Talk:Brewer–Dobson circulation

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Latest comment: 3 years ago1 comment1 person in discussion

Notes Concerning Article Evaluation: While everything in the article is relevant to the topic, there is only one paragraph, one visual, and only two citations in this entry. The article is missing information about the current status of the Brewer-Dobson circulation theory and is missing support from evidence. The information is also out of date, using citations from 1990 and 2001 when more current research exists on the subject of Brewer-Dobson circulation. However, the article does not use any other Wikipedia pages as reference, and all of the information is clear and accurate, just simply outdated. The information needs to be elaborated on to include examples of Brewer-Dobson circulation (such as in the tropics and extratropical latitudes), evidence as to why the theory of Brewer-Dobson circulation even exists (hemispheric differences in water transport and planetary wave activity, radiative balance, sinking air and meridionial overturning, etc.), changes in Brewer-Dobson circulation in the last four decades (using most recent research), and recent challenges in understanding the circulation theory and its response to climate change. Supporting citations based on research from 2014 and 2019 and supporting visuals can be added to enhance readers' understating of the information. The sources used currently are very credible and are peer-reviewed and scholarly, but they are outdated. Kaddington6 (talk) 03:31, 6 March 2021 (UTC)Reply

Wiki Education Foundation-supported course assignment

Latest comment: 2 years ago1 comment1 person in discussion

This article was the subject of a Wiki Education Foundation-supported course assignment, between 14 January 2021 and 5 May 2021. Further details are available on the course page. Student editor(s): Kaddington6. Peer reviewers: KyleeGraham20.

Above undated message substituted from Template:Dashboard.wikiedu.org assignment by PrimeBOT (talk) 11:35, 18 January 2022 (UTC)Reply

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