File:Images of proglacial icings of land-terminating glaciers.webp

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Captions

Captions

From the study "Groundwater springs formed during glacial retreat are a large source of methane in the high Arctic"

Summary edit

Description
English: "a, Drone image of a winter icing formed at the glacier margin and extending within the proglacial river floodplain. b, Ice blister formed within an icing due to pressurized groundwater flow during winter. c, Aerial image of glacier (right) and icing remnants (left) in mid-summer. d, Icing field in early summer. e, Icing surface in summer with person for scale; ice layers formed by subsequent winter groundwater outflows are visible."
Date
Source https://www.nature.com/articles/s41561-023-01210-6
Author Authors of the study: Gabrielle E. Kleber, Andrew J. Hodson, Leonard Magerl, Erik Schytt Mannerfelt, Harold J. Bradbury, Yizhu Zhu, Mark Trimmer & Alexandra V. Turchyn; Photograph in c, Norwegian Polar Institute.

Licensing edit

w:en:Creative Commons
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current16:26, 7 September 2023Thumbnail for version as of 16:26, 7 September 20231,826 × 1,114 (440 KB)Prototyperspective (talk | contribs)Uploaded a work by Authors of the study: Gabrielle E. Kleber, Andrew J. Hodson, Leonard Magerl, Erik Schytt Mannerfelt, Harold J. Bradbury, Yizhu Zhu, Mark Trimmer & Alexandra V. Turchyn from https://www.nature.com/articles/s41561-023-01210-6 with UploadWizard

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