Changes in climate at high southern latitudes: A unique daily record at Orcadas spanning 1903-2008

The climate observations at Orcadas represent the only southern high-latitude site where data span more than a century, and its daily measurements are presented for the first time in this paper. Although limited to a single station, the observed warming trends are among the largest found anywhere on...

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Autor principal: Zazulie, N.
Otros Autores: Rusticucci, M., Solomon, S.
Formato: Capítulo de libro
Lenguaje:Inglés
Publicado: 2010
Acceso en línea:Registro en Scopus
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100 1 |a Zazulie, N. 
245 1 0 |a Changes in climate at high southern latitudes: A unique daily record at Orcadas spanning 1903-2008 
260 |c 2010 
270 1 0 |m Solomon, S.; NOAA/ESRL/CSD, 325 Broadway, Boulder, CO 80305, United States; email: susan.solomon@noaa.gov 
506 |2 openaire  |e Política editorial 
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504 |a Schneider, D.P., Steig, E., Ice cores record significant 1940s Antarctic warmth related to tropical climate variability (2008) Proc. Natl. Acad. Sci. USA, 105, pp. 12 154-12 158 
504 |a Marshall, G., Steig, E.J., van Ommen, T.D., Bitz, C.M., Dixon, D.A., Mayewski, P.A., Jones, J.M., Temperatures in Antarctica over the past two centuries (2006) Geophys. Res. Lett, 33, pp. L16707. , doi:10.1029/2006GL027057 
504 |a Steig, E.J., Schneider, D.P., Rutherford, S.D., Mann, M.E., Comiso, J.C., Shindell, D.T., Warming of the Antarctic ice-sheet surface since the 1957 international geophysical year (2009) Nature, 457, pp. 459-462 
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520 3 |a The climate observations at Orcadas represent the only southern high-latitude site where data span more than a century, and its daily measurements are presented for the first time in this paper. Although limited to a single station, the observed warming trends are among the largest found anywhere on the earth, facilitating the study of changes in extreme temperatures as well as averages. Factors that may influence Antarctic climate include natural variability; changes in greenhouse gases; and, since about the mid-1970s, the development of the ozone hole. The seasonality of observed warming and its temporal evolution during the century are both key for interpretations of Antarctic climate change. No statistically significant climate trends are observed at Orcadas from 1903 to 1950. However, statistically significant warming is evident at Orcadas throughout all four seasons of the year since 1950. Particularly in austral fall and winter, the warming of the cold extremes (coldest 5% and 10% of days) substantially exceeds the warming of the mean or of the warmest days, providing a key indicator for cold season Antarctic climate change studies. Trends in the summer season means and extremes since 1970 are approximately twice as large as those observed earlier, supporting suggestions of additional regional warming in that season because of the effects of ozone depletion on the circulation. Further, in the spring and summer seasons, significant mean warming also occurred prior to the development of the Antarctic ozone hole (i.e., 1950-70), supporting an important role for processes other than ozone depletion, such as greenhouse gas increases, for the climate changes. © 2010 American Meteorological Society.  |l eng 
593 |a Departamento de Ciencias de la Atmósfera y los Océanos, FCEN, Universidad de Buenos Aires, Argentina 
593 |a Consejo Nacional de Investigaciones Científicas y Técnicas, Buenos Aires, Argentina 
593 |a National Oceanic and Atmospheric Admin./Earth System Research Laboratory/Chemical Sciences Division, Boulder, Colorado, United States 
690 1 0 |a ANTARCTIC CLIMATE 
690 1 0 |a ANTARCTIC OZONE HOLE 
690 1 0 |a CLIMATE OBSERVATIONS 
690 1 0 |a CLIMATE TRENDS 
690 1 0 |a COLD SEASON 
690 1 0 |a EXTREME TEMPERATURES 
690 1 0 |a KEY INDICATOR 
690 1 0 |a NATURAL VARIABILITY 
690 1 0 |a OZONE DEPLETION 
690 1 0 |a OZONE HOLE 
690 1 0 |a REGIONAL WARMING 
690 1 0 |a SEASONALITY 
690 1 0 |a SOUTHERN LATITUDES 
690 1 0 |a SUMMER SEASON 
690 1 0 |a TEMPORAL EVOLUTION 
690 1 0 |a GLOBAL WARMING 
690 1 0 |a GREENHOUSE GASES 
690 1 0 |a OZONE LAYER 
690 1 0 |a OZONE 
700 1 |a Rusticucci, M. 
700 1 |a Solomon, S. 
773 0 |d 2010  |g v. 23  |h pp. 189-196  |k n. 1  |p J. Clim.  |x 08948755  |w (AR-BaUEN)CENRE-5480  |t Journal of Climate 
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