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Atmospheric methane levels were nearly steady between 1999 and 2006, but have been rising since then. Increases in wetland emissions, the largest natural global CH4 source, may be partly responsible. Tropical regions like Amazonia, host some of the largest wetlands on Earth, but there are few in-situ observations, which allow large-scale flux estimation. To improve estimates of its contribution to the global CH4 budget we measured 590 lower-troposphere methane concentrations vertical profiles at four Amazonian sites between 2010 and 2018. We estimate that Amazonia emits 46.2±10.3 TgCH4 y-1 (~8% of global emissions) with no emission trend. Non-fire sources (mainly wetlands) dominate emissions, with a smaller biomass burning contribution (~17%). We find a distinct east-west contrast with an emission peak in the northeast. Furthermore, while northwest-central Amazon emissions are nearly aseasonal, consistent with weak precipitation seasonality, southern emissions are strongly seasonal synchronously with equivalent water thickness seasonality.
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Sensitive Response of Atmospheric Oxidative Capacity to the Uncertainty in the Emissions of Nitric Oxide (NO) From Soils in Amazonia
Abstract Soils are a major source of nitrogen oxides, which in the atmosphere help govern its oxidative capacity. Thus the response of soil nitric oxide (NO) emissions to forcings such as warming or forest loss has a meaningful impact on global atmospheric chemistry. We find that the soil emission rate of NO in Amazonia from a common inventory is biased low by at least an order of magnitude in comparison to tower‐based observations. Accounting for this regional bias decreases the modeled global methane lifetime by 1.4%–2.6%. In comparison, a fully deforested Amazonia, representing a 37% decrease in global emissions of isoprene, decreases methane lifetime by at most 4.6%, highlighting the sensitive response of oxidation rates to changes in emissions of NO compared to those of terpenes. Our results demonstrate that improving our understanding of soil NO emissions will yield a more accurate representation of atmospheric oxidative capacity.
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- Award ID(s):
- 1925837
- PAR ID:
- 10559777
- Publisher / Repository:
- American Geophysical Union
- Date Published:
- Journal Name:
- Geophysical Research Letters
- Volume:
- 51
- Issue:
- 13
- ISSN:
- 0094-8276
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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- Free Publicly Accessible Full Text
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Accepted Manuscript
- Journal Article:
- https://doi.org/10.1029/2023GL107214
