HIGHLIGHTS
SUMMARY
A significant contribution to this monitoring is expected from observations of atmospheric composition and atmospheric inversion systems (IPCC, 2019; European Commission et_al, 2016; Pinty et_al, 2017). The development of spaceborne imagery of the vertically integrated column of CO2 (XCO2 ), at spatial resolution better than 5 km, should make it possible to detect plumes downwind from anthropogenic sources of CO2 (Pillai et_al, 2016; Schwandner et_al, 2017; Broquet et_al, 2018). A key example of such imagery is the Copernicus Anthropogenic Carbon Dioxide Monitoring (CO2M; Pinty et_al, 2017; Kuhlmann et_al, 2019; Lespinas et_al, 2020) constellation, which is . . .
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