@Article{SaatchiAsMaArAnMyNe:2013:PeEfSe,
author = "Saatchi, S. and Asefi-Najafabady, S. and Malhi, Y. and
Arag{\~a}o, L. E. O. C. and Anderson, Liana Oighenstein and
Myneni, R. B. and Nemani, R.",
affiliation = "Jet Propulsion Laboratory, California Institute of Technology,
Pasadena, CA 91109, United States; Institute of Environment,
University of California, Los Angeles, CA 90045, United States and
Institute of Environment, University of California, Los Angeles,
CA 90045, United States and Environmental Change Institute, School
of Geography and the Environment, University of Oxford, Oxford OX1
3QY, United Kingdom and College of Life and Environmental
Sciences, University of Exeter, Devon EX4 4RJ, United Kingdom and
{Instituto Nacional de Pesquisas Espaciais (INPE)} and Department
of Geography and Environment, Boston University, Boston, MA 02215,
United States and Biospheric Sciences Branch, National Aeronautics
and Space Administration/Ames Research Center, Moffett Field, CA
94035, United States",
title = "Persistent effects of a severe drought on Amazonian forest
canopy",
journal = "Proceedings of the National Academy of Sciences of the United
Sates of America",
year = "2013",
volume = "110",
number = "2",
pages = "565--570",
month = "Jan.",
note = "{This article contains supporting information online at
www.pnas.org/lookup/suppl/doi:10.1073/pnas.1204651110/-/DCSupplemental.}",
keywords = "rain, water, article, canopy, drought, forest, moisture, priority
journal, water content, Brazil, Droughts, Fires, Geographic
Mapping, Microwaves, Radar, Time Factors, Trees, Tropical
Climate.",
abstract = "Recent Amazonian droughts have drawn attention to the
vulnerability of tropical forests to climate perturbations.
Satellite and in situ observations have shown an increase in fire
occurrence during drought years and tree mortality following
severe droughts, but to date there has been no assessment of
long-term impacts of these droughts across landscapes in Amazonia.
Here, we use satellite microwave observations of rainfall and
canopy backscatter to show that more than 70 million hectares of
forest in western Amazonia experienced a strong water deficit
during the dry season of 2005 and a closely corresponding decline
in canopy structure and moisture. Remarkably, and despite the
gradual recovery in total rainfall in subsequent years, the
decrease in canopy backscatter persisted until the next major
drought, in 2010. The decline in backscatter is attributed to
changes in structure and water content associated with the forest
upper canopy. The persistence of low backscatter supports the slow
recovery (>4 y) of forest canopy structure after the severe
drought in 2005. The result suggests that the occurrence of
droughts in Amazonia at 5-10 y frequency may lead to persistent
alteration of the forest canopy.",
doi = "10.1073/pnas.1204651110",
url = "http://dx.doi.org/10.1073/pnas.1204651110",
issn = "0027-8424",
label = "scopus",
language = "en",
targetfile = "PNAS-2013-Saatchi-565-70.pdf",
url = "www.pnas.org/cgi/doi/10.1073/pnas.1204651110",
urlaccessdate = "28 abr. 2024"
}