Southern Hemisphere climate: the modern record

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منابع مشابه

Southern Hemisphere Climate: the Modern Record

SALINGER, M.J. & JONES, P.D., 1996 (xi): Southern Hemisphere climate: the modern record. In Banks, M.R. & Brown, M.J. (Eds): CLIMATIC SUCCESSION AND GLACIAL HISTORY OF THE SOUTHERN HEMISPHERE OVER THE LAST FIVE MILLION YEARS. Pap. Proc. R. Soc. T asm. 130(2): 101-107. ISSN 0080-4703. National Institute of Water and Atmospheric Research (NIWA), PO Box 109 695, Newmarket, Auckland, New Zealand (M...

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Potential for Southern Hemisphere climate surprises

Climate model results suggest that future climate change in Antarctica will be accompanied by continued strengthening and poleward contraction of the Southern Ocean westerly wind belt. Paleoclimate records suggest past changes in the westerly winds can be abrupt and that healing of the Antarctic ozone hole could lead to poleward contraction of the westerlies and increased meridional atmospheric...

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Interpretation of recent Southern Hemisphere climate change.

Climate variability in the high-latitude Southern Hemisphere (SH) is dominated by the SH annular mode, a large-scale pattern of variability characterized by fluctuations in the strength of the circumpolar vortex. We present evidence that recent trends in the SH tropospheric circulation can be interpreted as a bias toward the high-index polarity of this pattern, with stronger westerly flow encir...

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Simulation of recent southern hemisphere climate change.

Recent observations indicate that climate change over the high latitudes of the Southern Hemisphere is dominated by a strengthening of the circumpolar westerly flow that extends from the surface to the stratosphere. Here we demonstrate that the seasonality, structure, and amplitude of the observed climate trends are simulated in a state-of-the-art atmospheric model run with high vertical resolu...

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Obliquity Control On Southern Hemisphere Climate During The Last Glacial

Recent paleoclimate reconstructions have challenged the traditional view that Northern Hemisphere insolation and associated feedbacks drove synchronous global climate and ice-sheet volume during the last glacial cycle. Here we focus on the response of the Patagonian Ice Sheet, and demonstrate that its maximum expansion culminated at 28,400 ± 500 years before present (28.4 ± 0.5 ka), more than 5...

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ژورنال

عنوان ژورنال: Papers and Proceedings of the Royal Society of Tasmania

سال: 1996

ISSN: 0080-4703

DOI: 10.26749/rstpp.130.2.101