4.5 Article

Cloud phase and macrophysical properties over the Southern Ocean during the MARCUS field campaign

Journal

ATMOSPHERIC MEASUREMENT TECHNIQUES
Volume 15, Issue 12, Pages 3761-3777

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/amt-15-3761-2022

Keywords

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Funding

  1. National Science Foundation (NSF) at the University of Arizona [AGS-2031750]

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This study investigated cloud phase and macrophysical properties over the Southern Ocean using meteorological measurements. The findings revealed key features of cloud cover, cloud types, and cloud layer temperatures. The study showed that the polar region had higher cloud cover, with low-level and deep convective clouds being the most common cloud types. Mixed-phase clouds were found to be more prevalent in the southern region. These findings are important for improving climate model simulations over the Southern Ocean.
To investigate the cloud phase and macrophysical properties over the Southern Ocean (SO), the Department of Energy (DOE) Atmospheric Radiation Measurement (ARM) Mobile Facility (AMF2) was installed on the Australian ice-breaker research vessel (R/V) Aurora Australis during the Measurements of Aerosols, Radiation, and Clouds over the Southern Ocean (MARCUS) field campaign (41 to 69 degrees S, 60 to 160 degrees E) from October 2017 to March 2018. To examine cloud properties over the midlatitude and polar regions, the study domain is separated into the northern (NSO) and southern (SSO) parts of the SO, with a demarcation line of 60 degrees S. The total cloud fractions (CFs) were 77.9 %, 67.6 %, and 90.3% for the entire domain, NSO and SSO, respectively, indicating that higher CFs were observed in the polar region. Low-level clouds and deep convective clouds are the two most common cloud types over the SO. A new method was developed to classify liquid, mixed-phase, and ice clouds in single-layered, low-level clouds (LOW), where mixed-phase clouds dominate with an occurrence frequency (Freq) of 54.5 %, while the Freqs of the liquid and ice clouds were 10.1% (most drizzling) and 17.4% (least drizzling). The meridional distributions of low-level cloud boundaries are nearly independent of latitude, whereas the cloud temperatures increased by similar to 8 K, and atmospheric precipitable water vapor increased from similar to 5 mm at 69 degrees S to similar to 18 mm at 43 degrees S. The mean cloud liquid water paths over NSO were much larger than those over SSO. Most liquid clouds occurred over NSO, with very few over SSO, whereas more mixed-phase clouds occurred over SSO than over NSO. There were no significant differences for the ice cloud Freq between NSO and SSO. The ice particle sizes are comparable to cloud droplets and drizzle drops and well mixed in the cloud layer. These results will be valuable for advancing our understanding of the meridional and vertical distributions of clouds and can be used to improve model simulations over the SO.

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