@InProceedings{FreireLonFreSilCoe:2018:EvImBi,
author = "Freire, Julliana L M and Longo, Karla M. and Freitas, Saulo R. and
Silva, Arlindo and Coelho, Caio A. S.",
title = "Evaluation of the impacts of biomass burning emissions on the nasa
geos seasonal climate forecast",
booktitle = "Anais...",
year = "2018",
editor = "Herdies, Dirceu Luis and Coelho, Simone Marilene Sievert da
Costa",
organization = "Encontro dos alunos de p{\'o}s-gradua{\c{c}}{\~a}o em
meteorologia do CPTEC/INPE, 17. (EPGMET)",
publisher = "Instituto Nacional de Pesquisas Espaciais (INPE)",
address = "S{\~a}o Jos{\'e} dos Campos",
keywords = "African, Modeling, Aerosol Particles.",
abstract = "Emission sources of trace gases and aerosol particles in the South
American (SA) and African (Af) continents have a strong seasonal
and space variability associated with the extensive vegetation
fires activities. Smoke aerosols also act as cloud condensation
nuclei affecting cloud microphysics properties and therefore,
changing the radiation budget, hydrological cycle and global
circulation patterns over disturbed areas (Andreae, et al. 2004;
Randles et al. 2013). This study aims to evaluate and quantify the
impact of including a comprehensive emission field of biomass
burning aerosol on the performance of a seasonal climate forecast
system, not only regarding the AOD itself but mainly on the
meteorological state variable (e.g., precipitation and
temperature). To address the questions put above, we designed two
numerical experiments: 1- named AERO_CTL which applies the QFED
emissions estimated with intra-diurnal variation (hereafter,BBE),
and 2- named AERO_CLM where the source emission is based on a
climatology of the QFED emissions, with only monthly variation
(hereafter,BBCLIM). Hindcast simulations were produced using the
GEOS5-S2S system with a nominal spatial resolution of 56km. In
both experiments, the aerosol feedbacks from cloud developments
and radiation interactions were accounted. The two experiments
consisted of 4 members each and ran from June to November spanning
over the years 2000 to 2015. Model performance was evaluated by
calculating statistical metrics on the mean area of SA and Af. Our
results demonstrated that the skill model in predicting AOD is
significantly improve when BBE source emission is applied over SA,
but not over the Af continent. Over SA, the correlation between
the AERO_CTL model configuration and MERRA-2 is 0.93 (R2= 0.86,
RMS=0.02, BIAS=0.01), while the AERO_CLM model presents a value of
0.81 (R2= 0.65, RMS=0.04, BIAS=0.06). However, the AERO_CTL
experiment better represents the inter-annual variability of the
AOD in both regions. The gain of the skill in predicting the AOD
by the AERO_CTL experiment is also seen in some meteorological
variables. We observed an increase in the model skill in
predicting the 2-meter temperature and precipitation of up to 0.3
for the AERO_CTL experiment in comparison to the AERO_CLM.
AERO_CLM. According to the analyzed hindcast, we inferred that
representing the BBE more realistically implies in a significant
gain of skills in the seasonal climate forecasting over SA and Af
continents.",
conference-location = "Cachoeira Paulista",
conference-year = "22-26 out. 2018",
language = "pt",
organisation = "Instituto Nacional de Pesquisas Espaciais (INPE)",
ibi = "8JMKD3MGPDW34R/3SR2CE8",
url = "http://urlib.net/ibi/8JMKD3MGPDW34R/3SR2CE8",
targetfile = "MG3-06.pdf",
type = "Modelagem Geral",
urlaccessdate = "19 maio 2024"
}