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Study on Spatial Characteristics of Sea Ice Reserves in Liaodong Bay of China

机译:中国辽东湾海冰储量空间特征研究

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The sea ice reserves in Liaodong Bay at periods of winter 1999/2000 was estimated using remote sensing. The ice thickness was estimated based on the exponent relationship between ice thickness and its reflectivity, The ice area was obtained by NOAA/AVHRR data at channel 1. To understand the distribution of sea ice reserves, Liaodong Bay was divided into 11 regions and each region was further subdivided into 5 plots in terms of the topographic trend and the distance from coast. The sea ice at the reserves was statistically counted for each plot over different periods. The maximum ice reserve in a normal ice year during the period of grand ice in a natural environment is 30X10~8 m~3, with the center of maximum ice thickness moving from the center of the sea to the eastern coast with the passing of a specific ice period. More ice reserves are distributed on the eastern coast of Liaodong Bay located in the regions between Ying-Kou and Xiong-Yue, and the western coastal regions around Xing-Cheng, whichmake up 30%-50% of the total ice reserves within Liaodong Bay. These regions are in the best positions to be set up as exploited bases. With respect to the increasing distance from the coast, the sea ice reserves decreased in the eastern coast, increasing slightly to the western coast.
机译:利用遥感估算了辽东湾1999/2000年冬季的海冰储量。根据冰层厚度与反射率之间的指数关系估算冰层厚度,利用NOAA / AVHRR数据在通道1获得冰面积。为了解海冰储量的分布,辽东湾分为11个区域,每个区域根据地形趋势和到海岸的距离,又分为5个地块。对不同时期每个地块的保护区海冰进行统计。自然环境下盛大冰期,正常冰年的最大储冰量为30X10〜8 m〜3,最大冰厚中心随海平面的变化而从海心向东部海岸移动。具体的冰期。营口至熊岳之间的辽东湾东海岸和兴城附近​​的西部沿海地区分布有更多的冰储量,占辽东湾总储冰量的30%-50% 。这些地区处于建立被利用基地的最佳位置。随着距海岸距离的增加,东海岸的海冰储量减少,至西海岸的海冰储量略有增加。

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