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Mechanisms of variability in decadal sea-level trends in the Baltic Sea over the 20th century

机译:20世纪波罗的海年代际海平面趋势变化的机制

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Coastal sea-level trends in the Baltic Sea display decadal-scale variations around a?long-term centennial trend. In this study, we analyse the spatial and temporal characteristics of the decadal trend variations and investigate the links between coastal sea-level trends and atmospheric forcing on a decadal timescale. For this analysis, we use monthly means of sea-level and climatic data sets. The sea-level data set is composed of long tide gauge records and gridded sea surface height (SSH) reconstructions. Climatic data sets are composed of sea-level pressure, air temperature, precipitation, evaporation, and climatic variability indices. The analysis indicates that atmospheric forcing is a?driving factor of decadal sea-level trends. However, its effect is geographically heterogeneous. This impact is large in the northern and eastern regions of the Baltic Sea. In the southern Baltic Sea area, the impacts of atmospheric circulation on decadal sea-level trends are smaller. To identify the influence of the large-scale factors other than the effect of atmospheric circulation in the same season on Baltic Sea sea-level trends, we filter out the direct signature of atmospheric circulation for each season separately on the Baltic Sea level through a?multivariate linear regression model and analyse the residuals of this regression model. These residuals hint at a?common underlying factor that coherently drives the decadal sea-level trends in the whole Baltic Sea. We found that this underlying effect is partly a?consequence of decadal precipitation trends in the Baltic Sea basin in the previous season. The investigation of the relation between the AMO index and sea-level trends implies that this detected underlying factor is not connected to oceanic forcing driven from the North Atlantic region.
机译:波罗的海沿岸海平面趋势显示了长期百年趋势附近的年代际尺度变化。在这项研究中,我们分析了年代际趋势变化的时空特征,并以年代际尺度研究了沿海海平面趋势与大气强迫之间的联系。对于此分析,我们使用海平面和气候数据集的每月平均值。海平面数据集由潮汐仪记录和网格海面高度(SSH)重建组成。气候数据集由海平面压力,气温,降水,蒸发和气候变异指数组成。分析表明,大气强迫是十年海平面趋势的推动因素。但是,其影响在地理位置上是不同的。这种影响在波罗的海的北部和东部地区影响很大。在波罗的海南部地区,大气环流对年代际海平面趋势的影响较小。为了确定除同一季节的大气环流影响以外的其他大规模因素对波罗的海海平面趋势的影响,我们通过以下方法过滤出每个季节的大气环流在波罗的海海平面上的直接特征:多元线性回归模型并分析该回归模型的残差。这些残差暗示了共同推动整个波罗的海年代际海平面趋势的共同潜在因素。我们发现,这种潜在影响部分是前一个季节在波罗的海盆地年代际降水趋势的结果。对AMO指数与海平面趋势之间关系的调查表明,这种检测到的潜在因素与北大西洋地区驱动的海洋强迫没有关系。

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