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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 17, issue 11
Ann. Geophys., 17, 1478–1492, 1999
https://doi.org/10.1007/s00585-999-1478-2
© European Geosciences Union 1999
Ann. Geophys., 17, 1478–1492, 1999
https://doi.org/10.1007/s00585-999-1478-2
© European Geosciences Union 1999

  30 Nov 1999

30 Nov 1999

The storm tracks and the energy cycle of the Southern Hemisphere: sensitivity to sea-ice boundary conditions

C. G. Menéndez1, V. Serafini2, and H. Le Treut2 C. G. Menéndez et al.
  • 1Centro de Investigaciones del Mar y la Atmósfera/CONICET-UBA, Ciudad Universitaria, Pabellón 2, Piso 2, (1428) Buenos Aires, Argentina
  • 2Laboratoire de Météorologie Dynamique/CNRS, Université P. et M. Curie, Tour 15-25, 4 place Jussieu, 75252 Paris Cedex 05, France

Abstract. The effect of sea-ice on various aspects of the Southern Hemisphere (SH) extratropical climate is examined. Two simulations using the LMD GCM are performed: a control run with the observed sea-ice distribution and an anomaly run in which all SH sea-ice is replaced by open ocean. When sea-ice is removed, the mean sea level pressure displays anomalies predominantly negatives near the Antarctic coast. In general, the meridional temperature gradient is reduced over most of the Southern Ocean, the polar jet is weaker and the sea level pressure rises equatorward of the control ice edge. The high frequency filtered standard deviation of both the sea level pressure and the 300-hPa geopotential height decreases over the southern Pacific and southwestern Atlantic oceans, especially to the north of the ice edge (as prescribed in the control). In contrast, over the Indian Ocean the perturbed simulation exhibits less variability equatorward of about 50°S and increased variability to the south. The zonal averages of the zonal and eddy potential and kinetic energies were evaluated. The effect of removing sea-ice is to diminish the available potential energy of the mean zonal flow, the available potential energy of the perturbations, the kinetic energy of the growing disturbances and the kinetic energy of the mean zonal flow over most of the Southern Ocean. The zonally averaged intensity of the subpolar trough and the rate of the baroclinic energy conversions are also weaker.

Key words. Air-sea interactions · Meteorology and atmospheric dynamics (climatology; ocean · atmosphere interactions)

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