Duan Zihao, Wang Guangsheng, Hu Jielong, Yu Tong, Chen Songgui, Zhang Yajing, Wang Yang, Liu Haicheng, Zhao Xu, Chen Hanbao
National Engineering Laboratory for Port Hydraulic Construction Technology, Tianjin Research Institute for Water Transport Engineering, Tianjin, China.
Key Laboratory of Ecosystem Network Observation and Modeling, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, China.
PLoS One. 2025 Jun 4;20(6):e0325546. doi: 10.1371/journal.pone.0325546. eCollection 2025.
Dynamic changes to the northern Caspian Sea shoreline have significant ecological implications, including impacts to biodiversity and the surrounding environment. This study employs Landsat datasets, historical records, and geographic information systems (GIS) to quantitatively analyze spatiotemporal variations along the northern Caspian Sea coastline from 1985 to 2023. The findings demonstrate pronounced cyclic variations in the Caspian Sea's water level. Compared to 1930, the water level decreased by 2.6 m by 2023, with 1935 marking the onset of a significant downward trend. From 1995 to 2023, a pronounced decline in the water level at a rate of 6.1 cm/year was observed. Multiscale temporal oscillations in water levels revealed periodic rises and falls with cycles ranging from 6-8 years to 10-16 years. Due to the broad and shallow morphology of the northern Caspian Sea, fluctuations in water level have resulted in significant displacements of the northern coastline. Between 1985 and 2023, the shoreline length decreased by 262 km, which is equivalent to a 17% reduction. The intensity of the coastline length index reached a critical point during from 2010 to 2015, after which it declined sharply by 3.67. By 2023, the coastline had shifted seaward by 1.33 × 10⁴ km2 relative to that in 1985. This continuous retreat of the shoreline poses a severe threat to the ecological stability of the northern Caspian Sea. If the trend persists, then the disappearance of the eastern basin of the South Aral Sea may be replicated in the northern Caspian Sea by 2100. These findings provide critical insights for formulating effective coastal management strategies and conservation initiatives.
里海北部海岸线的动态变化具有重大的生态影响,包括对生物多样性和周边环境的影响。本研究利用陆地卫星数据集、历史记录和地理信息系统(GIS)对1985年至2023年里海北部海岸线的时空变化进行定量分析。研究结果表明里海的水位存在明显的周期性变化。与1930年相比,到2023年水位下降了2.6米,1935年标志着显著下降趋势的开始。1995年至2023年期间,观察到水位以每年6.1厘米的速度显著下降。水位的多尺度时间振荡显示出周期性的上升和下降,周期从6 - 8年到10 - 16年不等。由于里海北部宽广且浅的形态,水位波动导致北部海岸线发生了显著位移。1985年至2023年期间,海岸线长度减少了262公里,相当于减少了17%。海岸线长度指数的强度在2010年至2015年期间达到临界点,之后急剧下降了3.67。到2023年,海岸线相对于1985年已向海移动了1.33×10⁴平方公里。海岸线的持续退缩对里海北部的生态稳定性构成了严重威胁。如果这种趋势持续下去,到2100年,里海北部可能会重现南咸海东部盆地消失的情况。这些发现为制定有效的海岸管理策略和保护举措提供了关键见解。