Summer sea ice floe perimeter density in the Arctic: high-resolution optical satellite imagery and model evaluation
Abstract < 10 –30 m) but a much smaller proportion for large floes (radius > 30 –50 m). Observations and the WIPoFSD model both show a negative correlation between sea ice concentration and the floe perimeter density, but the two prognostic models (CPOM-FSD and FSDv2-WAVE) show the opposite pattern. These differences between models and the observations may be attributed to limitations in the observations (e.g. the image resolution is not sufficient to detect small floes) or limitations in the model parameterisations, including the use of a global power-law exponent in the WIPoFSD model as well as too weak a floe welding and enhanced wave fracture in the prognostic models.
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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Summer sea ice floe perimeter density in the Arctic: high-resolution optical satellite imagery and model evaluation ; volume:17 ; number:8 ; year:2023 ; pages:3575-3591 ; extent:17
The Cryosphere ; 17, Heft 8 (2023), 3575-3591 (gesamt 17)
- Creator
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Wang, Yanan
Hwang, Byongjun
Bateson, Adam William
Aksenov, Yevgeny
Horvat, Christopher
- DOI
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10.5194/tc-17-3575-2023
- URN
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urn:nbn:de:101:1-2023083104305392579402
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
- 14.08.2025, 10:58 AM CEST
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Associated
- Wang, Yanan
- Hwang, Byongjun
- Bateson, Adam William
- Aksenov, Yevgeny
- Horvat, Christopher
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