@Article{JimenezMaAlSuTaFeCo:2021:RoENFl,
author = "Jimenez, Juan C. and Marengo, Jos{\'e} A. and Alves, Lincoln
Muniz and Sulca, Juan C. and Takahashi, Ken and Ferrett, Samantha
and Collins, Matthew",
affiliation = "{University of Valencia} and {Centro Nacional de Monitoramento e
Alertas de Desastres Naturais (CEMADEN)} and {Instituto Nacional
de Pesquisas Espaciais (INPE)} and {Instituto Geof{\'{\i}}sico
del Per{\'u} (IGP)} and SENAMHI and {University of Reading} and
{University of Exeter}",
title = "The role of ENSO flavours and TNA on recent droughts over Amazon
forests and the Northeast Brazil region",
journal = "International Journal of Climatology",
year = "2021",
volume = "41",
number = "7",
pages = "3761--3780",
month = "June",
note = "{Pr{\^e}mio CAPES Elsevier 2023 - ODS 2: Fome zero e Agricultura
sustent{\'a}vel}",
keywords = "Amazonia, drought, ENSO, Northeast Brazil, precipitation, TNA.",
abstract = "Amazon tropical forests and the semiarid Northeast Brazil (NEB)
region have registered very severe droughts during the last two
decades, with a frequency that may have exceeded natural climate
variability. Severe droughts impact the physiological response of
Amazon forests, decreasing the availability to absorb atmospheric
CO2, as well as biodiversity and increasing risk of fires.
Droughts on this region also affect population by isolating them
due to anomalous low river levels. Impacts of droughts over NEB
region are related to water and energy security and subsistence
agriculture. Most drought episodes over Amazonia and NEB are
associated with El Niņo (EN) events, anomalous warming over the
Tropical North Atlantic (TNA), and even an overlapping among them.
However, not all the dry episodes showed a large-scale pattern
linked to a canonical EN event or warm TNA episodes. For instance,
dry episodes linked to EN events present distinct spatial patterns
of precipitation anomalies depending on EN type (Central-Pacific
vs. Eastern-Pacific EN), and NEB region experienced a severe
drought in 2012 that is not attributed to EN or warm TNA events.
Even in the case of the strong EN in 2015/16, some regional
impacts have not been explained by EN contribution. This paper
discusses the effects of CP and EP EN events, and the role of warm
TNA events on tropical Walker and Hadley circulation leading to
drought over Amazonia and NEB regions.",
doi = "10.1002/joc.6453",
url = "http://dx.doi.org/10.1002/joc.6453",
issn = "0899-8418",
language = "en",
targetfile = "jimenez_role.pdf",
urlaccessdate = "28 abr. 2024"
}