@InProceedings{TanajuraChouYongNobr:2004:ExAtMo,
author = "Tanajura, Clemente A. S. and Chou, Sin Chan and Yong, Kang Xue and
Nobre, Carlos Afonso",
affiliation = "{CPTEC-INPE-Cachoeira Paulista-12630-000-SP-Brasil}",
title = "An experiment with the atmosphere-biosphere model Eta/SSiB on the
Amazon deforestation",
booktitle = "Resumos...",
year = "2004",
organization = "Workshop Latino Americano em Modelagem Regional de Tempo e Clima
Utilizando o Modelo ETA: Aspectos Fis{\'{\i}}cos e
Num{\'e}ricos, 1.",
abstract = "An experiment to investigate the impact of the Amazon
deforestation on the South American climate was performed with the
regional Eta model coupled to the simplified version of Simple
Biosphere model (SSiB). The model domain covered all South America
up to 50 oS. The initial and lateral boundary conditions were
provided by NCEP analyses. Nine one-month integrations during
November 1997 were done. The control integration had realistic
vegetation mask. The others had the vegetation type over the
Amazon changed from rain forest to savannah and grassland.
Changing rainforest to savannah produced large decrease of
precipitation in central and eastern Amazon. It also increased the
canopy air temperature by more than 1 oC in the whole Amazon
basin, with values of more than 5 oC in eastern Amazon.. The
differences also show increase of precipitation over the Rio de
Janeiro area around 22 oS. This region is located to the south of
the area with decreased precipitation. The stationary and
transient moisture transports were affected by the vegetation
change, not only over the continent but also over the Southwestern
Atlantic. This affected the simulated South Atlantic Convergence
Zone (SACZ), which depends on the Amazon precipitation and is
responsible for the precipitation maximum over southeast Brazil
during the austral summer. The upper level circulation was
influenced by the reduction of precipitation and the Bolivian High
was not formed. Changing vegetation type from rainforest to
grassland lead to patterns similar to those found previously, but
the precipitation decrease in most of the Amazon region was
smaller. This is due to the higher bare soil moisture flux
provided by the grassland in relation to the savannah. The
experiment shows that modifications in the climate of the Amazon
and other areas over South American may occur in Amazon
deforestation scenarios.",
conference-location = "INPE-CPTEC-Cachoeira Paulista",
conference-year = "21 - 26 mar.",
copyholder = "SID/SCD",
label = "self-archiving-INPE-MCTIC-GOV-BR",
language = "en",
organisation = "INPE/CPTEC/LAC/CTE/APLBA",
targetfile = "11935.pdf",
urlaccessdate = "20 maio 2024"
}