Analysis of spatio-temporal variability of Pacific water distribution in the Sea of Okhotsk based on Lagrangian approach

K. K. Kivva, M. V. Budyansky, M. Y. Uleysky, S. V. Prants
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Abstract

The aim of this work is characteristic of spatio-temporal variability of Pacific water distribution in the Sea of Okhotsk based on Lagrangian approach and spatial analysis. Materials and methods . The study is based on geostrophic current data product from satellite altimetry. The dataset has resolution of 0,25° × 0,25° × 1 day. This data is used for calculation of approximately 100000 water parcels trajectories during 400 days back in time for every day from 31st of January 1997 to 17th of April 2022. For each date in this interval, those parcels which intersected the conditional Kuril transect were determined, as well as region and date of transect intersection. Those two parameters were used in cluster analysis with DBSCAN method in order to distinguish individual Pacific intrusions. Position, shape, and size of each intrusion were investigated. Results allowed to suggest two types of indexes describing distribution of Pacific-origin water in the Sea of Okhotsk. First, centroid of particles of Pacific origin with residence time between 1 and 6 months is calculated. Variability of centroid position showed northward displacement of Pacific waters in spring-summer and south[1]ward displacement in autumn-winter. Eastward displacement towards Kamchatka coast usually occurs during winters and opposite westward displacement is usual for summers. In 1998, 2003, 2010, 2013, 2017, and 2019 waters of Pacific origin had the most northern location. Second type of indexes is based on location and shape characteristics of Pacific water intrusions. The fractal dimensionality and convexity measure of intrusions are rapidly decreasing after the intrusion reaches its maximum area. Centroids of the most prominent intrusions follow the path along 152–154 °E. Both types of indices showed intensification of Pacific inflow since 2010. Practical value . The time-series of resulted indexes are suggested to be implemented in integrated ecosystem assessments of the eastern Sea of Okhotsk.
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基于拉格朗日方法的鄂霍次克海太平洋水分布时空变异分析
基于拉格朗日方法和空间分析,研究了鄂霍次克海太平洋水分布的时空变化特征。材料和方法。该研究基于卫星测高的地转流数据产品。数据集的分辨率为0.25°× 0.25°× 1天。该数据用于计算从1997年1月31日到2022年4月17日每天400天内大约100000个水包的轨迹。对于该区间内的每个日期,确定与条件千岛样条相交的地块,以及样条相交的区域和日期。用DBSCAN方法对这两个参数进行聚类分析,以区分太平洋入侵的个体。研究了每个侵入的位置、形状和大小。结果允许提出两种描述鄂霍次克海太平洋源水分布的指标。首先,计算太平洋源粒子停留时间在1 ~ 6个月之间的质心。质心位置的变异表现为春夏太平洋海域向北移动,秋冬太平洋海域向南移动[1]。向堪察加海岸的向东位移通常发生在冬季,相反的向西位移通常发生在夏季。1998年、2003年、2010年、2013年、2017年和2019年,太平洋海域的位置最靠北。第二类指标基于太平洋水侵的位置和形态特征。在侵入面积达到最大值后,侵入的分形维数和凹凸度迅速减小。最突出的侵入体的质心沿152-154°E的路径移动。两类指标均显示2010年以来太平洋流入加剧。实用价值。建议将结果指标的时间序列应用于鄂霍次克海东部生态系统综合评价。
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