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MEAN SEA LEVEL IN THE ARCTIC OCEAN FROM SATELLITE ALTIMETRY

机译:来自北极海洋的平均海平面来自卫星高度的海洋

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The Arctic region’s climate is undergoing rapid changes. However, identifying such changes is difficult due to lack of observational data. In particular sea level variability is largely unknown. Satellite altimetry has proven to be an effective way of monitoring sea level changes on global and regional scales. At high latitudes, satellite altimetry suffers from low data quality and its use is not as straightforward. After investigating some sources of low satellite data quality at high latitudes, we derive a new processing for the Arctic Ocean region. We use this processing of satellite altimetry data to generate a set of weekly multimission grids over the 1993-2009 period. This improved dataset provides a better sampling of the Arctic Ocean compared to the AVISO multi-mission global grids used as a reference. The new dataset is used to calculate new estimates of regional and local sea level variability and trends which are slightly different from previous estimates of Arctic Ocean mean sea level rise. This work provides one of the first reliable attempts to evaluate regional sea level rise in the Arctic Ocean from satellite altimetry data.
机译:北极地区的气候正在进行快速变化。然而,由于缺乏观察数据,识别出这种变化是困难的。特别是海平面变异性很大程度上是未知的。卫星Altimetry已被证明是监测全球和区域尺度的海平面变化的有效方式。在高纬度地区,卫星Altimetry患有低数据质量,其使用并不直接。在高纬度地调查一些低卫星数据质量的来源之后,我们推导了北极海域的新加工。我们使用该处理卫星Altimetry数据来在1993 - 2009年期间生成一组每周的多重网格。与使用作为参考的Aviso多任务全球网格相比,这种改进的数据集提供了更好的北极海洋。新数据集用于计算区域和地方海平面变异性的新估计,趋势与以前的北极海洋平均海平面上升略有不同。这项工作提供了首次可靠的尝试中,从卫星高度数据中评估北冰洋区域的区域海平面上升之一。

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