Abstract. NASA's Plankton, Aerosol, Cloud, ocean Ecosystem (PACE) mission, scheduled for
launch in the timeframe of 2023, will carry a hyperspectral scanning
radiometer named the Ocean Color Instrument (OCI) and two multi-angle
polarimeters (MAPs): the UMBC Hyper-Angular Rainbow Polarimeter (HARP2) and the
SRON Spectro-Polarimeter for Planetary EXploration one (SPEXone). The MAP
measurements contain rich information on the microphysical properties of
aerosols and hydrosols and therefore can be used to retrieve accurate aerosol
properties for complex atmosphere and ocean systems. Most polarimetric aerosol
retrieval algorithms utilize vector radiative transfer models iteratively in
an optimization approach, which leads to high computational costs that limit
their usage in the operational processing of large data volumes acquired by
the MAP imagers. In this work, we propose a deep neural network (NN) forward
model to represent the radiative transfer simulation of coupled atmosphere and
ocean systems for applications to the HARP2 instrument and its
predecessors. Through the evaluation of synthetic datasets for AirHARP
(airborne version of HARP2), the NN model achieves a numerical accuracy
smaller than the instrument uncertainties, with a running time of
0.01 s in a single CPU core or 1 ms in a GPU. Using the NN as a
forward model, we built an efficient joint aerosol and ocean color retrieval
algorithm called FastMAPOL, evolved from the well-validated Multi-Angular
Polarimetric Ocean coLor (MAPOL) algorithm. Retrievals of aerosol properties
and water-leaving signals were conducted on both the synthetic data and the
AirHARP field measurements from the Aerosol Characterization from Polarimeter
and Lidar (ACEPOL) campaign in 2017. From the validation with the synthetic
data and the collocated High Spectral Resolution Lidar (HSRL) aerosol
products, we demonstrated that the aerosol microphysical properties and water-leaving signals can be retrieved efficiently and within acceptable
error. Comparing to the retrieval speed using a conventional radiative transfer
forward model, the computational acceleration is 103 times faster with CPU
or 104 times with GPU processors. The FastMAPOL algorithm can be used to
operationally process the large volume of polarimetric data acquired by PACE
and other future Earth-observing satellite missions with similar capabilities.