2011-2018年北冰洋测高海面高度异常和地转速度

Francesca Doglioni, R. Ricker, B. Rabe, T. Kanzow
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引用次数: 3

摘要

摘要近几十年来,北极海冰的减少改变了从大气到冰和海洋的垂直动量通量,从而影响了地表环流。在过去的十年里,卫星测高对了解这些变化做出了贡献。然而,来自冰雪覆盖地区的数据需要专门处理,导致冰雪覆盖地区和公海地区在偏差、校正和数据覆盖方面不一致。因此,仍然需要努力生成一致的全北极数据集,以便在全盆地尺度上研究北冰洋表面环流。在这里,我们提供并评估了海面高度异常和地转速度的月度网格数据集。本数据集基于2011年至2018年北极海冰覆盖和开放海域(北纬88°)的Cryosat-2观测数据,使用数据插值变分分析(DIVA)方法进行插值。在本研究之前,82°N以北地区没有地转速度。为了检验结果的稳健性,我们将生成的场与一个独立的测高数据集以及来自系泊的海底压力、立体高度和近表面海洋速度的独立数据进行了比较。与近地表海洋速度的比较结果表明,我们的地转速度场可以解析宽度大于50 km的边界流的季节到年际变化。在前人文献的基础上,进一步讨论了海面高度和地转速度的季节周期。出现了大尺度特征,即10 - 1月是全北极最大海面高度,其中陆架上的波幅最大,冬季北极斜坡流在盆地范围内加速。该数据集不仅可以用于研究大尺度海面高度和环流,还可以用于研究区域受限边界流。该数据集以netCDF格式可从PANGAEA获得,网址为[目前正在审查的数据]。
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Sea surface height anomaly and geostrophic velocity from altimetry measurements over the Arctic Ocean (2011–2018)
Abstract. In recent decades the decline of the Arctic sea ice has modified vertical momentum fluxes from the atmosphere to the ice and the ocean, thereby affecting the surface circulation. In the past ten years satellite altimetry has contributed to understand these changes. However, data from ice-covered regions require dedicated processing, originating inconsistency between ice-covered and open ocean regions in terms of biases, corrections and data coverage. Thus, efforts to generate consistent Arctic-wide datasets are still required to enable the study of the Arctic Ocean surface circulation at basin-wide scales. Here we provide and assess a monthly gridded dataset of sea surface height anomaly and geostrophic velocity. This dataset is based on Cryosat-2 observations over ice-covered and open ocean areas of the Arctic up to 88° N for the period 2011 to 2018, interpolated using the Data-Interpolating Variational Analysis (DIVA) method. Geostrophic velocity was not available north of 82° N before this study. To examine the robustness of our results, we compare the generated fields to one independent altimetry dataset and independent data of ocean bottom pressure, steric height and near-surface ocean velocity from moorings. Results from the comparison to near-surface ocean velocity show that our geostrophic velocity fields can resolve seasonal to interannual variability of boundary currents wider than about 50 km. We further discuss the seasonal cycle of sea surface height and geostrophic velocity in the context of previous literature. Large scale features emerge, i.e. Arctic-wide maximum sea surface height between October and January, with the highest amplitude over the shelves, and basin wide seasonal acceleration of Arctic slope currents in winter. We suggest that this dataset can be used to study not only the large scale sea surface height and circulation but also the regionally confined boundary currents. The dataset is available in netCDF format from PANGAEA at [data currently under review].
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