@Article{GonçalvesCoelKuboSouz:2022:InClAt,
author = "Gon{\c{c}}alves, Layrson de Jesus Menezes and Coelho, Simone
Marilene Sievert da Costa and Kubota, Paulo Yoshio and Souza,
Dayana Castilho de",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)}",
title = "Interaction between cloud-radiation, atmospheric dynamics and
thermodynamics based on observational data from GoAmazon 2014/15
and a cloud-resolving model",
journal = "Atmospheric Chemistry and Physics",
year = "2022",
volume = "22",
number = "23",
pages = "15509--15526",
month = "Dec.",
abstract = "Observational meteorological data from the field experiment
GoAmazon 2014/15 and data from numerical simulations with the
cloud-resolving model (CRM) called the System for Atmospheric
Modeling (SAM) are used to study the interaction between the
cloudiness-radiation as well as the atmospheric dynamics and
thermodynamics variables for a site located in the central Amazon
region (-3.2 \& LCIRC; S, -60.6 \& LCIRC; W) during the wet and
dry periods. The main aims are to (a) analyze the temporal series
of the integrated cloud fraction, precipitation rate and downward
shortwave flux as well as (b) to determine the relationship
between the integrated cloud fraction, radiative fluxes and
large-scale variable anomalies as a function of the previous day's
average. The temporal series of the integrated cloud fraction,
precipitation rate and downward shortwave flux from SAM
simulations showed physical consistency with the observations from
GoAmazon 2014/15. Shallow and deep convection clouds show to have
a meaningful impact on radiation fluxes in the Amazon region
during wet and dry periods. Anomalies of large-scale variables
(relative to the previous day's average) are physically associated
with cloud formation, evolution and dissipation. SAM consistently
simulated these results, where the cloud fraction vertical profile
shows a pattern very close to the observed data (cloud type).
Additionally, the integrated cloud fraction and large-scale
variable anomalies, as a function of the previous day's average,
have a good correlation. These results suggest that the memory of
the large-scale dynamics from the previous day can be used to
estimate the cloud fraction as well as the water content, which is
a variable of the cloud itself. In general, the SAM satisfactorily
simulated the interaction between cloud-radiation as well as
dynamic and thermodynamic variables of the atmosphere during the
periods of this study, being able to obtain atmospheric variables
that are impossible to obtain in an observational way.",
doi = "10.5194/acp-22-15509-2022",
url = "http://dx.doi.org/10.5194/acp-22-15509-2022",
issn = "1680-7316 and 1680-7324",
language = "en",
targetfile = "acp-22-15509-2022.pdf",
urlaccessdate = "05 maio 2024"
}