Sea-ice thermodynamics can determine waterbelt scenarios for Snowball Earth

<p>Snowball Earth refers to multiple periods in the Neoproterozoic during which geological evidence indicates that the Earth was largely covered in ice. A Snowball Earth results from a runaway ice–albedo feedback, but there is an ongoing debate about how the feedback stopped: with fully ice-co...

詳細記述

書誌詳細
主要な著者: J. Hörner, A. Voigt
フォーマット: 論文
言語:English
出版事項: Copernicus Publications 2024-03-01
シリーズ:Earth System Dynamics
オンライン・アクセス:https://esd.copernicus.org/articles/15/215/2024/esd-15-215-2024.pdf

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