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Abstract
East Africa is a key location for wetland emissions of methane (CH4), driven by variations in rainfall that are in turn influenced by sea-surface temperature gradients over the Indian Ocean. Using satellite observations of CH4 and an atmospheric chemistry-transport model, we quantified East African CH4 emissions during 2018 and 2019 when there was 3-σ anomalous rainfall during the long rains (March-May) in 2018 and the short rains (October-December) in 2019. These rainfall anomalies resulted in CH4 emissions of 6.2±0.3 Tg CH4 and 8.6±0.3 Tg CH4, in each three month period respectively, and represent a 10% and 37% increase compared to the equivalent season in the opposite year, when rainfall was close to the long-term seasonal mean. We find the additional short rains emissions were equivalent to over a quarter of the growth in global emissions in 2019, highlighting the disproportionate role of East Africa in the global CH4 budget.
Original language | English |
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Article number | 024021 |
Journal | Environmental Research Letters |
Volume | 16 |
Early online date | 6 Jan 2021 |
DOIs | |
Publication status | Published - 3 Feb 2021 |
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