YANG Xing, WANG Shi-yan, HAN Zhen, LI Bu-dong, WANG Liang, WANG Jie, SUN Long, BA Yi-bo
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Ecological water replenishment is an important initiative for the ecological environment management of Baiyangdian, and this paper divides the ecological water replenishment process of Baiyangdian into a temporary water replenishment stage, an emergency water replenishment stage, and a stable water replenishment stage according to the change process of ecological water replenishment mechanism. In order to analyze the spatial and temporal pattern changes of water bodies in Baiyangdian under each ecological recharge stage, this paper extracts water bodies and ice bodies from 701 remote sensing images of Baiyangdian from 1990 to 2022 through the GEE platform, analyzes the spatial and temporal pattern of the water bodies under different stages, as well as specifically analyzes the change of the ice bodies' area in the winter freezing period. The main conclusions are as follows: ① In each ecological recharge stage, the water body area of Baiyangdian is the smallest in summer and the largest in winter and spring, and with the continuous improvement of ecological water replenishment mechanism, Baiyangdian water body area change amplitude is gradually reduced, showing the change rule of “cutting peaks to make up for the low”. The range of monthly average water area in the temporary water replenishment stage is between 0.63~186.03 km2, and that in the stable water replenishment stage is between 17.88~109.15 km2, the magnitude of change reduced by 50.77%; ②The perfection of ecological water replenishment mechanism makes Baiyangdian present the change rule of permanent water body increasing greatly and intermittent water body decreasing greatly, among which the permanent water body area in the temporary water replenishment stage is 7.66 km2, while the permanent water body area in the stable water replenishment stage is 23.62 km2, which is an increase of 208.16%, and the area of the intermittent water body is reduced from 263.50 km2 to 143.58 km2, a decrease of 45.51%; ③ From the perspective of the change of the ice body area, with the continuous improvement of ecological water replenishment mechanism, the area of Baiyangdian's ice body decreased continuously, in which the average area of the ice body in January decreased from 72.77 km2 to 12.60 km2, which was reduced by 82.69%. The results show that the improvement of the ecological water replenishment mechanism did not lead to the continuous increase of the water body area of Baiyangdian, but made the water body environment of Baiyangdian more fragmented; under the influence of global warming and other factors, the ice area of Baiyangdian was greatly reduced; this tendency to fragmentation of the characteristics of the watershed may not be conducive to the preservation of biodiversity, but given that ecosystems have a lag in their hydrological response, it is necessary to further strengthen the monitoring and research on the process of ecological and hydrological response.