Comment on “An approach to sulfate geoengineering with surface emissions of carbonyl sulfide” by Quaglia et al. (2022)

Marc von Hobe, Christoph Brühl, Sinikka T. Lennartz, Mary E. Whelan, and Aleya Kaushik

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Feb 2023	69	21	1	91
Mar 2023	231	62	11	304
Apr 2023	49	20	6	75
May 2023	28	15	2	45
Jun 2023	233	38	8	279
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Jan 2024	15	9	1	25
Feb 2024	18	8	1	27
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Apr 2024	17	4	3	24
May 2024	8	1	3	12

Cumulative views and downloads (calculated since 28 Feb 2023)

Month	HTML	PDF	XML	Total
Feb 2023	69	21	1	91
Mar 2023	231	62	11	304
Apr 2023	49	20	6	75
May 2023	28	15	2	45
Jun 2023	233	38	8	279
Jul 2023	95	11	1	107
Aug 2023	82	11	2	95
Sep 2023	67	5	1	73
Oct 2023	87	10	1	98
Nov 2023	45	8	0	53
Dec 2023	38	10	3	51
Jan 2024	15	9	1	25
Feb 2024	18	8	1	27
Mar 2024	22	15	1	38
Apr 2024	17	4	3	24
May 2024	8	1	3	12

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720	127	25	872	17	21

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Latest update: 08 May 2024

Short summary

Carbonyl sulfide plays a role in the climate system as a greenhouse gas and as the major non-volcanic precursor of particles reflecting sunlight. Here, we comment on a proposal to increase the number of particles by emitting extra carbonyl sulfide at the surface. We show that the balance between aerosol cooling and greenhouse gas warming may not be as favorable as suggested and also that much of the carbonyl sulfide emissions will actually be taken up by the biosphere and the oceans.