Sea Ice Dynamic and Thermodynamic Processes Involved in the Genesis of Three Sea Ice Minima As Revealed by A 10-year Arctic Ocean-Sea Ice Synthesis

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Hauptverfasser: Lyu, Guokun, Koehl, Armin, Serra, Nuno, Zhou, Meng, Stammer, Detlef
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2026
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author Lyu, Guokun
Koehl, Armin
Serra, Nuno
Zhou, Meng
Stammer, Detlef
author_facet Lyu, Guokun
Koehl, Armin
Serra, Nuno
Zhou, Meng
Stammer, Detlef
collection Datos científicos de ciencias marinas y ambientales
contents Contributions of sea ice dynamic and thermodynamic processes to the late-summer sea ice volume (SIV) changes in 2007, 2012, and 2016 are investigated using a new dynamically-consistent ocean-sea ice synthesis product. The synthesis and satellite observations indicate that summer sea ice in the Pacific sector is sensitive to atmospheric and oceanic forcing and is reducing significantly since 2007. For 2012, reduced ice thickness in April preconditions the late-summer ice loss. Ice-ocean heat exchange and ice advection support further ice loss, resulting in unprecedented ice loss. Sea ice advected to the Eurasian Basin and the central Arctic survives until late summer in 2007 and 2016, increasing local SIV. Enhanced basal melting is visible in regions with strong contributions from dynamic processes.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_939179
institution PANGAEA
language en
publishDate 2026
publisher PANGAEA
record_format pangaea
spellingShingle Sea Ice Dynamic and Thermodynamic Processes Involved in the Genesis of Three Sea Ice Minima As Revealed by A 10-year Arctic Ocean-Sea Ice Synthesis
Lyu, Guokun
Koehl, Armin
Serra, Nuno
Zhou, Meng
Stammer, Detlef
Binary Object; Binary Object (File Size); Binary Object (MD5 Hash); Binary Object (Media Type); File content
Contributions of sea ice dynamic and thermodynamic processes to the late-summer sea ice volume (SIV) changes in 2007, 2012, and 2016 are investigated using a new dynamically-consistent ocean-sea ice synthesis product. The synthesis and satellite observations indicate that summer sea ice in the Pacific sector is sensitive to atmospheric and oceanic forcing and is reducing significantly since 2007. For 2012, reduced ice thickness in April preconditions the late-summer ice loss. Ice-ocean heat exchange and ice advection support further ice loss, resulting in unprecedented ice loss. Sea ice advected to the Eurasian Basin and the central Arctic survives until late summer in 2007 and 2016, increasing local SIV. Enhanced basal melting is visible in regions with strong contributions from dynamic processes.
title Sea Ice Dynamic and Thermodynamic Processes Involved in the Genesis of Three Sea Ice Minima As Revealed by A 10-year Arctic Ocean-Sea Ice Synthesis
topic Binary Object; Binary Object (File Size); Binary Object (MD5 Hash); Binary Object (Media Type); File content
url https://doi.org/10.1594/PANGAEA.939179