Persistent Supercooled Drizzle at Temperatures Below −25 °C Observed at McMurdo Station, Antarctica

Israel Silber, Ann M. Fridlind, Johannes Verlinde, Andrew S. Ackerman, Yao Sheng Chen, David H. Bromwich, Sheng Hung Wang, Maria Cadeddu, Edwin W. Eloranta

Research output: Contribution to journalArticle

Abstract

The rarity of reports in the literature of brief and spatially limited observations of drizzle at temperatures below −20 °C suggest that riming and other temperature-dependent cloud microphysical processes such as heterogeneous ice nucleation and ice crystal depositional growth prevent drizzle persistence in cold environments. In this study, we report on a persistent drizzle event observed by ground-based remote sensing measurements at McMurdo Station, Antarctica. The temperatures in the drizzle-producing cloud were below −25 °C and the drizzle persisted for a period exceeding 7.5 hr. Using ground-based, satellite, and reanalysis data, we conclude that drizzle was likely present in parts of a widespread cloud field, which stretched more than ~1,000 km along the Ross Ice Shelf coast. Parameter space sensitivity tests using two-moment bulk microphysics in large eddy simulations constrained by the observations suggest that activated ice freezing nuclei and accumulation-mode aerosol number concentrations aloft during this persistent drizzle period were likely on the order of 0.2 L−1 and 20 cm−3, respectively. In such constrained simulations, the drizzle moisture flux through cloud base exceeds that of ice. The simulations also indicate that drizzle can lead to the formation of multiple peaks in cloud water content profiles. This study suggests that persistent drizzle at these low temperatures may be common at the low aerosol concentrations typical of the Antarctic and Southern Ocean atmospheres.

Original languageEnglish (US)
Pages (from-to)10878-10895
Number of pages18
JournalJournal of Geophysical Research: Atmospheres
Volume124
Issue number20
DOIs
StatePublished - Oct 27 2019

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drizzle
Ice
Antarctic regions
Antarctica
ice
stations
aerosols
temperature
Aerosols
Antarctic Ocean
Ross ice shelf
ice nucleation
Temperature
remote sensing
crystals
Large eddy simulation
large eddy simulation
freezing
Crystallization
coasts

All Science Journal Classification (ASJC) codes

  • Geophysics
  • Forestry
  • Oceanography
  • Aquatic Science
  • Ecology
  • Water Science and Technology
  • Soil Science
  • Geochemistry and Petrology
  • Earth-Surface Processes
  • Atmospheric Science
  • Earth and Planetary Sciences (miscellaneous)
  • Space and Planetary Science
  • Palaeontology

Cite this

Silber, Israel ; Fridlind, Ann M. ; Verlinde, Johannes ; Ackerman, Andrew S. ; Chen, Yao Sheng ; Bromwich, David H. ; Wang, Sheng Hung ; Cadeddu, Maria ; Eloranta, Edwin W. / Persistent Supercooled Drizzle at Temperatures Below −25 °C Observed at McMurdo Station, Antarctica. In: Journal of Geophysical Research: Atmospheres. 2019 ; Vol. 124, No. 20. pp. 10878-10895.
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abstract = "The rarity of reports in the literature of brief and spatially limited observations of drizzle at temperatures below −20 °C suggest that riming and other temperature-dependent cloud microphysical processes such as heterogeneous ice nucleation and ice crystal depositional growth prevent drizzle persistence in cold environments. In this study, we report on a persistent drizzle event observed by ground-based remote sensing measurements at McMurdo Station, Antarctica. The temperatures in the drizzle-producing cloud were below −25 °C and the drizzle persisted for a period exceeding 7.5 hr. Using ground-based, satellite, and reanalysis data, we conclude that drizzle was likely present in parts of a widespread cloud field, which stretched more than ~1,000 km along the Ross Ice Shelf coast. Parameter space sensitivity tests using two-moment bulk microphysics in large eddy simulations constrained by the observations suggest that activated ice freezing nuclei and accumulation-mode aerosol number concentrations aloft during this persistent drizzle period were likely on the order of 0.2 L−1 and 20 cm−3, respectively. In such constrained simulations, the drizzle moisture flux through cloud base exceeds that of ice. The simulations also indicate that drizzle can lead to the formation of multiple peaks in cloud water content profiles. This study suggests that persistent drizzle at these low temperatures may be common at the low aerosol concentrations typical of the Antarctic and Southern Ocean atmospheres.",
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Silber, I, Fridlind, AM, Verlinde, J, Ackerman, AS, Chen, YS, Bromwich, DH, Wang, SH, Cadeddu, M & Eloranta, EW 2019, 'Persistent Supercooled Drizzle at Temperatures Below −25 °C Observed at McMurdo Station, Antarctica', Journal of Geophysical Research: Atmospheres, vol. 124, no. 20, pp. 10878-10895. https://doi.org/10.1029/2019JD030882

Persistent Supercooled Drizzle at Temperatures Below −25 °C Observed at McMurdo Station, Antarctica. / Silber, Israel; Fridlind, Ann M.; Verlinde, Johannes; Ackerman, Andrew S.; Chen, Yao Sheng; Bromwich, David H.; Wang, Sheng Hung; Cadeddu, Maria; Eloranta, Edwin W.

In: Journal of Geophysical Research: Atmospheres, Vol. 124, No. 20, 27.10.2019, p. 10878-10895.

Research output: Contribution to journalArticle

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AU - Silber, Israel

AU - Fridlind, Ann M.

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AU - Ackerman, Andrew S.

AU - Chen, Yao Sheng

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AU - Eloranta, Edwin W.

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