TY - JOUR
T1 - Characterizing the Occurrence and Spatial Heterogeneity of Liquid, Ice, and Mixed Phase Low-Level Clouds Over the Southern Ocean Using in Situ Observations Acquired During SOCRATES
AU - D'Alessandro, John J.
AU - McFarquhar, Greg Michael
AU - Wu, Wei
AU - Stith, Jeff L.
AU - Jensen, Jorgen B.
AU - Rauber, Robert M.
N1 - Funding Information:
This work was supported by the National Science Foundation (NSF) through grants AGS-1628674 and AGS-1762096. This material is based upon work supported by the National Center for Atmospheric Research, which is a major facility sponsored by the National Science Foundation under Cooperative Agreement No. 1852977. The data were collected using NSF's Lower Atmosphere Observing Facilities, which are managed and operated by NCAR's Earth Observing Laboratory. The authors thank the pilots, mechanics, technicians, scientists, software engineers, and project managers of the NCAR EOL Research Aviation Facility for their support in the field and in post-processing data. The authors would like to thank the Australian Bureau of Meteorology Tasmanian regional Office for the excellent forecast support and weather briefings provided during the field campaign with special thanks to Scott Carpentier, Michelle Hollister, Matthew Thomas, and Robert Schaap.
Funding Information:
This work was supported by the National Science Foundation (NSF) through grants AGS‐1628674 and AGS‐1762096. This material is based upon work supported by the National Center for Atmospheric Research, which is a major facility sponsored by the National Science Foundation under Cooperative Agreement No. 1852977. The data were collected using NSF's Lower Atmosphere Observing Facilities, which are managed and operated by NCAR's Earth Observing Laboratory. The authors thank the pilots, mechanics, technicians, scientists, software engineers, and project managers of the NCAR EOL Research Aviation Facility for their support in the field and in post‐processing data. The authors would like to thank the Australian Bureau of Meteorology Tasmanian regional Office for the excellent forecast support and weather briefings provided during the field campaign with special thanks to Scott Carpentier, Michelle Hollister, Matthew Thomas, and Robert Schaap.
Publisher Copyright:
© 2021. American Geophysical Union. All Rights Reserved.
PY - 2021/6/16
Y1 - 2021/6/16
N2 - Supercooled liquid water (SLW) and mixed phase clouds containing SLW and ice over the Southern Ocean (SO) are poorly represented in global climate and numerical weather prediction models. Observed SLW exists at lower temperatures than threshold values used to characterize its detrainment from convection in model parameterizations, and processes controlling its formation and removal are poorly understood. High-resolution observations are needed to better characterize SLW over the SO. This study characterizes the frequency and spatial distribution of different cloud phases (liquid, ice, and mixed) using in situ observations acquired during the Southern Ocean Clouds, Radiation, Aerosol Transport Experiment Study. Cloud particle phase is identified using multiple cloud probes. Results show occurrence frequencies of liquid phase samples up to 70% between −20°C and 0°C and of ice phase samples up to 10% between −5°C and 0°C. Cloud phase spatial heterogeneity is determined by relating the total number of 1 s samples from a given cloud to the number of segments whose neighboring samples are the same phase. Mixed phase conditions are the most spatially heterogeneous from −20°C to 0°C, whereas liquid phase conditions from −10°C to 0°C and ice phase conditions from −20°C to −10°C are the least spatially heterogeneous. Greater spatial heterogeneity is associated with broader distributions of vertical velocity. Decreasing droplet concentrations and increasing number-weighted mean liquid diameters occur within mixed phase clouds as the liquid water fraction decreases, possibly suggesting preferential evaporation of smaller drops during the Wegener-Bergeron-Findeisen process.
AB - Supercooled liquid water (SLW) and mixed phase clouds containing SLW and ice over the Southern Ocean (SO) are poorly represented in global climate and numerical weather prediction models. Observed SLW exists at lower temperatures than threshold values used to characterize its detrainment from convection in model parameterizations, and processes controlling its formation and removal are poorly understood. High-resolution observations are needed to better characterize SLW over the SO. This study characterizes the frequency and spatial distribution of different cloud phases (liquid, ice, and mixed) using in situ observations acquired during the Southern Ocean Clouds, Radiation, Aerosol Transport Experiment Study. Cloud particle phase is identified using multiple cloud probes. Results show occurrence frequencies of liquid phase samples up to 70% between −20°C and 0°C and of ice phase samples up to 10% between −5°C and 0°C. Cloud phase spatial heterogeneity is determined by relating the total number of 1 s samples from a given cloud to the number of segments whose neighboring samples are the same phase. Mixed phase conditions are the most spatially heterogeneous from −20°C to 0°C, whereas liquid phase conditions from −10°C to 0°C and ice phase conditions from −20°C to −10°C are the least spatially heterogeneous. Greater spatial heterogeneity is associated with broader distributions of vertical velocity. Decreasing droplet concentrations and increasing number-weighted mean liquid diameters occur within mixed phase clouds as the liquid water fraction decreases, possibly suggesting preferential evaporation of smaller drops during the Wegener-Bergeron-Findeisen process.
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U2 - 10.1029/2020JD034482
DO - 10.1029/2020JD034482
M3 - Article
AN - SCOPUS:85107476126
VL - 126
JO - Journal of Geophysical Research: Atmospheres
JF - Journal of Geophysical Research: Atmospheres
SN - 2169-897X
IS - 11
M1 - e2020JD034482
ER -