@Article{LemesOGFABBMSTGBB:2023:ImSoAm,
author = "Lemes, Murilo da Costa and Oliveira, Gilvan Sampaio de and
Garcia-Carreras, Luis and Fisch, Gilberto and Alves, Lincoln Muniz
and Bassett, Richard and Betts, Richard and Maksic, Jelena and
Shimizu, Mar{\'{\i}}lia Harumi and Torres, Roger Rodrigues and
Guatura, Marcelo Barbosa da Silva and Basso, Luana Santamaria and
Bispo, Polyanna da C.",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {University of
Manchester (UoM)} and {Universidade de Taubat{\'e} (UNITAU)} and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and {University
of Manchester (UoM)} and {Met Office Hadley Centre} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)} and {Universidade Federal de
Itajub{\'a} (UNIFEI)} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {Instituto Nacional de Pesquisas Espaciais
(INPE)} and {University of Manchester (UoM)}",
title = "Impacts on South America moisture transport under Amazon
deforestation and 2 °C global warming",
journal = "Science of the Total Environment",
year = "2023",
volume = "905",
pages = "e167407",
month = "Dec.",
keywords = "Aerial Rivers, Climate modeling, Global warming, La Plata basin,
Water budget.",
abstract = "The increase in greenhouse gasses (GHG) anthropogenic emissions
and deforestation over the last decades have led to many chemical
and physical changes in the climate system, affecting the
atmosphere's energy and water balance. A process that could be
affected is the Amazonian moisture transport in the South American
continent (including La Plata basin), which is crucial to the
southeast Brazilian water regime. The focus of our research is on
evaluating how local (i.e. Amazon deforestation) and global
forcings (increase of atmospheric GHG concentration) may modify
this moisture transport under climate change scenarios. We used
two coupled land-atmosphere models forced by CMIP6 sea surface
temperatures to simulate these processes for two scenarios: i)
increase in carbon dioxide (CO2) RCP8.5 atmospheric levels
(00DEF), and ii) total Amazon deforestation simultaneous with
atmospheric CO2 levels increased (100DEF). These scenarios were
compared with a control simulation, set with a constant CO2 of 388
ppm and present-day Amazon Forest cover. The 30-year Specific
Warming Level 2 (SWL2) index evaluated from the simulations is set
to be reached 2 years earlier due to Amazon deforestation. A
reduction in precipitation was observed in the Amazon basin
(\−3.1 mm·day\−1) as well as in La Plata Basin
(\−0.5 mm·day\−1) due to reductions in the Amazon
evapotranspiration (\−0.9 mm·day\−1) through a
stomatal conductance decrease (00DEF) and land cover change
(100DEF). In addition, the income moisture transport decreased (22
%) in the northern La Plata basin in both scenarios and model
experiments. Our results indicated a worse scenario than
previously found in the region. Both Amazon and La Plata
hydrological regimes are connected (moisture and energy
transport), indicating that a large-scale Amazon deforestation
will have additional climate, economic and social implications for
South America.",
doi = "10.1016/j.scitotenv.2023.167407",
url = "http://dx.doi.org/10.1016/j.scitotenv.2023.167407",
issn = "0048-9697",
language = "en",
targetfile = "1-s2.0-S0048969723060345-main.pdf",
urlaccessdate = "09 maio 2024"
}