Abstract
Aerosols play a key role in polar climate, and are affected by
long-range transport from the mid-latitudes, both in the Arctic and
Antarctic. This work investigates poleward extreme transport events of
aerosols, referred to as aerosol rivers (AeR), leveraging the concept of
atmospheric rivers (AR) which signal extreme transport of moisture.
Using reanalysis data, we build a detection catalog of polar AeRs for
black carbon, dust, sea salt and organic carbon aerosols, for the period
1980–2022. First, we describe the detection algorithm, discuss its
sensitivity, and evaluate its validity. Then, we present several extreme
transport case studies, in the Arctic and in the Antarctic, illustrating
the complementarity between ARs and AeRs. Despite similarities in
transport pathways during co-occurring AR/AeR events, vertical profiles
differ depending on the species, and large-scale transport patterns show
that moisture and aerosols do not necessarily originate from the same
areas. The complementarity between AR and AeR is also evidenced by their
long-term characteristics in terms of spatial distribution, seasonality
and trends. AeR detection, as a complement to AR, can have several
important applications for better understanding polar climate and its
connections to the mid-latitudes.