Future Antarctic snow accumulation trend is dominated by atmospheric synoptic-scale events

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Location: Deutsche Nationalbibliothek Frankfurt am Main

ISSN: 2662-4435

Extent: Online-Ressource

Language: Englisch

Notes: online resource.

Bibliographic citation: Future Antarctic snow accumulation trend is dominated by atmospheric synoptic-scale events ; volume:1 ; number:1 ; day:11 ; month:12 ; year:2020 ; pages:1-9 ; date:12.2020
Communications earth & environment ; 1, Heft 1 (11.12.2020), 1-9, 12.2020

Creator: Dalaiden, Quentin
Goosse, Hugues
Lenaerts, Jan
Cavitte, Marie G. P.
Henderson, Naomi

Contributor: SpringerLink (Online service)

DOI: 10.1038/s43247-020-00062-x

URN: urn:nbn:de:101:1-2021011519024585473757

Rights: Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.

Last update: 15.08.2025, 7:34 AM CEST

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Dalaiden, Quentin
Goosse, Hugues
Lenaerts, Jan
Cavitte, Marie G. P.
Henderson, Naomi
SpringerLink (Online service)

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Future Antarctic snow accumulation trend is dominated by atmospheric synoptic-scale events

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Other Objects (12)

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Regional Antarctic snow accumulation over the past 1000 years

Review of regional Antarctic snow accumulation over the past 1000 years

Evaluating the Twentieth Century Reanalysis Version 3 with synoptic typing and East Antarctic ice core accumulation

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First evidence of microplastics in Antarctic snow

First evidence of microplastics in Antarctic snow

Topography significantly influencing low flows in snow-dominated watersheds

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Penetration of interferometric radar signals in Antarctic snow

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Regional Antarctic snow accumulation over the past 1000 years

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Evaluating the Twentieth Century Reanalysis Version 3 with synoptic typing and East Antarctic ice core accumulation

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First evidence of microplastics in Antarctic snow

First evidence of microplastics in Antarctic snow

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Penetration of interferometric radar signals in Antarctic snow

Snow melting bias in microwave mapping of Antarctic snow accumulation

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Topography significantly influencing low flows in snow-dominated watersheds

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Penetration of interferometric radar signals in Antarctic snow

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