{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,3,18]],"date-time":"2026-03-18T10:38:20Z","timestamp":1773830300834,"version":"3.50.1"},"reference-count":15,"publisher":"American Geophysical Union (AGU)","issue":"21","license":[{"start":{"date-parts":[[2012,12,7]],"date-time":"2012-12-07T00:00:00Z","timestamp":1354838400000},"content-version":"vor","delay-in-days":4054,"URL":"http:\/\/onlinelibrary.wiley.com\/termsAndConditions#vor"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Geophysical Research Letters"],"published-print":{"date-parts":[[2001,11]]},"abstract":"<jats:p>Annular modes are patterns characterized by synchronous fluctuations in surface pressure of one sign over the polar caps and the opposite sign at lower latitudes. The Southern Annular Mode (SAM) and Northern Annular Mode (NAM, also called the Arctic Oscillation) patterns are the leading empirical orthogonal functions (EOFs) of slowly\u2010varying, hemispheric, cold\u2010season, sea\u2010level pressure anomalies (deviations from climatology). Daily indices of the SAM and NAM are a measure of the similarity between surface pressure anomaly patterns and the annular modes. Here it is shown that the first two EOF time series of daily, global, year\u2010round, zonally\u2010averaged surface pressure are nearly identical to the SAM and NAM indices. Together they account for more than 57% of the daily variance of zonally\u2010averaged surface pressure. The SAM and NAM patterns extend through the tropics, well into the opposite hemispheres. Fluctuations of the SAM and NAM indices are accompanied by interhemispheric transfer of mass.<\/jats:p>","DOI":"10.1029\/2001gl013564","type":"journal-article","created":{"date-parts":[[2004,2,5]],"date-time":"2004-02-05T00:11:20Z","timestamp":1075939880000},"page":"4115-4118","source":"Crossref","is-referenced-by-count":106,"title":["Annular modes in global daily surface pressure"],"prefix":"10.1029","volume":"28","author":[{"given":"Mark P.","family":"Baldwin","sequence":"first","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"13","published-online":{"date-parts":[[2012,12,7]]},"reference":[{"key":"e_1_2_1_2_1","doi-asserted-by":"publisher","DOI":"10.1007\/s005850050894"},{"key":"e_1_2_1_3_1","doi-asserted-by":"publisher","DOI":"10.1126\/science.1063315"},{"key":"e_1_2_1_4_1","doi-asserted-by":"publisher","DOI":"10.1175\/1520-0442(1989)002<0137:LSROAM>2.0.CO;2"},{"key":"e_1_2_1_5_1","doi-asserted-by":"publisher","DOI":"10.1029\/1999GL900003"},{"key":"e_1_2_1_6_1","doi-asserted-by":"publisher","DOI":"10.1029\/2000GL011563"},{"key":"e_1_2_1_7_1","doi-asserted-by":"publisher","DOI":"10.1175\/1520-0477(1996)077<0437:TNYRP>2.0.CO;2"},{"key":"e_1_2_1_8_1","doi-asserted-by":"publisher","DOI":"10.1175\/1520-0493(1970)098<0708:LSFOMM>2.3.CO;2"},{"key":"e_1_2_1_9_1","doi-asserted-by":"publisher","DOI":"10.1029\/1999GL010478"},{"key":"e_1_2_1_10_1","doi-asserted-by":"publisher","DOI":"10.1175\/1520-0493(1982)110<1375:SVOSLP>2.0.CO;2"},{"key":"e_1_2_1_11_1","doi-asserted-by":"publisher","DOI":"10.1029\/98GL00950"},{"key":"e_1_2_1_12_1","doi-asserted-by":"publisher","DOI":"10.1175\/1520-0442(2000)013<1000:AMITEC>2.0.CO;2"},{"key":"e_1_2_1_13_1","doi-asserted-by":"publisher","DOI":"10.1029\/94JD02043"},{"key":"e_1_2_1_14_1","doi-asserted-by":"publisher","DOI":"10.1175\/1520-0442(2000)013<0681:AMOTAA>2.0.CO;2"},{"key":"e_1_2_1_15_1","first-page":"791","article-title":"North Atlantic Oscillation\/Annular mode: two paradigms\u2014one phenomenon","volume":"126","author":"Wallace J. M.","year":"2000","journal-title":"Quart. J. Roy. Meteorol. Soc."},{"key":"e_1_2_1_16_1","doi-asserted-by":"publisher","DOI":"10.1175\/1520-0469(1979)036<1409:PCTTQG>2.0.CO;2"}],"container-title":["Geophysical Research Letters"],"original-title":[],"language":"en","link":[{"URL":"https:\/\/api.wiley.com\/onlinelibrary\/tdm\/v1\/articles\/10.1029%2F2001GL013564","content-type":"unspecified","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/agupubs.onlinelibrary.wiley.com\/doi\/pdf\/10.1029\/2001GL013564","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2023,11,21]],"date-time":"2023-11-21T23:38:56Z","timestamp":1700609936000},"score":1,"resource":{"primary":{"URL":"https:\/\/agupubs.onlinelibrary.wiley.com\/doi\/10.1029\/2001GL013564"}},"subtitle":[],"short-title":[],"issued":{"date-parts":[[2001,11]]},"references-count":15,"journal-issue":{"issue":"21","published-print":{"date-parts":[[2001,11]]}},"alternative-id":["10.1029\/2001GL013564"],"URL":"https:\/\/doi.org\/10.1029\/2001gl013564","archive":["Portico"],"relation":{},"ISSN":["0094-8276","1944-8007"],"issn-type":[{"value":"0094-8276","type":"print"},{"value":"1944-8007","type":"electronic"}],"subject":[],"published":{"date-parts":[[2001,11]]}}}