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Assessing recent trends in high-latitude Southern Hemisphere surface climate
Antarctic climate trends observed in the satellite record are compared with a two hundred year paleoclimate record. The satellite record is found to be too short to attribute changes to anthropogenic forcing, with natural variability overwhelming the forced signal. Understanding the causes of recent...
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Published in: | Nature climate change 2016-09, Vol.6 (10), p.917-926 |
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Main Authors: | , , , , , , , , , , , , , , , , , , , , , , , , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Antarctic climate trends observed in the satellite record are compared with a two hundred year paleoclimate record. The satellite record is found to be too short to attribute changes to anthropogenic forcing, with natural variability overwhelming the forced signal.
Understanding the causes of recent climatic trends and variability in the high-latitude Southern Hemisphere is hampered by a short instrumental record. Here, we analyse recent atmosphere, surface ocean and sea-ice observations in this region and assess their trends in the context of palaeoclimate records and climate model simulations. Over the 36-year satellite era, significant linear trends in annual mean sea-ice extent, surface temperature and sea-level pressure are superimposed on large interannual to decadal variability. Most observed trends, however, are not unusual when compared with Antarctic palaeoclimate records of the past two centuries. With the exception of the positive trend in the Southern Annular Mode, climate model simulations that include anthropogenic forcing are not compatible with the observed trends. This suggests that natural variability overwhelms the forced response in the observations, but the models may not fully represent this natural variability or may overestimate the magnitude of the forced response. |
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ISSN: | 1758-678X 1758-6798 |
DOI: | 10.1038/nclimate3103 |