TY - JOUR
T1 - Observations of clouds, aerosols, precipitation, and surface radiation over the southern ocean
AU - McFarquhar, Greg M.
AU - Bretherton, Christopher S.
AU - Marchand, Roger
AU - Protat, Alain
AU - DeMott, Paul J.
AU - Alexander, Simon P.
AU - Roberts, Greg C.
AU - Twohy, Cynthia H.
AU - Toohey, Darin
AU - Siems, Steve
AU - Huang, Yi
AU - Wood, Robert
AU - Rauber, Robert M.
AU - Lasher-Trapp, Sonia
AU - Jensen, Jorgen
AU - Stith, Jeffrey L.
AU - Mace, Jay
AU - Um, Junshik
AU - Järvinen, Emma
AU - Schnaiter, Martin
AU - Gettelman, Andrew
AU - Sanchez, Kevin J.
AU - McCluskey, Christina S.
AU - Russell, Lynn M.
AU - McCoy, Isabel L.
AU - Atlas, Rachel L.
AU - Bardeen, Charles G.
AU - Moore, Kathryn A.
AU - Hill, Thomas C.J.
AU - Humphries, Ruhi S.
AU - Keywood, Melita D.
AU - Ristovski, Zoran
AU - Cravigan, Luke
AU - Schofield, Robyn
AU - Fairall, Chris
AU - Mallet, Marc D.
AU - Kreidenweis, Sonia M.
AU - Rainwater, Bryan
AU - D'Alessandro, John
AU - Wang, Yang
AU - Wu, Wei
AU - Saliba, Georges
AU - Levin, Ezra J.T.
AU - Ding, Saisai
AU - Lang, Francisco
AU - Truong, Son C.H.
AU - Wolff, Cory
AU - Haggerty, Julie
AU - Harvey, Mike J.
AU - Klekociuk, Andrew R.
AU - McDonald, Adrian
N1 - Publisher Copyright:
© 2021 American Meteorological Society. All rights reserved.
PY - 2021/5
Y1 - 2021/5
N2 - Weather and climate models are challenged by uncertainties and biases in simulating Southern Ocean (SO) radiative fluxes that trace to a poor understanding of cloud, aerosol, precipitation, and radiative processes, and their interactions. Projects between 2016 and 2018 used in situ probes, radar, lidar, and other instruments to make comprehensive measurements of thermodynamics, surface radiation, cloud, precipitation, aerosol, cloud condensation nuclei (CCN), and ice nucleating particles over the SO cold waters, and in ubiquitous liquid and mixed-phase clouds common to this pristine environment. Data including soundings were collected from the NSF-NCAR G-V aircraft flying north-south gradients south of Tasmania, at Macquarie Island, and on the R/V Investigator and RSV Aurora Australis. Synergistically these data characterize boundary layer and free troposphere environmental properties, and represent the most comprehensive data of this type available south of the oceanic polar front, in the cold sector of SO cyclones, and across seasons. Results show largely pristine environments with numerous small and few large aerosols above cloud, suggesting new particle formation and limited long-range transport from continents, high variability in CCN and cloud droplet concentrations, and ubiquitous supercooled water in thin, multilayered clouds, often with small-scale generating cells near cloud top. These observations demonstrate how cloud properties depend on aerosols while highlighting the importance of dynamics and turbulence that likely drive heterogeneity of cloud phase. Satellite retrievals confirmed low clouds were responsible for radiation biases. The combination of models and observations is examining how aerosols and meteorology couple to control SO water and energy budgets.
AB - Weather and climate models are challenged by uncertainties and biases in simulating Southern Ocean (SO) radiative fluxes that trace to a poor understanding of cloud, aerosol, precipitation, and radiative processes, and their interactions. Projects between 2016 and 2018 used in situ probes, radar, lidar, and other instruments to make comprehensive measurements of thermodynamics, surface radiation, cloud, precipitation, aerosol, cloud condensation nuclei (CCN), and ice nucleating particles over the SO cold waters, and in ubiquitous liquid and mixed-phase clouds common to this pristine environment. Data including soundings were collected from the NSF-NCAR G-V aircraft flying north-south gradients south of Tasmania, at Macquarie Island, and on the R/V Investigator and RSV Aurora Australis. Synergistically these data characterize boundary layer and free troposphere environmental properties, and represent the most comprehensive data of this type available south of the oceanic polar front, in the cold sector of SO cyclones, and across seasons. Results show largely pristine environments with numerous small and few large aerosols above cloud, suggesting new particle formation and limited long-range transport from continents, high variability in CCN and cloud droplet concentrations, and ubiquitous supercooled water in thin, multilayered clouds, often with small-scale generating cells near cloud top. These observations demonstrate how cloud properties depend on aerosols while highlighting the importance of dynamics and turbulence that likely drive heterogeneity of cloud phase. Satellite retrievals confirmed low clouds were responsible for radiation biases. The combination of models and observations is examining how aerosols and meteorology couple to control SO water and energy budgets.
KW - Aerosol-cloud interaction
KW - Cloud microphysics
KW - Cloud radiative effects
KW - Cloud water/phase
KW - Radiation budgets
KW - Southern Ocean
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U2 - 10.1175/BAMS-D-20-0132.1
DO - 10.1175/BAMS-D-20-0132.1
M3 - Article
AN - SCOPUS:85106668029
SN - 0003-0007
VL - 102
SP - E894-E928
JO - Bulletin of the American Meteorological Society
JF - Bulletin of the American Meteorological Society
IS - 4
ER -