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* January 2012 in-print issue, page 34 & 35 ''Antarctic Undercut'' by Douglas Fox. [[Special:Contributions/97.87.29.188|97.87.29.188]] ([[User talk:97.87.29.188|talk]]) 01:32, 6 January 2012 (UTC)
* January 2012 in-print issue, page 34 & 35 ''Antarctic Undercut'' by Douglas Fox. [[Special:Contributions/97.87.29.188|97.87.29.188]] ([[User talk:97.87.29.188|talk]]) 01:32, 6 January 2012 (UTC)

== Further Reading addition from [[Skeptic (U.S. magazine)]]? ==

*Cover Story [http://www.skeptic.com/eskeptic/12-02-08/#feature ''How We Know Global Warming is Real and Human Caused''] in current Volume 17 Number 2 [[Skeptic (U.S. magazine)]]. Cover photo: A massive crack across Antarctica’s Pine Island Glacier will produce a giant iceberg of about 350 sq. miles (900 square k). Credit: NASA/ GSFC/METI/ERSDAC/JAROS, and U.S./Japan ASTER Science Team. [[Special:Contributions/99.181.140.167|99.181.140.167]] ([[User talk:99.181.140.167|talk]]) 09:02, 29 June 2012 (UTC) <span style="font-size: smaller;" class="autosigned">— Preceding [[Wikipedia:Signatures|unsigned]] comment added by [[Special:Contributions/99.181.141.90|99.181.141.90]] ([[User talk:99.181.141.90|talk]]) </span><!-- Template:Unsigned IP --> <!--Autosigned by SineBot-->
::Article link included above, with [http://www.nasa.gov/multimedia/imagegallery/image_feature_2165.html photo] [[Special:Contributions/99.181.136.208|99.181.136.208]] ([[User talk:99.181.136.208|talk]]) 07:47, 1 July 2012 (UTC) <span style="font-size: smaller;" class="autosigned">— Preceding [[Wikipedia:Signatures|unsigned]] comment added by [[Special:Contributions/99.181.143.181|99.181.143.181]] ([[User talk:99.181.143.181|talk]]) </span><!-- Template:Unsigned IP --> <!--Autosigned by SineBot--> <span style="font-size: smaller;" class="autosigned">— Preceding [[Wikipedia:Signatures|unsigned]] comment added by [[Special:Contributions/99.181.140.176|99.181.140.176]] ([[User talk:99.181.140.176|talk]]) </span><!-- Template:Unsigned IP --> <!--Autosigned by SineBot-->

Revision as of 06:55, 6 July 2012

Good articlePine Island Glacier has been listed as one of the Geography and places good articles under the good article criteria. If you can improve it further, please do so. If it no longer meets these criteria, you can reassess it.
Article milestones
DateProcessResult
June 9, 2009Good article nomineeListed
WikiProject iconGlaciers GA‑class High‑importance
WikiProject iconThis article is within the scope of WikiProject Glaciers, a collaborative effort to improve the coverage of Glaciers on Wikipedia. If you would like to participate, please visit the project page, where you can join the discussion and see a list of open tasks.
GAThis article has been rated as GA-class on Wikipedia's content assessment scale.
HighThis article has been rated as High-importance on the project's importance scale.
WikiProject iconAntarctica GA‑class High‑importance
WikiProject iconThis article is within the scope of WikiProject Antarctica, a collaborative effort to improve the coverage of Antarctica on Wikipedia. If you would like to participate, please visit the project page, where you can join the discussion and see a list of open tasks.
GAThis article has been rated as GA-class on Wikipedia's content assessment scale.
HighThis article has been rated as High-importance on the project's importance scale.

GA Review

This review is transcluded from Talk:Pine Island Glacier/GA1. The edit link for this section can be used to add comments to the review.

GA review – see WP:WIAGA for criteria

  1. Is it reasonably well written?
    A. Prose quality:
    B. MoS compliance:
  2. Is it factually accurate and verifiable?
    A. References to sources:
    B. Citation of reliable sources where necessary:
    C. No original research:
  3. Is it broad in its coverage?
    A. Major aspects:
    B. Focused:
  4. Is it neutral?
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  2. Is it stable?
    No edit wars, etc:
  3. Does it contain images to illustrate the topic?
    A. Images are copyright tagged, and non-free images have fair use rationales:
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  4. Overall:
    Pass or Fail:

There were some formatting errors, but I think the article is overall a very good article. ceranthor 22:38, 9 June 2009 (UTC)[reply]

Your last sentence in the acceleration section. It would seem that this question can be explored more by describing the acceleration observed. Polargeo I encourage you to do so. That is where is acceleration greatest, is it propogating. This will help indicate whether it is a calving front-ice shelf or upstream induced phenomenon. I did the bathymetry for the Polar Freeze journey for T.Kellogg and T.Hughes.

2010 Katz model

The paper just published in Proc royal soc does not really support any of the media hype. it is the testing of a fairly basic mathematical model on grounding line stability which just adds a peripheral Pine Island Glacier(ish) study. A quote from the paper if you are unconvinced "Given the complex, three-dimensional nature of the real Pine Island glacier, with its convergent feeder streams and subglacial hydrology, it should be clear that the above model is a very crude representation of reality" from the paper "Stability of ice-sheet grounding lines" Katz and Worster 2010. Polargeo (talk) 06:53, 17 January 2010 (UTC)[reply]

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  • January 2012 in-print issue, page 34 & 35 Antarctic Undercut by Douglas Fox. 97.87.29.188 (talk) 01:32, 6 January 2012 (UTC)[reply]

Further Reading addition from Skeptic (U.S. magazine)?

Article link included above, with photo 99.181.136.208 (talk) 07:47, 1 July 2012 (UTC) — Preceding unsigned comment added by 99.181.143.181 (talk) — Preceding unsigned comment added by 99.181.140.176 (talk) [reply]