@Article{PendharkarFVKSKAVGNH:2023:AeMiIn,
author = "Pendharkar, Jayant and Figueroa, Silvio Nilo and Vara-Vela, Angel
and Krishna, R. Phani Murali and Schuch, Daniel and Kubota, Paulo
Yoshio and Alvim, D{\'e}bora Souza and Vendrasco, {\'E}der Paulo
and Gomes, Helber Barros and Nobre, Paulo and Herdies, Dirceu
Luis",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Aarhus University}
and {Indian Institute of Tropical Meteorology} and {Northeastern
University} and {Instituto Nacional de Pesquisas Espaciais (INPE)}
and {Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and
{Universidade Federal de Alagoas (UFAL)} and {Instituto Nacional
de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)}",
title = "Towards unified online-coupled aerosol parameterization for the
Brazilian Global Atmospheric Model (BAM): aerosol-cloud
microphysical-radiation interactions",
journal = "Remote Sensing",
year = "2023",
volume = "15",
number = "1",
pages = "e278",
month = "Jan.",
keywords = "aerosol-cloud microphysical-radiation interactions, aerosols,
global model.",
abstract = "In this work, we report the ongoing implementation of
online-coupled aerosol-cloud microphysical-radiation interactions
in the Brazilian global atmospheric model (BAM) and evaluate the
initial results, using remote-sensing data for JFM 2014 and JAS
2019. Rather than developing a new aerosol model, which incurs
significant overheads in terms of fundamental research and
workforce, a simplified aerosol module from a preexisting global
aerosol-chemistry-climate model is adopted. The aerosol module is
based on a modal representation and comprises a suite of aerosol
microphysical processes. Mass and number mixing ratios, along with
dry and wet radii, are predicted for black carbon, particulate
organic matter, secondary organic aerosols, sulfate, dust, and sea
salt aerosols. The module is extended further to include
physically based parameterization for aerosol activation, vertical
mixing, ice nucleation, and radiative optical properties
computations. The simulated spatial patterns of surface mass and
number concentrations are similar to those of other studies. The
global means of simulated shortwave and longwave cloud radiative
forcing are comparable with observations with normalized mean
biases <= 11% and <= 30%, respectively. Large positive bias in BAM
control simulation is enhanced with the inclusion of aerosols,
resulting in strong overprediction of cloud optical properties.
Simulated aerosol optical depths over biomass burning regions are
moderately comparable. A case study simulating an intense biomass
burning episode in the Amazon is able to reproduce the transport
of smoke plumes towards the southeast, thus showing a potential
for improved forecasts subject to using near-real-time
remote-sensing fire products and a fire emission model. Here, we
rely completely on remote-sensing data for the present evaluation
and restrain from comparing our results with previous results
until a complete representation of the aerosol lifecycle is
implemented. A further step is to incorporate dry deposition,
in-cloud and below-cloud scavenging, sedimentation, the sulfur
cycle, and the treatment of fires.",
doi = "10.3390/rs15010278",
url = "http://dx.doi.org/10.3390/rs15010278",
issn = "2072-4292",
label = "self-archiving-INPE-MCTIC-GOV-BR",
language = "en",
targetfile = "remotesensing-15-00278-v2.pdf",
urlaccessdate = "16 jun. 2024"
}