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词条 Antarctic oscillation
释义

  1. See also

  2. References

  3. External links

The Antarctic oscillation (AAO, to distinguish it from the Arctic oscillation or AO) is a low-frequency mode of atmospheric variability of the southern hemisphere. It is also known as the Southern Annular Mode (SAM). It is defined as a belt of westerly winds or low pressure surrounding Antarctica which moves north or south as its mode of variability.[1] In its positive phase, the westerly wind belt that drives the Antarctic Circumpolar Current intensifies and contracts towards Antarctica[2], while its negative phase involves this belt moving towards the Equator. Winds associated with the Southern Annular Mode cause oceanic upwelling of warm circumpolar deep water along the Antarctic continental shelf,[3][4] which has been linked to ice shelf basal melt,[5] representing a possible wind-driven mechanism that could destabilize large portions of the Antarctic Ice Sheet.[6]

In 2014, Dr Nerilie Abram used a network of temperature-sensitive ice core and tree growth records to reconstruct a 1000-year history of the Southern Annular Mode. This work suggests that the Southern Annular Mode is currently in its most extreme positive phase over at least the last 1000 years, and that recent positive trends in the SAM are attributed to increasing greenhouse gas levels and later stratospheric ozone depletion.[7][8]

See also

  • North Atlantic oscillation
  • Arctic oscillation
  • Pacific decadal oscillation
  • Anticyclone
  • John Michael Wallace

References

1. ^Australian Bureau of Meteorology - The Southern Annular Mode. Accessed 25/10/2013. http://www.bom.gov.au/climate/enso/history/ln-2010-12/SAM-what.shtml
2. ^{{Cite journal|last=Thompson|first=David W. J.|last2=Solomon|first2=Susan|last3=Kushner|first3=Paul J.|last4=England|first4=Matthew H.|last5=Grise|first5=Kevin M.|last6=Karoly|first6=David J.|date=2011-10-23|title=Signatures of the Antarctic ozone hole in Southern Hemisphere surface climate change|url=http://www.nature.com/articles/ngeo1296|journal=Nature Geoscience|language=En|volume=4|issue=11|pages=741–749|doi=10.1038/ngeo1296|issn=1752-0894}}
3. ^{{Cite journal|last=Hayakawa|first=Hideaki|last2=Shibuya|first2=Kazuo|last3=Aoyama|first3=Yuichi|last4=Nogi|first4=Yoshifumi|last5=Doi|first5=Koichiro|date=2012|title=Ocean bottom pressure variability in the Antarctic Divergence Zone off Lützow-Holm Bay, East Antarctica|url=http://linkinghub.elsevier.com/retrieve/pii/S0967063711001713|journal=Deep Sea Research Part I: Oceanographic Research Papers|volume=60|pages=22–31|doi=10.1016/j.dsr.2011.09.005|issn=0967-0637|via=}}
4. ^{{Cite journal|last=Spence|first=Paul|last2=Griffies|first2=Stephen M.|last3=England|first3=Matthew H.|last4=Hogg|first4=Andrew McC.|last5=Saenko|first5=Oleg A.|last6=Jourdain|first6=Nicolas C.|date=2014-07-12|title=Rapid subsurface warming and circulation changes of Antarctic coastal waters by poleward shifting winds|url=http://doi.wiley.com/10.1002/2014GL060613|journal=Geophysical Research Letters|language=en|volume=41|issue=13|pages=4601–4610|doi=10.1002/2014gl060613|issn=0094-8276}}
5. ^{{Cite journal|last=Greene|first=Chad A.|last2=Blankenship|first2=Donald D.|last3=Gwyther|first3=David E.|last4=Silvano|first4=Alessandro|last5=Wijk|first5=Esmee van|date=2017-11-01|title=Wind causes Totten Ice Shelf melt and acceleration|url=http://advances.sciencemag.org/content/3/11/e1701681|journal=Science Advances|language=en|volume=3|issue=11|pages=e1701681|doi=10.1126/sciadv.1701681|issn=2375-2548}}
6. ^{{Cite journal|last=Anderson|first=R. F.|last2=Ali|first2=S.|last3=Bradtmiller|first3=L. I.|last4=Nielsen|first4=S. H. H.|last5=Fleisher|first5=M. Q.|last6=Anderson|first6=B. E.|last7=Burckle|first7=L. H.|date=2009-03-13|title=Wind-Driven Upwelling in the Southern Ocean and the Deglacial Rise in Atmospheric CO2|url=http://science.sciencemag.org/content/323/5920/1443|journal=Science|language=en|volume=323|issue=5920|pages=1443–1448|doi=10.1126/science.1167441|issn=0036-8075|pmid=19286547}}
7. ^{{Cite web|url = http://hurricane.ncdc.noaa.gov/pls/paleox/f?p=519:1:0::::P1_STUDY_ID:16197|accessdate = 18 August 2014|title = Data: 1000-year Southern Annular Mode reconstruction|publisher=National Climatic Data Center}}
8. ^{{cite news |last=Abram |first=Nerilie|url=http://www.nature.com/nclimate/journal/v4/n7/full/nclimate2235.html |title=Evolution of the Southern Annular Mode during the past millennium |work=Nature |date=2014-05-11 |accessdate=2014-09-13 }}

External links

  • http://www.antarctica.ac.uk/met/gjma/sam.html Observation-based SAM index from 1957–present
  • http://hurricane.ncdc.noaa.gov/pls/paleox/f?p=519:1:0::::P1_STUDY_ID:16197 1000-year Southern Annular Mode reconstruction
  • Monthly Southern Hemisphere Annular Mode (SAM) Index or Antarctic Oscillation (AAO) Index 1850 - 2013
  • Daily Southern Hemisphere Annular Mode (SAM) Index or Antarctic Oscillation (AAO) Index 1948 - 2013
  • http://www.cpc.ncep.noaa.gov/products/precip/CWlink/daily_ao_index/aao/aao.loading.shtml
  • https://web.archive.org/web/20081216220433/http://stratus.astr.ucl.ac.be/textbook//pdf/Chapter_5.pdf (chapter 5.2.3)
  • Animation of Southern Annular Mode in Victoria, Australia
  • [https://web.archive.org/web/20110706132255/http://stratus.astr.ucl.ac.be/textbook/chapter5_node6.html The Southern Annular Mode ] Introduction to climate dynamics and climate modelling, Université catholique de Louvain
{{Climate oscillations}}{{climate-stub}}

4 : Climate|Climate of Antarctica|Climate patterns|Environment of Antarctica

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