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Earth system science data
11 (2019): 1–22. doi:10.5194/essd-11-1-2019
info:cnr-pdr/source/autori:Giuseppe Etiope1,2, Giancarlo Ciotoli3,1, Stefan Schwietzke4,5,a, and Martin Schoell6/titolo:Gridded maps of geological methane emissions and their isotopic signature/doi:10.5194%2Fessd-11-1-2019/rivista:Earth system science data (Print)/anno:2019/pagina_da:1/pagina_a:22/intervallo_pagine:1–22/volume:11
Earth System Science Data, Vol 11, Pp 1-22 (2019)
11 (2019): 1–22. doi:10.5194/essd-11-1-2019
info:cnr-pdr/source/autori:Giuseppe Etiope1,2, Giancarlo Ciotoli3,1, Stefan Schwietzke4,5,a, and Martin Schoell6/titolo:Gridded maps of geological methane emissions and their isotopic signature/doi:10.5194%2Fessd-11-1-2019/rivista:Earth system science data (Print)/anno:2019/pagina_da:1/pagina_a:22/intervallo_pagine:1–22/volume:11
Earth System Science Data, Vol 11, Pp 1-22 (2019)
Methane (CH4) is a powerful greenhouse gas, whose natural and anthropogenic emissions contribute ∼20 % to global radiative forcing. Its atmospheric budget (sources and sinks), however, has large uncertainties. Inverse modelling, using atmospheric