{"title":"夏威夷莫纳罗亚的大气二氧化碳变化","authors":"R.P. Kane, E.R. de Paula","doi":"10.1016/0021-9169(95)00193-X","DOIUrl":null,"url":null,"abstract":"<div><p>The 12-month running mean series of atmospheric CO<sub>2</sub> directly measured at Mauna Loa, Hawaii, showed highly significant periodicities near <em>T</em> = 14, 8, 5, 3–4 years. This CO<sub>2</sub> series also showed a significant oscillation at <em>T</em> = 2.56 years which matches with <em>T</em> = 2.6 years of the Southern Oscillation (SO) index but not with the QBO (<em>T</em> = 2.33 and 2.68 years) of the stratospheric zonal wind. On the other hand, the yearly range (maximum minus minimum) series of CO<sub>2</sub> showed periodicities <em>T</em> = 2.45 and 2.75 years (significant at the 2 sigma level) which seem similar to those of the stratospheric wind QBO (<em>T</em> = 2.33 and 2.68 years). No evidence was found for a 11 year (solar cycle) component.</p></div>","PeriodicalId":100754,"journal":{"name":"Journal of Atmospheric and Terrestrial Physics","volume":"58 15","pages":"Pages 1673-1681"},"PeriodicalIF":0.0000,"publicationDate":"1996-11-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0021-9169(95)00193-X","citationCount":"18","resultStr":"{\"title\":\"Atmospheric CO2 changes at Mauna Loa, Hawaii\",\"authors\":\"R.P. Kane, E.R. de Paula\",\"doi\":\"10.1016/0021-9169(95)00193-X\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>The 12-month running mean series of atmospheric CO<sub>2</sub> directly measured at Mauna Loa, Hawaii, showed highly significant periodicities near <em>T</em> = 14, 8, 5, 3–4 years. This CO<sub>2</sub> series also showed a significant oscillation at <em>T</em> = 2.56 years which matches with <em>T</em> = 2.6 years of the Southern Oscillation (SO) index but not with the QBO (<em>T</em> = 2.33 and 2.68 years) of the stratospheric zonal wind. On the other hand, the yearly range (maximum minus minimum) series of CO<sub>2</sub> showed periodicities <em>T</em> = 2.45 and 2.75 years (significant at the 2 sigma level) which seem similar to those of the stratospheric wind QBO (<em>T</em> = 2.33 and 2.68 years). No evidence was found for a 11 year (solar cycle) component.</p></div>\",\"PeriodicalId\":100754,\"journal\":{\"name\":\"Journal of Atmospheric and Terrestrial Physics\",\"volume\":\"58 15\",\"pages\":\"Pages 1673-1681\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"1996-11-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1016/0021-9169(95)00193-X\",\"citationCount\":\"18\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Atmospheric and Terrestrial Physics\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/002191699500193X\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Atmospheric and Terrestrial Physics","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/002191699500193X","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
The 12-month running mean series of atmospheric CO2 directly measured at Mauna Loa, Hawaii, showed highly significant periodicities near T = 14, 8, 5, 3–4 years. This CO2 series also showed a significant oscillation at T = 2.56 years which matches with T = 2.6 years of the Southern Oscillation (SO) index but not with the QBO (T = 2.33 and 2.68 years) of the stratospheric zonal wind. On the other hand, the yearly range (maximum minus minimum) series of CO2 showed periodicities T = 2.45 and 2.75 years (significant at the 2 sigma level) which seem similar to those of the stratospheric wind QBO (T = 2.33 and 2.68 years). No evidence was found for a 11 year (solar cycle) component.
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