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Characteristics of Ice Bottom Topography from the Sea of Okhotsk off Hokkaido: Observation Results in 2007

机译:北海道鄂霍次克海冰底地形特征:2007年观测结果

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Bottom-mounted IPS and ADCP were used to monitor the drafts and drifts of the pack ice passing over the mooring site on the Sea of Okhotsk off Hokkaido. A spectrum of sea ice bottom topography (draft profile) with non-stationary characteristics was estimated by the locally stationary AR model to compare it with the results in the past. The normalized spectrum of ice bottom topography might be common regardless of spatial and temporal component. Also, we found that the significant amplitude of sea ice draft, which means the standard deviation multiplied by 3.4, would give a subjective/intuitive the height of roughness of the bottom topography.
机译:底部安装的IPS和ADCP用于监视经过北海道鄂霍次克海停泊处的浮冰的吃水和漂移。通过局部平稳的AR模型估算了具有非平稳特征的海冰海底地形(吸水剖面)频谱,并将其与过去的结果进行了比较。不论空间和时间成分如何,冰底地形的归一化频谱可能很常见。此外,我们发现海冰吃水的幅度很大,这意味着标准偏差乘以3.4,将在主观/直觉上给出底部地形的粗糙度高度。

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