{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,4,29]],"date-time":"2026-04-29T07:55:06Z","timestamp":1777449306936,"version":"3.51.4"},"reference-count":35,"publisher":"SAGE Publications","issue":"2","license":[{"start":{"date-parts":[[2016,1,1]],"date-time":"2016-01-01T00:00:00Z","timestamp":1451606400000},"content-version":"tdm","delay-in-days":0,"URL":"https:\/\/journals.sagepub.com\/page\/policies\/text-and-data-mining-license"}],"content-domain":{"domain":["journals.sagepub.com"],"crossmark-restriction":true},"short-container-title":["Asymptotic Analysis"],"published-print":{"date-parts":[[2016,1,7]]},"abstract":"<jats:p>We consider the three-dimensional primitive equations of the atmosphere with humidity and saturation associated with suitable boundary conditions. These equations have been shown to lead to well-posed problem producing a continuous semigroup despite the discontinuities due to the change of phase between vapor water and liquid water. In this article, we aim to show the existence of a global attractor for a model problem.<\/jats:p>","DOI":"10.3233\/asy-151332","type":"journal-article","created":{"date-parts":[[2016,1,8]],"date-time":"2016-01-08T10:08:16Z","timestamp":1452247696000},"page":"91-107","update-policy":"https:\/\/doi.org\/10.1177\/sage-journals-update-policy","source":"Crossref","is-referenced-by-count":0,"title":["Global attractor of atmospheric equations"],"prefix":"10.1177","volume":"96","author":[{"given":"Youngjoon","family":"Hong","sequence":"first","affiliation":[{"name":"Department of Mathematics, Statistics, and Computer Science, University of Illinois, Chicago, IL, USA. 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