Anomalies in Tropical Methane Emissions: Using Isotopes to Characterise Source Variability. / Brownlow, Rebecca.

2017. 248 p.

Research output: ThesisDoctoral Thesis

Unpublished

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@phdthesis{736011b84ed34dd696cf8f28e22e5180,
title = "Anomalies in Tropical Methane Emissions: Using Isotopes to Characterise Source Variability",
abstract = "In 2007 a sustained atmospheric global growth of methane began and was particularly strong in the tropics. The tropics are poorly understood with few measurements, despite being an important part of the global methane budget. Sources include natural wetlands, rice agriculture, biomass burning, ruminants, fossil fuels and waste. This thesis focuses on sources sampled across the tropics using Tedlar bags, with Bachok, Malaysia and Ascension Island selected for more detailed sampling and studies. Samples were analysed for methane mole fractions using cavity ring-down spectroscopy and for isotopic source signatures, δ13C, using gas chromatography/isotope-ratio mass spectrometry. Using δ13C and mole fraction measurements means both global and regional emissions can be constrained in models with better source apportionment improving the understanding of the sustained tropical methane growth. Keeling plots have been used to calculate the δ13C source signature of each source type. Tropical wetlands have a signature between -61.5 ± 2.9 ‰  and -53.0 ± 0.4 ‰ and are generally more enriched than temperate and boreal wetlands.Continuous monitoring of greenhouse gases and collection of air samples at Bachok research station, Malaysia showed the background CH4 mole fraction is influenced by air masses arriving from over China and Southeast Asia. Local CH4peaks were not predominantly biomass burning as expected, but instead gave a signature of -54.9 ± 1.2 ‰, suggesting mixing with biogenic sources, showing the importance of monitoring CH4 isotopes.Ascension Island is a remote South Atlantic equatorial site, ideal for monitoring tropical background CH4. Octocopters were used to collect air samples from different heights above and below the Trade Wind Inversion (TWI). This work has shown it is possible to retrieve air samples up to an altitude of 2700m above mean sea level. Both campaigns show a consistently higher mole fraction above the TWI, representative of air masses arriving from over Africa compared to below the TWI where air masses arrive from the remote south Atlantic.",
keywords = "methane, tropics, d13C, carbon isotope",
author = "Rebecca Brownlow",
year = "2017",
language = "English",
school = "Royal Holloway, University of London",

}

RIS

TY - THES

T1 - Anomalies in Tropical Methane Emissions: Using Isotopes to Characterise Source Variability

AU - Brownlow, Rebecca

PY - 2017

Y1 - 2017

N2 - In 2007 a sustained atmospheric global growth of methane began and was particularly strong in the tropics. The tropics are poorly understood with few measurements, despite being an important part of the global methane budget. Sources include natural wetlands, rice agriculture, biomass burning, ruminants, fossil fuels and waste. This thesis focuses on sources sampled across the tropics using Tedlar bags, with Bachok, Malaysia and Ascension Island selected for more detailed sampling and studies. Samples were analysed for methane mole fractions using cavity ring-down spectroscopy and for isotopic source signatures, δ13C, using gas chromatography/isotope-ratio mass spectrometry. Using δ13C and mole fraction measurements means both global and regional emissions can be constrained in models with better source apportionment improving the understanding of the sustained tropical methane growth. Keeling plots have been used to calculate the δ13C source signature of each source type. Tropical wetlands have a signature between -61.5 ± 2.9 ‰  and -53.0 ± 0.4 ‰ and are generally more enriched than temperate and boreal wetlands.Continuous monitoring of greenhouse gases and collection of air samples at Bachok research station, Malaysia showed the background CH4 mole fraction is influenced by air masses arriving from over China and Southeast Asia. Local CH4peaks were not predominantly biomass burning as expected, but instead gave a signature of -54.9 ± 1.2 ‰, suggesting mixing with biogenic sources, showing the importance of monitoring CH4 isotopes.Ascension Island is a remote South Atlantic equatorial site, ideal for monitoring tropical background CH4. Octocopters were used to collect air samples from different heights above and below the Trade Wind Inversion (TWI). This work has shown it is possible to retrieve air samples up to an altitude of 2700m above mean sea level. Both campaigns show a consistently higher mole fraction above the TWI, representative of air masses arriving from over Africa compared to below the TWI where air masses arrive from the remote south Atlantic.

AB - In 2007 a sustained atmospheric global growth of methane began and was particularly strong in the tropics. The tropics are poorly understood with few measurements, despite being an important part of the global methane budget. Sources include natural wetlands, rice agriculture, biomass burning, ruminants, fossil fuels and waste. This thesis focuses on sources sampled across the tropics using Tedlar bags, with Bachok, Malaysia and Ascension Island selected for more detailed sampling and studies. Samples were analysed for methane mole fractions using cavity ring-down spectroscopy and for isotopic source signatures, δ13C, using gas chromatography/isotope-ratio mass spectrometry. Using δ13C and mole fraction measurements means both global and regional emissions can be constrained in models with better source apportionment improving the understanding of the sustained tropical methane growth. Keeling plots have been used to calculate the δ13C source signature of each source type. Tropical wetlands have a signature between -61.5 ± 2.9 ‰  and -53.0 ± 0.4 ‰ and are generally more enriched than temperate and boreal wetlands.Continuous monitoring of greenhouse gases and collection of air samples at Bachok research station, Malaysia showed the background CH4 mole fraction is influenced by air masses arriving from over China and Southeast Asia. Local CH4peaks were not predominantly biomass burning as expected, but instead gave a signature of -54.9 ± 1.2 ‰, suggesting mixing with biogenic sources, showing the importance of monitoring CH4 isotopes.Ascension Island is a remote South Atlantic equatorial site, ideal for monitoring tropical background CH4. Octocopters were used to collect air samples from different heights above and below the Trade Wind Inversion (TWI). This work has shown it is possible to retrieve air samples up to an altitude of 2700m above mean sea level. Both campaigns show a consistently higher mole fraction above the TWI, representative of air masses arriving from over Africa compared to below the TWI where air masses arrive from the remote south Atlantic.

KW - methane

KW - tropics

KW - d13C

KW - carbon isotope

M3 - Doctoral Thesis

ER -