1. Impact of Giant Iceberg A68A on the Physical Conditions of the Surface South Atlantic, Derived Using Remote Sensing.
- Author
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Smith, R. M. and Bigg, G. R.
- Subjects
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REMOTE sensing , *ICEBERGS , *SEAWATER salinity , *OCEAN temperature , *PHYSICAL measurements , *SURFACE temperature - Abstract
Giant icebergs release cold, fresh meltwater as they drift, perturbing the physical conditions of the surface ocean. This study uses satellite‐derived sea surface salinity and temperature measurements to explore the physical impact of supergiant iceberg A68A between September 2020 and June 2021. During A68A's drift through the Scotia Sea in austral spring, gradual but persistent edge‐wasting contributed to a freshening of several psu extending hundreds of kilometers ahead of the iceberg, whilst the cooling signal was more pronounced in the iceberg's wake. The magnitude of the physical perturbation intensified during A68A's breakup near South Georgia. Several large meltwater lenses surrounding the descendant icebergs displayed temperature anomalies of up to −4.5°C, whilst the salinity measurements indicated a surface (skin‐depth) anomaly regularly exceeding order −10 psu. The perturbations stretched at times >1,000 km and persisted for >2 months following A68A's melt in April 2021. Plain Language Summary: Giant icebergs release cold, fresh meltwater as they drift, altering the conditions of the ocean. This study uses sea surface salinity and temperature data collected by satellites to explore these impacts for iceberg A68 between September 2020 and June 2021. During A68A's drift through the Scotia Sea, a freshening of several psu extended hundreds of kilometers ahead of the iceberg, and a pronounced cooling followed behind. The magnitude of the salinity and temperature anomalies intensified when A68A fragmented near South Georgia. The surface ocean displayed temperature anomalies of up to −4.5°C, and salinity anomalies regularly exceeding −10 psu. The perturbation stretched at times >1,000 km and persisted for >2 months following A68A's melt in April 2021. Key Points: Meltwater released from giant iceberg A68A caused large scale freshening and cooling of the surrounding surface oceanIntense temperature and salinity anomalies up to −4.5°C and exceeding −10 psu were recorded during the breakup near South GeorgiaThe freshening and cooling signals stretched at times over 1,000 km and persisted for over 2 months following the iceberg's melt [ABSTRACT FROM AUTHOR]
- Published
- 2023
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