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The added value of satellite observations of methane forunderstanding the contemporary methane budget
Author(s) -
Paul I. Palmer,
Liang Feng,
Mark F. Lunt,
Robert J. Parker,
Hartmut Bösch,
Xin Lan,
Alba Lorente,
Tobias Borsdorff
Publication year - 2021
Publication title -
philosophical transactions of the royal society a mathematical physical and engineering sciences
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.074
H-Index - 169
eISSN - 1471-2962
pISSN - 1364-503X
DOI - 10.1098/rsta.2021.0106
Subject(s) - environmental science , atmospheric methane , greenhouse gas , methane , satellite , atmospheric sciences , troposphere , sciamachy , global warming , climatology , climate change , meteorology , geography , geology , physics , chemistry , oceanography , astronomy , organic chemistry
Surface observations have recorded large and incompletely understood changes to atmospheric methane (CH4 ) this century. However, their ability to reveal the responsible surface sources and sinks is limited by their geographical distribution, which is biased towards the northern midlatitudes. Data from Earth-orbiting satellites designed specifically to measure atmospheric CH4 have been available since 2009 with the launch of the Japanese Greenhouse gases Observing SATellite (GOSAT). We assess the added value of GOSAT to data collected by the US National Oceanic and Atmospheric Administration (NOAA), which have been the lynchpin for knowledge about atmospheric CH4 since the 1980s. To achieve that we use the GEOS-Chem atmospheric chemistry transport model and an inverse method to infera posteriori flux estimates from the NOAA and GOSAT data using commona priori emission inventories. We find the main benefit of GOSAT data is from its additional coverage over the tropics where we report large increases since the 2014/2016 El Niño, driven by biomass burning, biogenic emissions and energy production. We use data from the European TROPOspheric Monitoring Instrument to show how better spatial coverage and resolution measurements allow us to quantify previously unattainable diffuse sources of CH4 , thereby opening up a new research frontier.This article is part of a discussion meeting issue ‘Rising methane: is warming feeding warming? (part 1)’.

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