2022
DOI: 10.1007/s41064-022-00215-x
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Recent Ice Trends in Swiss Mountain Lakes: 20-year Analysis of MODIS Imagery

Abstract: Depleting lake ice is a climate change indicator, just like sea-level rise or glacial retreat. Monitoring Lake Ice Phenology (LIP) is useful because long-term freezing and thawing patterns serve as sentinels to understand regional and global climate change. We report a study for the Oberengadin region of Switzerland, where several small- and medium-sized mountain lakes are located. We observe the LIP events, such as freeze-up, break-up and ice cover duration, across two decades (2000–2020) from optical satelli… Show more

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Cited by 2 publications
(2 citation statements)
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References 47 publications
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“…Following [5], we opt for a higher freeze threshold of 30% to estimate the two LIP events. I.e., ice-on is detected when <30% of the lake is not frozen, and ice-off when >30% of it returns to the non-frozen state after the freeze period.…”
Section: Ice-on/off Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…Following [5], we opt for a higher freeze threshold of 30% to estimate the two LIP events. I.e., ice-on is detected when <30% of the lake is not frozen, and ice-off when >30% of it returns to the non-frozen state after the freeze period.…”
Section: Ice-on/off Resultsmentioning
confidence: 99%
“…Lake freezing and thawing are strongly correlated to local warming of the atmosphere [5], [6], and Lake Ice Cover has been included in the list of essential climate variables [7]. Hence, lake ice monitoring is important to support climate science and cryosphere research, and ultimately to support climate change mitigation [8].…”
Section: Introductionmentioning
confidence: 99%