Oceans

Halogens emitted from oceans excited global warming of methane in the atmosphere

An international team, led by researchers from the Spanish National Research Council (CSIC), has performed climate-related chemistry simulations to assess the impact of oceanic emissions of halogenated compounds (iodine, bromine and chlorine) on methane in the atmosphere, the second most important contributor to global warming after carbon dioxide (CO2). The results, published in Nature Communicationsreveal that the emission of these compounds over the century has increased the lifetime and greenhouse effect of methane by 6% to 9%.

Methane is the most abundant reactive greenhouse gas. However, unlike CO2Current climate models underestimate the lifetime of methane, thereby indicating that there are still uncertainties in its emission and removal processes from the atmosphere.

“This work highlights the importance of considering the chemical complexity of our atmosphere when forecasting the effect of methane on global warming in future climate scenarios,” explains CSIC researcher and coordinator of this study Alfonso Saiz López, from the Instituto de Química Física Rocasolano (IQFR) -CSIC),

Ocean halogens are produced by biological activity and photochemical reactions at the ocean surface, from where they are transferred to the atmosphere. According to the researchers, the increase in methane concentration due to halogens will be equivalent at the end of the century to the increase in methane in the atmosphere over the last three to four decades.

“This work evaluates for the first time the effect of halogen chemistry on atmospheric methane over this century, for two different climate scenarios. The analysis of the results shows that the increase in methane persistence in the atmosphere when halogens are included is significant and similar in both climate scenarios, “says Saiz-López.

The results of the study, framed within the international ERC-Consolidator Climahal project, show that the inclusion of the emissions and chemistry of these compounds increases the atmospheric lifetime of methane and, thus, the current gap between model estimates and observations of the atmospheric lifetime of methane is reduced.

Qinyi Li, researcher at IQFR-CSIC and first author of the paper, emphasizes: “Our results indicate that the chemistry of methaneated compounds emitted from the oceans, and so far not considered in climate models, should be incorporated in future climate simulations assessing the influence of methane on global warming during this century “.

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