13 citations as recorded by crossref.

1. Why does stratospheric aerosol forcing strongly cool the warm pool? M. Günther et al. 10.5194/acp-24-7203-2024
2. Indirect stratospheric moisture increase after a Pinatubo-magnitude eruption can be comparable to direct increase after 2022 Hunga C. Kroll & A. Schmidt 10.1038/s43247-024-01651-w
3. The Influence of Internal Climate Variability on Stratospheric Water Vapor Increases After Large‐Magnitude Explosive Tropical Volcanic Eruptions X. Zhou et al. 10.1029/2023GL103076
4. Volcanic effects on climate: recent advances and future avenues L. Marshall et al. 10.1007/s00445-022-01559-3
5. Assessing the impact of very large volcanic eruptions on the risk of extreme climate events N. Freychet et al. 10.1088/2752-5295/acee9f
6. Tonga volcanic eruption triggered anomalous Arctic warming in early 2022 Y. Bao et al. 10.1016/j.ocemod.2023.102258
7. Reckoning with the Rocky Relationship Between Eruption Size and Climate Response: Toward a Volcano-Climate Index A. Schmidt & B. Black 10.1146/annurev-earth-080921-052816
8. Stratospheric water vapour and ozone response to the quasi-biennial oscillation disruptions in 2016 and 2020 M. Diallo et al. 10.5194/acp-22-14303-2022
9. Out of the blue: Volcanic SO2 emissions during the 2021–2022 eruptions of Hunga Tonga—Hunga Ha’apai (Tonga) S. Carn et al. 10.3389/feart.2022.976962
10. The impact of stratospheric aerosol heating on the frozen hydrometeor transport pathways in the tropical tropopause layer C. Kroll et al. 10.1088/1748-9326/ad33d0
11. Microphysical Interactions Determine the Effectiveness of Solar Radiation Modification via Stratospheric Solid Particle Injection S. Vattioni et al. 10.1029/2024GL110575
12. The Sensitivity of Moisture Flux Partitioning in the Cold‐Point Tropopause to External Forcing C. Kroll et al. 10.1029/2022GL102262
13. Sensitivity of regional monsoons to idealised equatorial volcanic eruption of different sulfur emission strengths R. D’Agostino & C. Timmreck 10.1088/1748-9326/ac62af