1. Characterizing Precipitation and Improving Rainfall Estimates Over the Southern Ocean Using Ship‐Borne Disdrometer and Dual‐Polarimetric C‐Band Radar.
- Author
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Aragon, L. G. B., Huang, Y., May, P. T., Crosier, J., Montoya Duque, E., Connolly, P. J., and Bower, K. N.
- Subjects
HYDROLOGIC cycle ,RAINDROP size ,RADAR ,CYCLONES ,OCEAN ,RAINFALL ,RAIN gauges - Abstract
Large satellite discrepancies and model biases in representing precipitation over the Southern Ocean (SO) are related directly to the region's limited surface observations of precipitation. To help address this knowledge gap, the study investigated the precipitation characteristics and rain rate retrievals over the remote SO using ship‐borne data of the Ocean Rainfall And Ice‐phase precipitation measurement Network disdrometer (OceanRAIN) and dual‐polarimetric C‐band radar (OceanPOL) aboard the Research Vessel (RV) Investigator in the Austral warm seasons of 2016–2018. Seven distinct synoptic types over the SO were analyzed based on their radar polarimetric signatures, surface precipitation phase, and rain microphysical properties. OceanRAIN observations revealed that the SO precipitation was dominated by drizzle and light rain, with small‐sized raindrops (diameter <1 mm) constituting up to 47% of total accumulation. Precipitation occurred most frequently over the warm sector of extratropical cyclones, while concentrations of large‐sized raindrops (diameter >3 mm) were prominent over synoptic types with colder and more convectively unstable environments. OceanPOL observations complement and extend the surface precipitation properties sampled by OceanRAIN, providing unique information to help characterize the variety of potential precipitation types and associated mechanisms under different synoptic conditions. Raindrop size distributions (DSD) measured with OceanRAIN over the SO were better characterized by analytical DSD forms with two‐shape parameters than single‐shape parameters currently implemented in satellite retrieval algorithms. This study also revised a rainfall retrieval algorithm for C‐band radars to reflect the large amount of small drops and provide improved radar rainfall estimates over the SO. Plain Language Summary: Precipitation is a major component of the hydrologic cycle in high‐latitude regions including the remote Southern Ocean (SO). However, large differences continue to exist among current precipitation products in the region, owing in part to the absence of high‐quality surface observational records suitable for evaluation across a range of temporal and spatial scales. This work uses two instruments aboard the RV Investigator over the Australian sector of the SO in the Austral warm seasons of 2016–2018: the OceanRAIN disdrometer and OceanPOL radar. We found variability in radar features and surface precipitation properties among seven distinct synoptic conditions over the SO. This work also discussed two important findings related to remote sensing retrievals of SO rain. First, we demonstrated why the rainfall retrieval assumptions in satellite algorithms may need to be refined to account for the unique rainfall properties in the SO. Second, we formulated a new set of equations suitable for shipborne C‐band radars in improving rain rate estimates over the region. This work leads toward more accurate, high‐resolution estimates of precipitation over the measurement‐sparse SO to better understand a range of climatological and meteorological processes in the region. Key Points: Different synoptic types across the Southern Ocean exhibit distinctive polarimetric signatures and surface precipitation propertiesSmall raindrops of less than one millimeter contribute up to 47% of total accumulation during the Austral warm seasons over the regionA new formulation for radar rainfall estimates that reflects the large numbers of small drops over the Southern Ocean is proposed [ABSTRACT FROM AUTHOR]
- Published
- 2024
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