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• W2107058407 abstract "This paper reviews our understanding of how the effects of the El Niño–southern oscillation (ENSO) might be transmitted from the tropical Pacific Ocean to the Antarctic, and examines the evidence for such signals in the Antarctic meteorological, sea ice, ice core and biological records. Many scientific disciples concerned with the Antarctic require an understanding of how the climatic conditions in the tropical and mid-latitude regions affect the Antarctic, and it is hoped that this review will aid their work. The most pronounced signals of ENSO are found over the southeast Pacific as a result of a climatological Rossby wave train that gives positive (negative) height anomalies over the Amundsen–Bellingshausen Sea during El Niño (La Niña) events. However, the extra-tropical signature can sometimes show a high degree of variability between events in this area. In West Antarctica, links between ENSO and precipitation have shown variability on the decadal time scale. Across the continent itself, it is even more difficult to relate meteorological conditions to ENSO, yet analyses of the long meteorological records from the stations do indicate a distinct switch in sign of the pressure anomalies from positive to negative across the minimum in the southern oscillation index. The oceanic signals of ENSO around the Antarctic are less clear, but it has been suggested that the Antarctic circumpolar wave could be forced by the phenomenon. Ice-core data offer the potential to help in understanding the long-term relationship between ENSO and the climate of the Antarctic, but there are difficulties because of the need to smooth the ice-core data to overcome the mixing of snow on the surface. Nevertheless, analysis of methylsulphonic acid in a South Pole core has shown high variability on ENSO time scales. It is clear that some evidence of ENSO can be found in the Antarctic meteorological and ice-core records; however, many of the relationships tend not to be stable with time, and we currently have a poor understanding of the transfer functions by which such signals arrive at the Antarctic from the tropical Pacific. Copyright © 2004 Royal Meteorological Society" @default.
• W2107058407 created "2016-06-24" @default.
• W2107058407 creator A5073681203 @default.
• W2107058407 date "2004-01-01" @default.
• W2107058407 modified "2023-10-11" @default.
• W2107058407 title "The El Niño-southern oscillation and Antarctica" @default.
• W2107058407 cites W120405837 @default.
• W2107058407 cites W1562140210 @default.
• W2107058407 cites W1574392831 @default.
• W2107058407 cites W1627908127 @default.
• W2107058407 cites W1643376493 @default.
• W2107058407 cites W1664260848 @default.
• W2107058407 cites W1965590263 @default.
• W2107058407 cites W1969521349 @default.
• W2107058407 cites W1969942502 @default.
• W2107058407 cites W1971418850 @default.
• W2107058407 cites W1975024484 @default.
• W2107058407 cites W1975411398 @default.
• W2107058407 cites W1978562309 @default.
• W2107058407 cites W1978835100 @default.
• W2107058407 cites W1981649995 @default.
• W2107058407 cites W1986584375 @default.
• W2107058407 cites W1991292890 @default.
• W2107058407 cites W1993196883 @default.
• W2107058407 cites W2000046380 @default.
• W2107058407 cites W2001605360 @default.
• W2107058407 cites W2002990310 @default.
• W2107058407 cites W2003160793 @default.
• W2107058407 cites W2003591120 @default.
• W2107058407 cites W2005019103 @default.
• W2107058407 cites W2005810633 @default.
• W2107058407 cites W2011679229 @default.
• W2107058407 cites W2014943459 @default.
• W2107058407 cites W2019537773 @default.
• W2107058407 cites W2020365420 @default.
• W2107058407 cites W2028014989 @default.
• W2107058407 cites W2028644122 @default.
• W2107058407 cites W2029320315 @default.
• W2107058407 cites W2033030060 @default.
• W2107058407 cites W2033634936 @default.
• W2107058407 cites W2034231630 @default.
• W2107058407 cites W2040622122 @default.
• W2107058407 cites W2044490660 @default.
• W2107058407 cites W2047604301 @default.
• W2107058407 cites W2047885660 @default.
• W2107058407 cites W2051387452 @default.
• W2107058407 cites W2054069860 @default.
• W2107058407 cites W2058174641 @default.
• W2107058407 cites W2062776038 @default.
• W2107058407 cites W2066076926 @default.
• W2107058407 cites W2068153367 @default.
• W2107058407 cites W2070766630 @default.
• W2107058407 cites W2074741151 @default.
• W2107058407 cites W2074743113 @default.
• W2107058407 cites W2079376684 @default.
• W2107058407 cites W2081369555 @default.
• W2107058407 cites W2083418404 @default.
• W2107058407 cites W2083591834 @default.
• W2107058407 cites W2092497323 @default.
• W2107058407 cites W2094496866 @default.
• W2107058407 cites W2095098813 @default.
• W2107058407 cites W2095450532 @default.
• W2107058407 cites W2099830627 @default.
• W2107058407 cites W2104203249 @default.
• W2107058407 cites W2107287559 @default.
• W2107058407 cites W2107760445 @default.
• W2107058407 cites W2112177158 @default.
• W2107058407 cites W2115201009 @default.
• W2107058407 cites W2120115499 @default.
• W2107058407 cites W2128360837 @default.
• W2107058407 cites W2132617504 @default.
• W2107058407 cites W2136830623 @default.
• W2107058407 cites W2146681603 @default.
• W2107058407 cites W2158924093 @default.
• W2107058407 cites W2159447010 @default.
• W2107058407 cites W2162074073 @default.
• W2107058407 cites W2167221624 @default.
• W2107058407 cites W2172581250 @default.
• W2107058407 cites W2172958845 @default.
• W2107058407 cites W2173251738 @default.
• W2107058407 cites W2174367230 @default.
• W2107058407 cites W2175236913 @default.
• W2107058407 cites W2175519760 @default.
• W2107058407 cites W2176548234 @default.
• W2107058407 cites W2177677497 @default.
• W2107058407 cites W2177686615 @default.
• W2107058407 cites W2178186723 @default.
• W2107058407 cites W2180542249 @default.
• W2107058407 cites W2180666476 @default.
• W2107058407 cites W2616366954 @default.
• W2107058407 cites W297841283 @default.
• W2107058407 cites W3213567142 @default.
• W2107058407 doi "https://doi.org/10.1002/joc.965" @default.
• W2107058407 hasPublicationYear "2004" @default.
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