TY - JOUR
T1 - In Situ Aerosol Size Spectra Measurements in the Austral Polar Vortex Before and After the Hunga Tonga-Hunga Ha'apai Volcanic Eruption
AU - Deshler, Terry
AU - Kalnajs, Lars E.
AU - Norgren, Matthew
AU - Zhu, Yunqian
AU - Zhang, Jun
N1 - Publisher Copyright:
© 2024. The Author(s).
PY - 2024/11/28
Y1 - 2024/11/28
N2 - Aerosol from the Hunga Tonga-Hunga Ha'apai (HT-HH) volcanic eruption (20.6°S) in January 2022 were not incorporated into the austral polar vortex until the following year, March 2023. Within the polar vortex in situ profiles of aerosol size spectra were completed in the austral autumns of 2019 and 2023, from McMurdo Station, Antarctica (78˚S), 30 months prior to and 15 months after the HT-HH eruption. The measurements indicate that the HT-HH impact on aerosol size was primarily confined to particles with diameters >0.5 μm leading to differences in aerosol mass, surface area, and extinction from factors of 2–4 at the volcanic layer's peak below 20 km, increasing to ratios of 5–10 above 20 km. Effective radius, with radiative and microphysical implications, increased from ∼0.2 to ∼0.3 μm. An Earth system model with a modal aerosol package compares favorably with the in situ measurements of the HT-HH aerosol impact.
AB - Aerosol from the Hunga Tonga-Hunga Ha'apai (HT-HH) volcanic eruption (20.6°S) in January 2022 were not incorporated into the austral polar vortex until the following year, March 2023. Within the polar vortex in situ profiles of aerosol size spectra were completed in the austral autumns of 2019 and 2023, from McMurdo Station, Antarctica (78˚S), 30 months prior to and 15 months after the HT-HH eruption. The measurements indicate that the HT-HH impact on aerosol size was primarily confined to particles with diameters >0.5 μm leading to differences in aerosol mass, surface area, and extinction from factors of 2–4 at the volcanic layer's peak below 20 km, increasing to ratios of 5–10 above 20 km. Effective radius, with radiative and microphysical implications, increased from ∼0.2 to ∼0.3 μm. An Earth system model with a modal aerosol package compares favorably with the in situ measurements of the HT-HH aerosol impact.
KW - Hunga Tonga aerosol impacts
KW - aerosol size spectra within the austral autumn polar vortex
KW - in situ measurements
KW - volcanic impacts on stratospheric aerosol
UR - https://www.scopus.com/pages/publications/85208825745
U2 - 10.1029/2024GL111388
DO - 10.1029/2024GL111388
M3 - Article
AN - SCOPUS:85208825745
SN - 0094-8276
VL - 51
JO - Geophysical Research Letters
JF - Geophysical Research Letters
IS - 22
M1 - e2024GL111388
ER -