Former featured articleRetreat of glaciers since 1850 is a former featured article. Please see the links under Article milestones below for its original nomination page (for older articles, check the nomination archive) and why it was removed.
Main Page trophyThis article appeared on Wikipedia's Main Page as Today's featured article on April 18, 2006.
Article milestones
DateProcessResult
February 10, 2006Peer reviewReviewed
March 7, 2006Featured article candidateNot promoted
April 3, 2006Featured article candidatePromoted
January 8, 2022Featured article reviewDemoted
Current status: Former featured article


Some suggestions about restructuring (revisited) edit

I am repeating some suggestions which I had made a year ago but which were mostly dismissed as it was in the middle of the featured article review. Now that the article has been reviewed and demoted, I'd like to raise my points again. This is what I had written earlier: "I see that was I had suggested as "fundamentals" has now been added before the regional information, and I have just reworked it a bit now. My original suggestion was: "I think we are missing some more information about "fundamentals" at the start of the article, before it dives into all the different regions. I.e. things that are common throughout the world. I am missing a section on "causes" (Ok, might just be one sentence: it's getting warmer), but also one on "measurement techniques" perhaps? I have moved the section on "effects" up towards the start for that reason, too. Also the third paragraph in the lead contains information that is not really well covered in the main body; that's not ideal as the lead is meant to be a summary of the article. So I think we should have a section about the broad historical outline (after 1850), and then summarise that briefly in the lead. The lead should be made into a better summary, although it won't be easy to summarise all that content from the different regions. Note the article is also very long (60 kB of prose). Is it going into too much details in some areas where sub-articles exist?" - The current structure is now like this which is better (i.e. we no longer need a section called "fundamentals" now):

1 Causes
2 Measurements
2.1 Estimated glacial losses ---> does this fit under "measurements" or should it be elsewhere?
3 Effects
3.1 Water supply
3.2 Ecosystems
3.3 Floods
3.4 Sea level rise
3.5 Management approaches --> does this fit here? It's very short which is why I didn't think that it should be a Level-1 heading. 

EMsmile (talk) 11:16, 8 June 2022 (UTC)Reply

I've made some changes to the structure now in order to address the concerns I had raised here a year ago. I think it's better now. EMsmile (talk) 07:52, 26 July 2023 (UTC)Reply
The new structure is now like this:
Scale at the global level
Causes
Impacts
Middle latitude
Polar regions
Tropics
Management approaches

EMsmile (talk) 07:53, 26 July 2023 (UTC)Reply

Is the statement in the lead about the 5500 gigatons correct? edit

I came back to this article while working on water cycle which I am currently updating for climate change effects. I wanted to include something about glaciers and saw the sentence in the lead Excluding peripheral glaciers of ice sheets, total global glacial losses were likely 5500 gigatons over 1993–2018. However, I can't find this figure in the source provided (AR 6). Is it wrong? I found this statement in chapter 9 of the WG I report: Excluding peripheral glaciers of ice sheets (RGI regions 5 and 19), glacier mass loss rate was very likely 170 ± 80 Gt yr –1 for the period 1971 to 2019 (8 [4 to 14] % of 1971 glacier mass), 210 ± 50 Gt yr –1 over the period 1993–2019 (6 [4 to 8] % of 1993 glacier mass) and 240 ± 40 Gt yr–1 over the period 2006–2019 (3 [2 to 4] % of 2006 glacier mass.. Maybe it's anyway better for this statement in the lead to not provide actual numbers (nobody has a feel for Gt anyhow) but to just say this In summary, new evidence published since SROCC shows that, during the decade 2010–2019, glaciers lost more mass than in any other decade since the beginning of the observational record (same report, 9. 1275) EMsmile (talk) 09:46, 29 September 2022 (UTC)Reply

Ah, I got the answer now: I checked with Thian Y Gan (one of the IPCC authors) and he explained it to me: "I believe that is about right based on the estimate of 210 ± 50 Gt yr –1 over the period 1993–2019, 210 x 26 = 5460 Gt? That statement is found in page 65 of Chapter 9 of ARG-WGI- " So the 5500 gigaton figure is the accumulated amount over 26 years whereas the other figures are averages for a "per year" (hence it's called rate). I think I'll provide both figures here in the article for greater clarity. EMsmile (talk) 19:14, 29 September 2022 (UTC)Reply

Add more references to the lead? edit

My suggestion is that more refs should be added to the lead. This would be particularly useful if the lead is transcribed to another article with the excerpt too. Does anyone object? If not, which are the main refs we should use, I am assuming Chapter 9 of the AR 6 WG 2 report? EMsmile (talk) 09:20, 28 April 2023 (UTC)Reply

Some condensing needed edit

The article is a bit on the long side (60 kB (9918 words)). Looking at the section sizes (see top of the talk page), it seems that the sections about Europe, Himalayas and Antarctica are a bit too long. Probably some of that content could be moved to sub-articles (which perhaps didn't exist yet when this article was first created). Most of this article's content was added in 2006 and in 2015. So updating of figures and references is also needed. EMsmile (talk) 08:17, 26 July 2023 (UTC)Reply

Wiki Education assignment: Current Topics in Earth and Environmental Sciences edit

  This article was the subject of a Wiki Education Foundation-supported course assignment, between 20 August 2023 and 9 December 2023. Further details are available on the course page. Student editor(s): Dylan5723 (article contribs).

— Assignment last updated by Dylan5723 (talk) 20:30, 10 October 2023 (UTC)Reply