@Article{GloorGWPBPCPZBMMJP:2021:LaMeEm,
author = "Gloor, M. and Gatti, Luciana Vanni and Wilson, C. and Parker, R.
J. and Boesch, H. and Popa, E. and Chipperfield, M. P. and
Poulter, B. and Zhang, Z. and Basso, Luana Santamaria and Miller,
J. and McNorton, J. and Jimenez, C. and Prigent, C.",
affiliation = "{University of Leeds} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {University of Leeds} and {University of
Leicester} and {University of Leicester} and {Universiteit
Utrecht} and {University of Leeds} and {University of Maryland}
and {University of Maryland} and {Instituto Nacional de Pesquisas
Espaciais (INPE)} and {National Oceanic and Atmospheric
Administration (NOAA)} and {European Centre for Medium-Range
Weather Forecasts} and {Observatoire de Paris} and {Observatoire
de Paris}",
title = "Large Methane Emissions From the Pantanal During Rising
Water-Levels Revealed by Regularly Measured Lower Troposphere CH4
Profiles",
journal = "Global Biogeochemical Cycles",
year = "2021",
volume = "35",
number = "10",
pages = "e2021GB006964",
month = "Oct.",
abstract = "The Pantanal region of Brazil is the largest seasonally flooded
tropical grassland and, according to local chamber measurements, a
substantial CH4 source. CH4 emissions from wetlands have recently
become of heightened interest because global atmospheric 13CH4
data indicate they may contribute to the resumption of atmospheric
CH4 growth since 2007. We have regularly measured vertical
atmospheric profiles for 2 years in the center of the Pantanal
with the objectives to obtain an estimate of CH4 emissions using
an atmospheric approach, and provide information about flux
seasonality and its relation to controlling factors. Boundary
layer-free troposphere differences observed in the Pantanal are
large compared to other wetlands. Total emissions based on a
planetary boundary layer budgeting technique are 2.02.8 TgCH4
yr\−1 (maximum flux \∼0.4 gCH4 m\−2
d\−1) while those based on a Bayesian inversion using an
atmospheric transport model are \∼3.3 TgCH4 yr\−1.
Compared to recent estimates for Amazonia (\∼41 ± 3 TgCH4
yr\−1, maximum flux \∼0.3 gCH4 m\−2
d\−1) these emissions are not that large. Our Pantanal data
suggest a clear flux seasonality with CH4 being released in large
amounts just after water levels begin to rise again after minimum
levels have been reached. CH4 emissions decline substantially once
the maximum water level has been reached. While predictions with
prognostic wetland CH4 emission models agree well with the
magnitude of the fluxes, they disagree with the phasing. Our
approach shows promise for detecting and understanding longer-term
trends in CH4 emissions and the potential for future wetlands CH4
emissions climate feedbacks.",
doi = "10.1029/2021GB006964",
url = "http://dx.doi.org/10.1029/2021GB006964",
issn = "0886-6236",
language = "en",
targetfile = "gloor_large_2021.pdf",
urlaccessdate = "11 jun. 2024"
}