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首页> 外文期刊>Progress in Oceanography >Variability of the meridional overturning circulation at the Greenland-Portugal OVIDE section from 1993 to 2010
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Variability of the meridional overturning circulation at the Greenland-Portugal OVIDE section from 1993 to 2010

机译:1993年至2010年格陵兰-葡萄牙OVIDE部分的子午向翻转环流的变化

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摘要

The meridional overturning circulation (MOC) in the North Atlantic transports heat from the subtropics to high latitudes and hence plays an important role in the Earth's climate. A region crucial for the MOC is the northern North Atlantic and the adjacent Nordic Seas, where waters transported northward in the MOC upper limb progressively cool, gain density and eventually sink. Here we discuss the variability of the gyre circulation, the MOC and heat flux as quantified from a joint analysis of hydrographic and velocity data from six repeats of the Greenland to Portugal OVIDE section (1997-2010), satellite altimetry and Argo float measurements. For each repeat of the OVIDE section, the full-depth absolute circulation and transports were assessed using an inverse model constrained by ship-mounted Acoustic Doppler Current Profiler data and by an overall mass balance. The obtained circulation patterns revealed remarkable transport changes in the whole water column and evidenced large variations (up to 50% of the lowest value) in the magnitude of the MOC computed in density coordinates (MOC sigma). The extent and time scales of the MOC sigma variability in 1993-2010 were then evaluated using a monthly MOC sigma index built upon altimetry and Argo. The MOC sigma index, validated by the good agreement with the estimates from repeat hydrographic surveys, shows a large variability of the MOC sigma at OVIDE on monthly to decadal time scales. The intra-annual variability is dominated by the seasonal component with peak-to-peak amplitude of 4.3 Sv (1 Sv = 10(6) m(3) s(-1)). On longer time scales, the MOC sigma index varies from less than 15 Sv to about 25 Sv. It averages to 18.1 +/- 1.4 Sv and shows an overall decline of 2.5 +/- 1.4 Sv (95% confidence interval) between 1993 and 2010. The heat flux estimates from repeat hydrographic surveys, which vary between 0.29 and 0.70 +/- 0.05 PW, indicate that the heat flux across the OVIDE section is linearly related to the MOC sigma intensity (0.054 PW/Sv). (C) 2013 Elsevier Ltd. All rights reserved.
机译:北大西洋的子午翻转循环(MOC)将热量从亚热带转移到高纬度地区,因此在地球气候中起着重要作用。对MOC至关重要的地区是北大西洋北部和邻近的北欧海域,在MOC上肢向北运输的水逐渐变凉,增加密度并最终下沉。在这里,我们讨论了环流的可变性,MOC和热通量,这是根据对格陵兰至葡萄牙OVIDE断面(1997-2010年)的六个重复的水文和速度数据,卫星测高仪和Argo浮标测量的联合分析所量化的。对于OVIDE部分的每个重复,使用反模型评估全深度绝对循环和运输,该模型受船载声学多普勒电流剖面仪数据和整体质量平衡的限制。所获得的循环模式显示了整个水柱中的显着运输变化,并证明了以密度坐标(MOC sigma)计算的MOC大小存在较大变化(最高为最小值的50%)。然后使用建立在测高仪和Argo上的每月MOC sigma指数评估1993-2010年MOC sigma变异的程度和时间尺度。 MOC sigma指数通过与重复水文调查的估计值良好吻合而得到验证,该指数显示了OVIDE上MOC sigma的每月到十年时间范围的较大变化。年内变化主要由季节分量决定,其峰峰值幅度为4.3 Sv(1 Sv = 10(6)m(3)s(-1))。在较长的时间尺度上,MOC sigma指数从小于15 Sv到大约25 Sv不等。它的平均值为18.1 +/- 1.4 Sv,并且在1993年至2010年之间总体下降了2.5 +/- 1.4 Sv(95%置信区间)。重复水文测量的热通量估计值在0.29到0.70 +/-之间变化0.05 PW表示穿越OVIDE截面的热通量与MOCσ强度(0.054 PW / Sv)呈线性关系。 (C)2013 Elsevier Ltd.保留所有权利。

著录项

  • 来源
    《Progress in Oceanography》 |2015年第3期|250-261|共12页
  • 作者单位

    UBO, CNRS, Ifremer IRD, Ifremer Ctr Brest,Lab Phys Oceans,UMR 6523, F-29280 Plouzane, France;

    UBO, IFREMER, IRD, Ifremer Ctr Brest,Lab Phys Oceans,UMR 6523, F-29280 Plouzane, France;

    PP Shirshov Oceanol Inst, Moscow, Russia;

    UBO, IFREMER, IRD, Ifremer Ctr Brest,Lab Phys Oceans,UMR 6523, F-29280 Plouzane, France;

    UBO, CNRS, Ifremer IRD, Lab Phys Oceans,UMR 6523, F-29285 Brest, France;

    UBO, CNRS, Ifremer IRD, Ifremer Ctr Brest,Lab Phys Oceans,UMR 6523, F-29280 Plouzane, France;

    PP Shirshov Oceanol Inst, Moscow, Russia;

    UBO, CNRS, Ifremer IRD, Ifremer Ctr Brest,Lab Phys Oceans,UMR 6523, F-29280 Plouzane, France;

    UBO, CNRS, Ifremer IRD, Ifremer Ctr Brest,Lab Phys Oceans,UMR 6523, F-29280 Plouzane, France;

    UBO, CNRS, Ifremer IRD, Ifremer Ctr Brest,Lab Phys Oceans,UMR 6523, F-29280 Plouzane, France;

    UBO, IFREMER, IRD, Ifremer Ctr Brest,Lab Phys Oceans,UMR 6523, F-29280 Plouzane, France;

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