冯琦, 李广雪, 2024. 基于Sentinel-1的辽东湾海冰冰情监测[J]. 海岸工程, 43(1): 66-78. doi: 10.12362/j.issn.1002-3682.20230716001.
    引用本文: 冯琦, 李广雪, 2024. 基于Sentinel-1的辽东湾海冰冰情监测[J]. 海岸工程, 43(1): 66-78. doi: 10.12362/j.issn.1002-3682.20230716001.
    FENG Q, LI G X, 2024. Monitoring of sea ice situation in the Liaodong Bay based on Sentinel-1 data[J]. Coastal Engineering, 43(1): 66-78. doi: 10.12362/j.issn.1002-3682.20230716001
    Citation: FENG Q, LI G X, 2024. Monitoring of sea ice situation in the Liaodong Bay based on Sentinel-1 data[J]. Coastal Engineering, 43(1): 66-78. doi: 10.12362/j.issn.1002-3682.20230716001

    基于Sentinel-1的辽东湾海冰冰情监测

    Monitoring of Sea Ice Situation in the Liaodong Bay Based on Sentinel-1 Data

    • 摘要: 辽东湾是渤海的三大海湾之一,在每年冬季经常会遭受大面积海冰灾害影响。本文选取2015年至2023年Sentinel-1 A/B遥感数据,对照Landsat-8数据采用灰度共生矩阵提取SAR影像纹理特征,对比了神经网络、支持向量机以及最大似然分类三种分类方法的精度;统计2015年至2023年辽东湾海冰冰情信息,研究了气温、海表面温度、盐度与海冰的相关关系和相互影响。研究结果表明:对于Sentinel-1 A/B数据,最大似然分类方法精度最高,分类精度达到82.75%;辽东湾海冰通常在12月底或者1月初开始发育,辽东湾结冰顺序为由北向南、由近岸向远岸,消融时顺序为由西向东、由远岸向近岸;辽东湾海冰与气温的Pearson相关系数为−0.502(P<0.01),与海表面温度的Pearson相关系数为−0.553(P<0.01),说明辽东湾冰情与气温、海表面温度为显著负相关,海表面温度对海冰的形成、发育及消融影响更大。此外,盐度对于海冰的影响存在一定的滞后性。

       

      Abstract: The Liaodong Bay is one of the three big bays in the Bohai Sea. It can be affected frequently by large area of sea ice disasters in every winter season. To study the correlation and mutual influences between the sea ice and the air temperature, sea surface temperature and salinity, the remote sensing data of Sentinel-1 A/B obtained in winters from 2015 to 2023 are used, the SAR image textural features are extracted by contrasting Landsat-8 satellite imagery and utilizing gray scale co-occurrence matrix, the precisions of classification methods such as neural network, support vector machine and maximum likelihood classification are compared and the information about sea ice in the Liaodong Bay from 2015 to 2023 is summarized. The results show that for the Sentinel-1 A/B data, the maximum likelihood classification method has the highest precision, being up to 82.75%. The sea ice in the Liaodong Bay begin to form usually at the end of December or the beginning of January and follows a freezing order of north to south and near-shore to far-shore. The sea ice melting order is, however, from west to east and far-shore to near-shore. In the Liaodong Bay the Pearson correlation coefficient is −0.502 (P<0.01) between the air temperature and the sea ice and −0.553 (P<0.01) between the sea surface temperature and the sea ice, indicating that the sea ice in the Liaodong Bay has a significant negative correlation both to the air temperature and to the sea surface temperature. This suggests that both the air temperature and the sea surface temperature have an impact on the formation, development and melting process of the sea ice, of which the sea surface temperature may exert an even greater influence. As to the salinity, its influence on the sea ice exhibits a certain lag.

       

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