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首页> 外文期刊>Journal of Climate >North Atlantic interdecadal variability: oceanic response to the North Atlantic oscillation (1865-1997)
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North Atlantic interdecadal variability: oceanic response to the North Atlantic oscillation (1865-1997)

机译:北大西洋年代际变化:海洋对北大西洋振荡的反应(1865-1997年)

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摘要

In contrast to the atmosphere, knowledge about interdecadal variability of the North Atlantic circulation is relatively restricted. It is the objective of this study to contribute to understanding how the North Atlantic circulation responds to a forcing by the North Atlantic oscillation (NAO) on interdecadal timescales. For this purpose, the authors analyze observed atmospheric and sea surface temperature (SST) data along with the response of an ocean general circulation model to a realistic monthly surface flux forcing that is solely associated with the NAO for the period 1865-1997. In agreement with previous studies, it is shown that the relationship between the local forcing by the NAO and observed SST anomalies on interdecadal timescales points toward the importance of oceanic dynamics in generating SST anomalies. A comparison between observed and modeled SST anomalies reveals that the model results can be used to assess interdecadal variability of the North Atlantic circulation. The observed/modeled developments of interdecadal SST anomalies during the periods 1915-39 and 1960-84 against the local damping influence from the NAO can be traced back to the lagged response (10-20 yr) of the North Atlantic thermohaline circulation and the subpolar gyre strength to interdecadal variability of the NAO. Additional sensitivity experiments suggest that primarily interdecadal variability in the surface net heat flux forcing associated with the NAO governs interdecadal changes of the North Atlantic circulation.
机译:与大气层相反,有关北大西洋环流年代际变化的知识相对有限。这项研究的目的是有助于了解北大西洋环流如何响应年代际尺度上的北大西洋振荡(NAO)强迫。为此,作者分析了观测到的大气和海表温度(SST)数据,以及海洋总环流模型对1865-1997年期间仅与NAO相关的现实月表面通量强迫的响应。与以前的研究一致,研究表明,NAO的局部强迫与年代际尺度上观测到的海温异常之间的关系指出了海洋动力学在海温异常产生中的重要性。对观测到的SST异常和模拟的SST异常之间的比较表明,该模型结果可用于评估北大西洋环流年代际变化。在1915-39年和1960-84年间,由于NAO的局部阻尼影响,年代际SST异常的观测/模拟发展可以追溯到北大西洋热盐环流和亚极的滞后响应(10-20年)。回转强度对NAO年代际变化的影响。其他敏感性实验表明,与NAO相关的表面净热通量强迫的年代际变化主要控制着北大西洋环流的年代际变化。

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