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首页> 外文期刊>Progress in Physical Geography >Reconstructions of the southern annular mode (SAM) during the last millennium
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Reconstructions of the southern annular mode (SAM) during the last millennium

机译:南方环形模式(SAM)的重建在最后一千年期间

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摘要

>The leading mode of atmospheric variability in the Southern Hemisphere is the Southern Annular Mode (SAM), which affects the atmosphere and ocean from the mid-latitudes to the Antarctic. However, the short instrumental record of the SAM does not adequately represent its multi-decadal to centennial-scale variability. Long palaeoclimatic reconstructions of the SAM would improve our understanding of its low frequency behavior and its effects on regional temperature, rainfall, sea ice, and ecosystem processes. In this progress report, we review three published palaeoclimatic reconstructions available for understanding multi-decadal to centennial-scale variability of the SAM. Reconstructions reviewed here show similar patterns of decadal SAM variability during the last two centuries, but earlier centuries are less coherent. Reconstructions clearly maintain similar trends towards more positive SAM states since the onset of significant anthropogenic climate forcing from rising greenhouse gas (GHG) concentrations and ozone depletion and these excursions appear unprecedented over at least the last 500 years. We describe how new multi-proxy reconstructions of the SAM could further improve our understanding of its long-term variability and effects across all geographic sectors of the Southern Hemisphere. Here, we recommend careful selection and development of proxies in SAM-sensitive regions and seasons. In particular, proxies related to cool-season conditions and from the poorly-sampled Indian Ocean sector would allow for a true circumpolar and year-round reconstruction of past SAM variability.
机译:>南半球大气变化的主要模式是南环形模式(SAM),影响从中纬度到南极的大气和海洋。然而,SAM的短仪器记录并不能充分反映其从几十年到百年尺度的变化。对SAM的长期古气候重建将提高我们对其低频行为及其对区域温度、降雨、海冰和生态系统过程的影响的理解。在本进度报告中,我们回顾了三次已发表的古气候重建,这些重建可用于理解SAM的多个年代到百年尺度的变化。这里回顾的重建显示了过去两个世纪中SAM的十年变化的类似模式,但早期的世纪不太一致。自温室气体(GHG)浓度上升和臭氧消耗导致的重大人为气候强迫开始以来,重建显然保持了向更积极的SAM状态发展的类似趋势,这些变化至少在过去500年中是前所未有的。我们描述了SAM的新多代理重建如何进一步提高我们对其长期可变性的理解,以及对南半球所有地理区域的影响。在这里,我们建议在SAM敏感区域和季节仔细选择和开发代理。特别是,与冷季条件和印度洋部门取样不良相关的代理将允许对过去SAM变化进行真正的绕极和全年重建

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