Quantifying dissolution rates of Antarctic icebergs in open water

• Published in: Annals of Glaciology
• Main Authors: Olav Orheim, A. Barry Giles, T. H. (Jo) Jacka, Geir Moholdt
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press
• Subjects: Antarctic glaciology; ice/ocean interactions; iceberg calving; icebergs; Meteorology. Climatology; QC851-999; Antarctic; Antarctic Peninsula; Greenwich; Southern Ocean; The Antarctic; Weddell; Weddell Sea; Annals of Glaciology; Antarc*; Iceberg*; South Atlantic Ocean
• Online Access: https://doi.org/10.1017/aog.2023.26; https://doaj.org/article/9dfa9665f2d1468fbfaa0416f230d5e4

At any one time 130 000 icebergs are afloat in the Southern Ocean; 97% of these are too small to be registered in current satellite-based databases, yet the melting of these small icebergs provides a major input to the Southern Ocean. We use a unique set of visual size observations of 53 000 icebergs in the South Atlantic Ocean, the SCAR International Iceberg Database, to derive average iceberg dissolution rates. Fracture into two parts is the dominant dissolution process for tabular icebergs, with an average half-life of 30 days for icebergs <4 km length and 60 days for larger icebergs. Complete shatter producing many icebergs <1 km length is rare. A side attrition rate of 0.23 m d−1 combined with drift speed of 6 km d−1, or any proportional change in both numbers fits the observed changes in iceberg distribution. The largest injection into the Southern Ocean of fresh water and any iceberg-transported material takes place in a ~2.3 × 10⁶ km2 zone extending east-northeast from the Antarctic Peninsula to the Greenwich meridian. The iceberg contribution to salinities and temperatures, with maximum contribution north of the Weddell Sea, differs in some regions, from those indicated by tracking large icebergs.