File:Glacier-ice shelf interactions.svg

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Summary

Description Glacier-ice shelf interactions: In a stable glacier-ice shelf system, the glacier's downhill movement is offset by the buoyant force of the water on the front of the shelf. Warmer temperatures destabilize this system by lubricating the glacier's base and creating melt ponds that eventually carve through the shelf. Once the ice shelf retreats to the grounding line, the buoyant force that used to offset glacier flow becomes negligible, and the glacier picks up speed on its way to the sea.
Date
Source http://nsidc.org/sotc/iceshelves.html
Author Original Image by Ted Scambos and Michon Scott, National Snow and Ice Data Center. Redrawn by Sagredo⊙☿♀♁♂♃♄

Licensing

Public domain
This work is in the public domain in the United States because it is a work prepared by an officer or employee of the United States Government as part of that person’s official duties under the terms of Title 17, Chapter 1, Section 105 of the US Code. Note: This only applies to original works of the Federal Government and not to the work of any individual U.S. state, territory, commonwealth, county, municipality, or any other subdivision. This template also does not apply to postage stamp designs published by the United States Postal Service since 1978. (See § 313.6(C)(1) of Compendium of U.S. Copyright Office Practices). It also does not apply to certain US coins; see The US Mint Terms of Use.

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23 May 2008

File history

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Date/TimeThumbnailDimensionsUserComment
current17:36, 27 May 2014Thumbnail for version as of 17:36, 27 May 2014800 × 489 (572 KB)Szczureqconverted '''everything''' to paths to prevent blackboxing
17:31, 27 May 2014Thumbnail for version as of 17:31, 27 May 2014800 × 489 (344 KB)Szczureqremoved black boxes... finally?
11:57, 5 November 2012Thumbnail for version as of 11:57, 5 November 2012800 × 489 (346 KB)SzczureqInkscape lied - reverted to version as of 00:11, 21 May 2012
11:53, 5 November 2012Thumbnail for version as of 11:53, 5 November 2012800 × 489 (86 KB)Szczureqremoved even more invisible objects (incl. black box-generating); paths converted to text
00:11, 21 May 2012Thumbnail for version as of 00:11, 21 May 2012800 × 489 (346 KB)Sagredoremoved invisible objects
23:53, 20 May 2012Thumbnail for version as of 23:53, 20 May 2012800 × 489 (469 KB)Sagredouse stroke to path to try to remove black boxes in wikipedia renderings
23:52, 20 May 2012No thumbnail800 × 489 (469 KB)Sagredouse stroke to path to try to remove black boxes in wikipedia renderings
19:35, 23 May 2008Thumbnail for version as of 19:35, 23 May 20081,200 × 734 (455 KB)Sagredo{{Information |Description=Glacier-ice shelf interactions: In a stable glacier-ice shelf system, the glacier's downhill movement is offset by the buoyant force of the water on the front of the shelf. Warmer temperatures destabilize this system by lubricat
19:23, 23 May 2008Thumbnail for version as of 19:23, 23 May 20081,200 × 734 (118 KB)Sagredo{{Information |Description=Glacier-ice shelf interactions: In a stable glacier-ice shelf system, the glacier's downhill movement is offset by the buoyant force of the water on the front of the shelf. Warmer temperatures destabilize this system by lubricat
19:21, 23 May 2008Thumbnail for version as of 19:21, 23 May 20081,200 × 734 (118 KB)Sagredo{{Information |Description=Glacier-ice shelf interactions: In a stable glacier-ice shelf system, the glacier's downhill movement is offset by the buoyant force of the water on the front of the shelf. Warmer temperatures destabilize this system by lubricat
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