@InProceedings{LemesSampFisc:2023:AmDeCo,
author = "Lemes, Murilo Ruv da Costa and Sampaio, Gilvan and Fisch, Gilberto
Fernando",
affiliation = "{Instituto Nacional de Pesquisas Espaciais (INPE)} and {Instituto
Nacional de Pesquisas Espaciais (INPE)} and {Instituto Nacional de
Pesquisas Espaciais (INPE)}",
title = "Amazon deforestation combined high atmospheric CO2 concentration,
a new state of South America climate",
booktitle = "Proceedings...",
year = "2023",
organization = "AGU FAll Meeting",
publisher = "AGU",
abstract = "The land cover change in the Amazon basin has been a high-impact
subject in climate studies, especially those that evaluated the
hydrological issues not only locally but also regionally. However,
the increase of atmospheric carbon dioxide may lead to different
behavior in the biosphere-atmosphere coupled system, which brings
a worse climate change scenario. Therefore, the main goal is to
evaluate how the total Amazon deforestation and higher atmospheric
carbon dioxide concentration modulate the moisture transport
mechanism in the South America continent. Through a climate
modelling study, the CPTEC-BAM (Brazilian Atmospheric Model) and
CESM (Community Earth System Model) were selected to simulate such
processes over the Amazon basin and Sao Paulo region during the
austral summer (December-January-February / wet season). Both
models were forced by HadGEM- CMIP6 Sea Surface Temperature (SST).
The Amazon forest was completely replaced by grasslands (C4) and
the Representative Concentration Pathway 8.5 (RCP8.5) was
considered as a greenhouse gas scenario. Finally, the Specific
Warming Level 2 (SWL2) was applied as the main index to analyze
the atmospheric changes. The 30-year period in which the 2.0o C is
reached in comparison to the pre-industrial period is considered
the SWL period (in this case 2024-2054 (CPTEC-BAM) and 2029-2059
(CESM)). The results showed a stronger local evapotranspiration
(physiological parameters stomatal conductance reduction) and
precipitation reduction (~ -0.7 mm.day-1 and ~ -1.5 mm.day-1),
however, the wind speed over the Amazon forest increased (17%).
Such change contributed to higher moisture amount brought from the
Atlantic Tropical Ocean (+10%), which increase the moisture
transport over the western Amazon basin and decreased (-15%) in
the southern boundary. Looking at the regional domain, the
precipitation over the Sao Paulo area decreased by around 7.8% due
to total Amazon deforestation and higher carbon dioxide, which is
shown by the moisture incoming reduction of around 11%, which
means 1.5 kg m-1 s-1 less. Although both models showed a different
anomaly signal for bias moisture incoming in Sao Paulo CPTEC-BAM
(+) and CESM (-). In addition, the decrease of the CAPE index over
the Sao Paulo area may indicate not only a hydrological collapse
situation but also severe energy balance changes. In conclusion,
when the SWL2 approach is used to evaluate land cover changes
through climate modelling some results may be different from
well-known literature because more effects are added. In this way,
a strong connection between the Amazon moisture source and Sao
Paulo was identified, which climate changes may be
catastrophically looking at the most important economic South
America region (31% of gross internal Brazilian product Nexus
water-food-energy).",
conference-location = "San Francisco, CA",
conference-year = "11-15 Dec. 2023",
language = "en",
urlaccessdate = "29 jun. 2024"
}