Tao Yulong, Zhang Yiran, Kong Xiangzhen, Zhang Sheng, Xue Yufei, Ao Wen, Pang Bo, Dou Huashan, Xue Bin
Water Conservancy and Civil Engineering College, Inner Mongolia Agricultural University, Hohhot, 010018, China; Hulunbuir Academy of Inland Lakes in Northern Cold and Arid Areas, Hulunbuir, 021008, China; State Gauge and Research Station of Wetland Ecosystem, Hulun Lake, Inner Mongolia, China.
Key Laboratory of Lake and Watershed Science for Water Security, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, 211135, China; State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing, 211135, China.
Environ Res. 2025 Mar 1;268:120813. doi: 10.1016/j.envres.2025.120813. Epub 2025 Jan 9.
Cyanobacterial blooms represent a significant environmental issue posing widespread threats to global aquatic ecological health. Climate and nutrient enrichment were the most studied factors modulating cyanobacterial blooms in eutrophic lakes. However, in many floodplain lakes, the importance of hydrological variation in driving and predicting cyanobacterial blooms is often overlooked and largely underestimated, which has hampered the effectiveness of lake management. Here, we use a process-based lake ecosystem model (GOTM-WET) to evaluate the potential drivers of the record-setting cyanobacterial bloom during summer 2022 (>70% of lake area) in the largest shallow lake in Northern China (Hulun Lake). The model was calibrated based on a comprehensive field dataset including both remote sensing (surface water temperature) and in-lake observations (water quality). We performed a scenario analysis with various combinations of nutrient loading, hydrological variations and climate change. Our modeling results unravel that the profound water level rise through 2021 to 2022 serves as the main trigger of the severe cyanobacterial bloom in summer 2022. Our model predicted a decrease of 60.5% in the annual average of cyanobacterial biomass when water level remained stable. In addition, water level change and nutrient concentration explains 72.5% of the variance in long-term maximum area of cyanobacterial blooms. Our model further reveals that the water level rise drives the cyanobacterial bloom via bringing in excessive nutrient to lake water column from the lake basin. Thus, our results suggest that continuous increase in water level across two years could serve as an early warning signal to cyanobacterial blooms in the consecutive summer. Our findings may be applicable to similar temperate shallow lakes in floodplain areas, especially for those located in agricultural and pasture regions with abundant nutrient legacy, thus may provide a new indicator for cyanobacterial blooms prediction.
蓝藻水华是一个重大的环境问题,对全球水生生态健康构成广泛威胁。气候和营养物质富集是富营养化湖泊中调节蓝藻水华的研究最多的因素。然而,在许多洪泛平原湖泊中,水文变化在驱动和预测蓝藻水华方面的重要性常常被忽视且严重低估,这阻碍了湖泊管理的有效性。在此,我们使用基于过程的湖泊生态系统模型(GOTM-WET)来评估中国北方最大的浅水湖泊(呼伦湖)2022年夏季创纪录的蓝藻水华(>70%的湖区面积)的潜在驱动因素。该模型基于包括遥感(地表水温度)和湖内观测(水质)在内的综合实地数据集进行了校准。我们对营养负荷、水文变化和气候变化的各种组合进行了情景分析。我们的建模结果表明,2021年至2022年期间水位的大幅上升是2022年夏季严重蓝藻水华的主要触发因素。我们的模型预测,当水位保持稳定时,蓝藻生物量的年平均值将下降60.5%。此外,水位变化和营养浓度解释了蓝藻水华长期最大面积变化的72.5%。我们的模型进一步揭示,水位上升通过将过多营养物质从湖盆带入湖水水柱来驱动蓝藻水华。因此,我们的结果表明连续两年水位持续上升可能是连续夏季蓝藻水华的预警信号。我们的研究结果可能适用于洪泛平原地区类似的温带浅水湖泊,特别是那些位于营养物质丰富的农业和牧区的湖泊,从而可能为蓝藻水华预测提供一个新的指标。