{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,10,12]],"date-time":"2025-10-12T00:18:36Z","timestamp":1760228316098,"version":"build-2065373602"},"reference-count":63,"publisher":"MDPI AG","issue":"10","license":[{"start":{"date-parts":[[2022,5,10]],"date-time":"2022-05-10T00:00:00Z","timestamp":1652140800000},"content-version":"vor","delay-in-days":0,"URL":"https:\/\/creativecommons.org\/licenses\/by\/4.0\/"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Remote Sensing"],"abstract":"<jats:p>The purpose of this work is to study quasi-stationary wave structure in the mid-latitude stratosphere and mesosphere (40\u201350\u00b0N) and its role in the formation of the annual ozone cycle. Geopotential height and ozone from Aura MLS data are used and winter climatology for January\u2013February 2011\u20132020 is considered. The 10-degree longitude segment centered on Longfengshan Brewer station (44.73\u00b0N, 127.60\u00b0E), China, is examined in detail. The station is located in the region of the Aleutian Low associated with the quasi-stationary zonal maximum of total ozone. Annual and semi-annual oscillations in ozone using units of ozone volume mixing ratio and concentration, as well as changes in ozone peak altitude and in time series of ozone at individual pressure levels between 316 hPa (9 km) and 0.001 hPa (96 km) were compared. The ozone maximum in the vertical profile is higher in volume mixing ratio (VMR) values than in concentration by about 15 km (5 km) in the stratosphere (mesosphere), consistent with some previous studies. We found that the properties of the annual cycle are better resolved in the altitude range of the main ozone maximum: middle\u2013upper stratosphere in VMR and lower stratosphere in concentration. Both approaches reveal annual and semi-annual changes in the ozone peak altitudes in a range of 4\u20136 km during the year. In the lower-stratospheric ozone of the Longfengshan domain, an earlier development of the annual cycle takes place with a maximum in February and a minimum in August compared to spring and autumn, respectively, in zonal means. This is presumably due to the higher rate of dynamical ozone accumulation in the region of the quasi-stationary zonal ozone maximum. The \u201cno-annual-cycle\u201d transition layers are found in the stratosphere and mesosphere. These layers with undisturbed ozone volume mixing ratio are of interest for more detailed future study.<\/jats:p>","DOI":"10.3390\/rs14102309","type":"journal-article","created":{"date-parts":[[2022,5,10]],"date-time":"2022-05-10T21:52:11Z","timestamp":1652219531000},"page":"2309","update-policy":"https:\/\/doi.org\/10.3390\/mdpi_crossmark_policy","source":"Crossref","is-referenced-by-count":1,"title":["The Annual Cycle in Mid-Latitude Stratospheric and Mesospheric Ozone Associated with Quasi-Stationary Wave Structure by the MLS Data 2011\u20132020"],"prefix":"10.3390","volume":"14","author":[{"given":"Chenning","family":"Zhang","sequence":"first","affiliation":[{"name":"International Center of Future Science, College of Physics, Jilin University, Changchun 130012, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-0582-559X","authenticated-orcid":false,"given":"Oleksandr","family":"Evtushevsky","sequence":"additional","affiliation":[{"name":"Physics Faculty, Taras Shevchenko National University of Kyiv, 01601 Kyiv, Ukraine"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-2342-2615","authenticated-orcid":false,"given":"Gennadi","family":"Milinevsky","sequence":"additional","affiliation":[{"name":"International Center of Future Science, College of Physics, Jilin University, Changchun 130012, China"},{"name":"Physics Faculty, Taras Shevchenko National University of Kyiv, 01601 Kyiv, Ukraine"},{"name":"Department of Atmosphere Physics and Geospace, National Antarctic Scientific Center, 01601 Kyiv, Ukraine"},{"name":"Laboratoire d\u2019Optique Atmosph\u00e9rique, D\u00e9partement de Physique, Universit\u00e9 de Lille, 59655 Villeneuve d\u2019Ascq, France"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-3335-0034","authenticated-orcid":false,"given":"Andrew","family":"Klekociuk","sequence":"additional","affiliation":[{"name":"Antarctic Climate Program, Australian Antarctic Division, Kingston 7050, Australia"},{"name":"Department of Physics, University of Adelaide, Adelaide 5005, Australia"}]},{"given":"Yulia","family":"Andrienko","sequence":"additional","affiliation":[{"name":"Physics Faculty, Taras Shevchenko National University of Kyiv, 01601 Kyiv, Ukraine"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-6529-5610","authenticated-orcid":false,"given":"Valery","family":"Shulga","sequence":"additional","affiliation":[{"name":"International Center of Future Science, College of Physics, Jilin University, Changchun 130012, China"},{"name":"Department of Millimeter Radio Astronomy, Institute of Radio Astronomy, National Academy of Sciences of Ukraine, 61002 Kharkiv, Ukraine"}]},{"given":"Wei","family":"Han","sequence":"additional","affiliation":[{"name":"International Center of Future Science, College of Physics, Jilin University, Changchun 130012, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-6972-2122","authenticated-orcid":false,"given":"Yu","family":"Shi","sequence":"additional","affiliation":[{"name":"International Center of Future Science, College of Physics, Jilin University, Changchun 130012, China"}]}],"member":"1968","published-online":{"date-parts":[[2022,5,10]]},"reference":[{"key":"ref_1","doi-asserted-by":"crossref","first-page":"8873","DOI":"10.1029\/92JD02820","article-title":"Quasi-stationary planetary waves in total ozone and their correlation with lower stratospheric temperature","volume":"98","author":"Wirth","year":"1998","journal-title":"J. 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