{"title":"Constraints of the enhanced snow melt in the northern Antarctic Peninsula during the 2021/22 melt season from Sentinel-1 data and in-situ observations","authors":"Kateřina Fárová , Kamil Láska , Zbyněk Engel","doi":"10.1016/j.coldregions.2025.104722","DOIUrl":null,"url":null,"abstract":"<div><div>A time series of 32 Sentinel-1 images were used to establish the constraints of the surface melt on the Trinity Peninsula and James Ross Island from October 2021 to April 2022. The consistency of the decrease in the backscatter coefficient (σ<sup>0</sup>) with the rise in air temperature above 0 °C was validated through in-situ measured meteorological data. The correlation coefficient between the air temperature characteristics and σ<sup>0</sup> was highest in the accumulation area of the glaciers on James Ross Island. A decrease of σ<sup>0</sup> by −4 dB, compared to the winter mean value, was chosen as the threshold for the melt constraint. The number of melt days, derived from the Sentinel-1 data, was in better agreement with the same characteristics retrieved from the six-day mean air temperature, than that from the sum of positive degree days. The method proved to be useful when applied to the percolation zone, but unsuitable for the termination zone of glaciers with bare ice and for the dry snow zone. The snow-melt indices were subject to detailed analysis along selected transects across the Trinity Peninsula and James Ross Island in terms of both elevation and local/regional differences. The maximum number of melt days ranged from 150 to 180 days on the west coast of the Trinity Peninsula to 90–120 days on the southeastern part of James Ross Island. The earliest occurrence and longest duration of snow melt was observed on the northwestern coast of the Trinity Peninsula. On the east coast of the Peninsula, in the area from 200 to 600 m a.s.l., the melt duration was approximately 100 days. During a significant temperature anomaly in early February 2022, the snow melt extended to the summit of Mt. Haddington. At the same time, surface snow melting advanced to an elevation of 1600 m a.s.l. on the Trinity Peninsula. Apart from this extreme event, melting at altitudes above 1000–1200 m a.s.l. was rarely observed.</div></div>","PeriodicalId":10522,"journal":{"name":"Cold Regions Science and Technology","volume":"242 ","pages":"Article 104722"},"PeriodicalIF":4.9000,"publicationDate":"2026-01-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Cold Regions Science and Technology","FirstCategoryId":"5","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0165232X25003052","RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"2025/10/20 0:00:00","PubModel":"Epub","JCR":"Q1","JCRName":"ENGINEERING, CIVIL","Score":null,"Total":0}
引用次数: 0
Abstract
A time series of 32 Sentinel-1 images were used to establish the constraints of the surface melt on the Trinity Peninsula and James Ross Island from October 2021 to April 2022. The consistency of the decrease in the backscatter coefficient (σ0) with the rise in air temperature above 0 °C was validated through in-situ measured meteorological data. The correlation coefficient between the air temperature characteristics and σ0 was highest in the accumulation area of the glaciers on James Ross Island. A decrease of σ0 by −4 dB, compared to the winter mean value, was chosen as the threshold for the melt constraint. The number of melt days, derived from the Sentinel-1 data, was in better agreement with the same characteristics retrieved from the six-day mean air temperature, than that from the sum of positive degree days. The method proved to be useful when applied to the percolation zone, but unsuitable for the termination zone of glaciers with bare ice and for the dry snow zone. The snow-melt indices were subject to detailed analysis along selected transects across the Trinity Peninsula and James Ross Island in terms of both elevation and local/regional differences. The maximum number of melt days ranged from 150 to 180 days on the west coast of the Trinity Peninsula to 90–120 days on the southeastern part of James Ross Island. The earliest occurrence and longest duration of snow melt was observed on the northwestern coast of the Trinity Peninsula. On the east coast of the Peninsula, in the area from 200 to 600 m a.s.l., the melt duration was approximately 100 days. During a significant temperature anomaly in early February 2022, the snow melt extended to the summit of Mt. Haddington. At the same time, surface snow melting advanced to an elevation of 1600 m a.s.l. on the Trinity Peninsula. Apart from this extreme event, melting at altitudes above 1000–1200 m a.s.l. was rarely observed.
期刊介绍:
Cold Regions Science and Technology is an international journal dealing with the science and technical problems of cold environments in both the polar regions and more temperate locations. It includes fundamental aspects of cryospheric sciences which have applications for cold regions problems as well as engineering topics which relate to the cryosphere.
Emphasis is given to applied science with broad coverage of the physical and mechanical aspects of ice (including glaciers and sea ice), snow and snow avalanches, ice-water systems, ice-bonded soils and permafrost.
Relevant aspects of Earth science, materials science, offshore and river ice engineering are also of primary interest. These include icing of ships and structures as well as trafficability in cold environments. Technological advances for cold regions in research, development, and engineering practice are relevant to the journal. Theoretical papers must include a detailed discussion of the potential application of the theory to address cold regions problems. The journal serves a wide range of specialists, providing a medium for interdisciplinary communication and a convenient source of reference.