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Thin Ice Thickness Measured by Upward-Looking Sonar in a Marginal Sea

机译:上海声纳测得的薄冰厚度

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摘要

Upward-looking sonar (ULS) has been used successfully to observe icernthickness in polar regions since the 1990s, but studies of applying ULSrnto the measurement of thin ice are rare. In the 2003/2004 winter, a ULSrnwas deployed to measure ice thickness at an oil platform in Bohai Sea.rnThe data, with a relatively high sampling frequency, were transmittedrnthrough a cable from the observation system and stored in a computerrnset on the platform and also sent to a remote computer in real time. Arnpractical model to derive the thickness of thin ice in the marginal icernzones is developed. In the Bohai Sea, the tide is one of the significantrnhydrodynamic features. The role of tide in affecting the residual totalrnerror in the determined mean ice thickness is discussed. The results ofrnsea ice thicknesses derived with the model were compared tornobservations and estimates from analysis of digital camera images. Thernmodel shows reasonable skill in detecting ice less than 0.5 m thick.
机译:自1990年代以来,向上声纳(ULS)已成功用于观测极地的冰厚,但很少有将ULSrn用于测量薄冰的研究。在2003/2004年冬季,部署了ULSrn来测量渤海石油平台上的冰厚度.rn数据以较高的采样频率通过观测系统的电缆传输,并存储在平台上的计算机中。实时发送到远程计算机。建立了推论边缘冰带薄冰厚度的实用模型。在渤海,潮汐是重要的水动力特征之一。讨论了潮汐对确定的平均冰层厚度中剩余总误差的影响。用该模型得出的海冰厚度结果与冰冻观测结果进行了比较,并通过对数码相机图像的分析进行了估算。该模型显示出检测厚度小于0.5 m的冰的合理技巧。

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