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Pacific decadal climate variability: Indices, patterns and tropical-extratropical interactions

机译:太平洋年代际气候变率:指数,模式和热带-热带关系

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Pacific decadal variability (PDV) plays a critical role in the climate system. Here I present a review of indices and patterns of decadal climate variability in the Pacific from observations and palaeoclimate reconstructions. I examine the spatial characteristics of Pacific sea surface temperature variability and the metrics used to track observations of PDV. I find commonalities between the PDV patterns, the Interdecadal Pacific Oscillation (IPO) and its North and South Pacific counterparts, the Pacific Decadal and South Pacific Decadal Oscillations (PDO and SPDO). I present a tool to provide probabilistic quantification of the recent state of the IPO, and use the tool to provide reliable estimates of IPO state up to 2 years prior to the present. The tool indicates a probability of 80-90% that the IPO remained in its negative state until 2014-2015. I review palaeoclimate reconstructions of the IPO and PDO, and outline advances and challenges in our pre-instrumental understanding of PDV. I draw attention to a Pacific-wide tropical-extratropical mechanism that suggests that the cool and warm phases of PDV are not driven by tropical or extratropical variability alone, but are instead the result of continuous tropicalextratropical interactions on decadal timescales. I conclude by noting key sources of remaining uncertainty and emphasising the need to better understand decadal variability. This will occur through continual improvements in observations, an expansion of palaeoclimate exploration and data collection, and renewed efforts in model development.
机译:太平洋年代际变率(PDV)在气候系统中起着至关重要的作用。在这里,我从观测和古气候重建中回顾了太平洋年代际气候变化的指数和模式。我检查了太平洋海表温度变化的空间特征以及用于跟踪PDV观测值的度量。我发现PDV模式,年代际太平洋涛动(IPO)与它的北太平洋和南太平洋同行,太平洋年代际和南太平洋年代际振荡(PDO和SPDO)之间有共同点。我提出了一种工具,可以对IPO的最新状态进行概率量化,并使用该工具提供可靠的IPO状态(直至目前的2年)估计值。该工具表明,直到2014-2015年,IPO仍处于负状态的可能性为80-90%。我回顾了IPO和PDO的古气候重建,并概述了我们对PDV的仪器前理解的进步和挑战。我提请注意整个太平洋范围的热带-热带机制,这表明PDV的冷暖阶段不仅是由热带或热带外变率驱动的,而是在十年时间尺度上持续热带-热带互动相互作用的结果。最后,我指出了仍然存在不确定性的关键原因,并强调需要更好地了解年代际变异性。这将通过观测的不断改进,古气候探索和数据收集的扩大以及对模型开发的新努力来实现。

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