagano, Japan. Twelve sun photometers were installed around
Nagano prefecture. The effects of topography on aerosols were studied
using observations and simulations. In this study, a regional chemical
transport model (SCALE-Chem) was employed. Three numerical experiments
were conducted: E1 (control experiment), E2 (E1 without topography), and
E3 (E1 with removal of all anthropogenic emissions over Nagano
prefecture). In E2, the terrain effect was not considered; the
difference between E1 and E2 indicated the influence of mountains. The
differences between E1 and E3 evaluate the local emission effect. In
some cases, the mountainous terrain seemed to have suppressed aerosol
inflow (i.e., reduced aerosol concentration), while in other cases, the
mountains contributed to aerosol retention on days when aerosols tended
to accumulate in mountain basins due to local emissions. Thus, while
mountains prevent the inflow of aerosols from outside, they also
contribute to increased aerosol concentration in the basin. Naturally,
more significant effects are produced by meteorological conditions and
the presence or absence of transboundary pollution from the outside.
From observations and model simulations, we found that the aerosol
concentration was not high around the J-ALPS site because of the
mountain effect that prevents advection from the outside, even when
transboundary pollution was observed in Japan in March 2020.