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Decadal variability of the Elbe River streamflow

机译:易北河水流的年代际变化

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The decadal variability (>7 years) of annual Elbe River flow in connection with large-scale atmospheric circulation is analysed for the period 1902-2002. The relationship with temperature over land (TT) and global sea surface temperature (SST) and atmospheric circulation over the Northern Hemisphere is investigated.High anomalies of the river flow are associated with a tripole-like pattern in the North Atlantic and with negative SST anomalies in the central North Pacific and positive anomalies in the eastern and central tropical Pacific. The pattern identified in the sea level pressure (SLP) resembles the negative phase of the Arctic Oscillation pattern.Two distinct decadal time components of approximately 12-13 years and 20 years in the time series were identified by using the Singular Spectral Analysis. To isolate the main frequencies identified by the Singular Spectrum Analysis (SSA) and to analyse the connection between the decadal components and Elbe River streamflow, we have applied a band pass filter to the SST field, to be able to suppress all the variance outside the prescribed windows.
机译:分析了1902-2002年期间易北河年流量与大规模大气环流的年代际变化(> 7年)。研究了北半球陆地温度(TT)和全球海表温度(SST)与大气环流之间的关系。北大西洋的河流流量高异常与三脚架状模式相关,并且与负SST异常相关在北太平洋中部出现,在东部和中部热带太平洋出现正异常。在海平面压力(SLP)中识别出的模式类似于北极涛动模式的负相位。使用奇异频谱分析识别了时间序列中大约12-13年和20年的两个不同的年代际时间分量。为了隔离由奇异频谱分析(SSA)识别的主要频率并分析年代分量与易北河水流之间的联系,我们对SST字段应用了带通滤波器,以便能够抑制频谱外的所有变化。规定的窗户。

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