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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Sea surface temperatures in cooler climate stages bear more similarity with atmospheric CO _2 forcing
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Sea surface temperatures in cooler climate stages bear more similarity with atmospheric CO _2 forcing

机译:海洋表面温度在凉爽气候阶段熊与大气CO _2更相似迫使

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The interglacial Marine Isotope Stage (MIS) 11 received special attention due to its remarkable resemblance with present-day climate. Based on synchronicity of marine, ice sheet and terrestrial proxy responses, warm episodes with intervening cool phase(s) at MIS 11 are qualitatively established. Here we quantitatively evaluate 15 climate proxies during 368-552 kyr intervals adopting a novel long-range cross-correlation approach and information theory based similarity measures. We also estimate the information flow rate and dominant flow direction between these climate variables using transfer entropy and the related directionality index. Our results unequivocally establish that atmospheric CO _2 (pCO2) is the driving signal while all other proxies used in this study are the responses. The climate forcing greenhouse gas, the atmospheric CO _2 (pCO2) and the response signals like sea surface temperature (SST) and carbon isotope composition of total organic carbon (δ ~(13)CTOC) proxies are strongly correlated (?1 or -1) without significant observable time lag (less than 1 kyr). Various substages of MIS 11 are recognizable in the SST data alone based on normalized similarity measures. Additionally, eight more proxies from lacustrine sediments are identified as primary. During the cooler substages these proxies bear more similarity with ambient atmospheric pCO2. Thus, the information theory-based similarity measures suggest that atmospheric CO _2 fluctuations are best captured by at least 9 climate proxies during cooler interglacial events. Based on the results related to interglacial MIS 11 and 13 obtained in this study, an important implication relevant to anthropogenic CO _2 input to the present-day atmosphere can be distilled. It is that sensitive and better-coupled response proxies such as SST and MAT, which already show an increasing trend, are likely to behave in a more dissimilar manner in future. That is, they tend to behave more independently in the near future (?0.75 kyr).
机译:间冰期海洋同位素阶段(MIS) 11由于其显著的收到了特别的关注相似,与当今的气候。同步性的海洋,冰盖和地面代理反应,温暖的情节干预降温阶段(s)在MIS 11定性。在368 - 552可以评估15气候代理采用一种新型远程互相关方法和信息理论基于相似的措施。信息流量和占主导地位的流向这些气候变量之间使用转移熵和相关方向指数。结果明确建立大气公司“_2(二氧化碳分压)是所有驱动信号在这项研究中使用的其他代理都响应。大气CO .) _2(二氧化碳分压)和响应海表面温度(SST)和信号总有机碳同位素组成碳(δ~(13)中华奥)代理强烈相关(?可观测时滞(小于1可以)。子阶段的MIS 11对海温辨认数据基于归一化的相似措施。湖泊沉积物被确定为主要。在冷却器子阶段这些代理承担与周围大气二氧化碳分压更相似。因此,基于理论的相似的信息表明,大气CO _2措施波动是最好被至少9在冷却器间冰期气候代理事件。间冰期MIS 11和13了研究中,一个重要的含义有关人为公司_2今天的输入气氛可以蒸馏。和代理等SST better-coupled响应垫,已经表现出增加的趋势,可能会表现得更不同的方式在未来。独立在不久的将来可以0.75(?)。

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