Detection of Antarctic surface meltwater using Sentinel-2 remote sensing images via U-Net with attention blocks: A case study over the Amery Ice Shelf

• Published in: IEEE transactions on geoscience and remote sensing 2023-01, Vol.61, p.1-1
• Main Authors: Niu, Lihang, Tang, Xueyuan, Yang, Shuhu, Zhang, Yun, Zheng, Lei, Wang, Lijuan
• Format: Article
• Language: English
• Subjects: Air Content; Amery Ice Shelf; Antarctica; Artificial intelligence; attention mechanism; Channels; Deep learning; Firn; Ice shelf; Ice shelves; Katabatic winds; Land ice; Mass balance; Meltwater; Ocean temperature; Polar environments; Remote sensing; Sea level changes; Sea level rise; Sea surface; Snow; Snowfall; Snowmelt; Solar radiation; Spatial distribution; surface meltwater; Surface water; Task analysis; Temperature; Water bodies; Winds
• ISSN: 0196-2892; 1558-0644
• DOI: 10.1109/TGRS.2023.3275076

Surface meltwater critically impacts the Antarctic mass balance and global sea level rise. Quantifying the extent of surface meltwater in Antarctica on a large scale is a challenging task. Traditional methods, such as thresholding, have many limitations. We used a deep learning method, the U-Net with attention blocks, to automatically extract surface meltwater from Sentinel-2 images. We inserted attention mechanism blocks into U-Net to assign different weights to all pixels and channels to utilize the high resolution and multiple channels of Sentinel-2 images. The model was used to map surface water bodies in Sentinel-2 images, and the average accuracy reached 0.9969 on the test dataset. In East Antarctica, the Amery Ice Shelf (AIS) exhibits the largest surface meltwater area. Studying surface meltwater dynamics on the AIS is useful for understanding the East Antarctic mass balance and demonstrating the model performance. We analyzed the classification results for surface water bodies on the AIS from January 2017-2022. Spatially, 96% of surface water bodies are concentrated inland of the AIS from 70-73°S and account for 93% of the region 20 km from the coastline of the AIS. Temporally, the water body area varies considerably in different years, with a maximum in 2017 (932.54 km 2 ) and a minimum in 2021 (58.34 km 2 ). The spatial distribution of surface water body on the AIS is controlled by the firn air content, katabatic winds, bare rocks and blue ice. The interannual variability is associated with complex climate factors, including temperature, surface net solar radiation, snowfall, and snowmelt, among which temperature and snowfall show strong correlation.