Does prognostic seeding along flight tracks produce the desired effects of cirrus cloud thinning?

Abstract µ m and scale the mass emissions of seeding particles by at least a factor of 100 or 1000. This latter scaling factor led to a large net top-of-atmosphere (TOA) warming effect of 5.9 W m- 2 > 10 5 - 1 - 2 × 1000, scenario. We attributed this peculiar behavior to the differences in the competition between different seeding particle concentrations and background particles. Finally, we also found that seeding with such large concentrations increased the albedo effect of mixed-phase clouds in the NH due to less efficient cloud droplet consumption, consistent with previous findings from our model. Overall, however, based on this study it is recommended to pause further modeling efforts of CCT unless more observational-based evidence of aerosol–ice-cloud interactions indicates favorable conditions for producing the desired outcome of this CI proposal.

Standort
Deutsche Nationalbibliothek Frankfurt am Main
Umfang
Online-Ressource
Sprache
Englisch

Erschienen in
Does prognostic seeding along flight tracks produce the desired effects of cirrus cloud thinning? ; volume:23 ; number:13 ; year:2023 ; pages:7673-7698 ; extent:26
Atmospheric chemistry and physics ; 23, Heft 13 (2023), 7673-7698 (gesamt 26)

Urheber
Tully, Colin
Neubauer, David
Villanueva, Diego
Lohmann, Ulrike

DOI
10.5194/acp-23-7673-2023
URN
urn:nbn:de:101:1-2023072004341000511929
Rechteinformation
Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
Letzte Aktualisierung
14.08.2025, 10:46 MESZ

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