@Article{MelackHeGaFoHaLiNo:2004:ReMeEm,
author = "Melack, John M. and Hess, Laura L. and Gastil, Mary and Forsberg,
Bruce R. and Hamilton, Stephen K. and Lima, Ivan B. T. and Novo,
Evlyn Marcia Leao de Moraes",
affiliation = "Bren School of Environmental Science and Management, University of
California, Santa Barbara, CA 93106, USA and Institute for
Computational Earth System Science, University of California,
Santa Barbara, CA 93106, USA and Depto. de Ecologia, Instituto
Nacional de Pesquisas da Amazonia, Manaus, Amazonas, Brazil and
Kellogg Biological Station and Department of Zoology, Michigan
State University, 3700 E. Gull Lake Dr, Hickory Corners, MI 49060,
USA and Divis{\~a}o de Sensoriamento Remoto, Instituto Nacional
de Pesquisas Espaciais, C.P. 515, CEP 12201, S{\~a}o Jos{\'e}
dos Campos, S{\~a}o Paulo, Brazil",
title = "Regionalization of methane emissions in the Amazon Basin with
microwave remote sensing",
journal = "Global Change Biology",
year = "2004",
volume = "10",
pages = "530--544",
keywords = "Amazon, biogeochemistry, carbon, methane, microwave remote
sensing, wetlands.",
abstract = "Wetlands of the Amazon River basin are globally significant
sources of atmospheric methane. Satellite remote sensing (passive
and active microwave) of the temporally varying extent of
inundation and vegetation was combined with field measurements to
calculate regional rates of methane emission for Amazonian
wetlands. Monthly inundation areas for the fringing floodplains of
the mainstem Solimoes/Amazon River were derived from analysis of
the 37GHz polarization difference observed by the Scanning
Multichannel Microwave Radiometer from 1979 to 1987. L-band
synthetic aperture radar data (Japanese Earth Resources
Satellite-1) were used to determine inundation and wetland
vegetation for the Amazon basin (o500m elevation) at high
(May-June 1996) and low water (October 1995). An extensive set of
measurements of methane emission is available from the literature
for the fringing floodplains of the central Amazon, segregated
into open water, flooded forest and floating macrophyte habitats.
Uncertainties in the regional emission rates were determined by
Monte Carlo error analyses that combined error estimates for the
measurements of emission and for calculations of inundation and
habitat areas. The mainstem Solimoes/Amazon floodplain (54 01W)
emitted methane at a mean annual rate of 1.3 TgCyr1, with a
standard deviation (SD) of the mean of 0.3 TgCyr1; 67% of this
range in uncertainty is owed to the range in rates of methane
emission and 33% is owed to uncertainty in the areal estimates of
inundation and vegetative cover. Methane emission from a 1.77
million square kilometers area in the central basin had a mean of
6.8 TgCyr1 with a SD of 1.3 TgCyr1. If extrapolated to the whole
basin below the 500m contour, approximately 22 TgCyr1 is emitted;
this mean flux has a greenhouse warming potential of about 0.5 PgC
as CO2. Improvement of these regional estimates will require many
more field measurements of methane emission, further examination
of remotely sensed data for types of wetlands not represented in
the central basin, and process-based models of methane production
and emission.",
copyholder = "SID/SCD",
issn = "1354-1013",
language = "<end-of-file>",
targetfile = "Regionalization of methane emissions in the
Amazon.1365-2486.2004.00763.x.pdf",
urlaccessdate = "29 jun. 2024"
}