Cryoconite holes geomorphometry, spatial distribution and radiative impact over the Hells Gate Ice Shelf, East Antarctica

• Published in: Annals of Glaciology
• Main Authors: Giacomo Traversa, Riccardo Scipinotti, Samuele Pierattini, Gianluca Bianchi Fasani, Biagio Di Mauro
• Format: Article in Journal/Newspaper
• Language: English
• Published: Cambridge University Press
• Subjects: Antarctic glaciology; blue ice; ice shelves; remote sensing; Meteorology. Climatology; QC851-999; Annals of Glaciology; Antarc*; Antarctic; Antarctica; East Antarctica; Ice Sheet; Ice Shelf; Ice Shelves; Victoria Land
• Online Access: https://doi.org/10.1017/aog.2024.20; https://doaj.org/article/a04ed42eeb1042dbaf9844194ae8febe

Cryoconite holes are structures characteristic of the glacierised ablation areas, formed from dark sediment deposition which melt the glacier ice leading to their cylindrical structure formation. The present study focuses on an unstudied blue ice area of East Antarctica over the Hells Gate Ice Shelf in Northern Victoria Land. Taking advantage of neural network methodology applied on drone acquisitions, an automatic detection of cryoconite holes was carried out (88% of accuracy), mapping ~3500 m2 (0.4% fractional cover) of cryoconite holes over an area of 900 000 m2. The surveyed area showed heterogeneity in cryoconite hole distribution, with some regions showing an area fraction of holes (regions exhibiting frozen ponds and ice bands) as high as 8%. Thanks to this detection, the spatially integrated radiative forcing of cryoconite holes over blue ice surface was estimated to be almost 1 Wm−2. This estimation was based on the measured albedo difference between the two surfaces, which averages 0.31. However, the radiative forcing is strongly increased if calculated at a single cryoconite hole scale, showing an average of ~200 Wm−2. In conclusion, the present research represents a first attempt of analysing cryoconite holes as factors impacting the blue ice in Northern Victoria Land, deepening our understanding of their glaciological role at the margins of the East Antarctic Ice Sheet.