圣塔菲纳平原流域的洪水动力学

E. Espinosa, L. Rodríguez, Carlos Scioli
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摘要

本文研究了阿根廷圣达菲省典型平原盆地受水地表的时间演变、空间分布和发生频率。该分析基于2000-2021年期间Landsat 8和MODIS图像获得的mnwi时间序列。采用MNDWI阈值法对开放水面和混合水面进行了识别。此外,还探讨了受水影响面随降水季节周期变化的时间波动,这将受到前期储水量的影响。大部分受水影响的表面由混合水组成,开放水面由某些出现频率较高的水体组成,位于盆地的下部。上部有一个聚集区与“cañadas”区域重合。在盆地的其他部分,受水影响的地表发生频率较低。这些结果有助于了解研究区水动力学,对区域水资源的规划和管理具有重要意义。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Dinámica de inundación de una cuenca de la llanura Santafecina
This paper studies the temporal evolution, spatial distribution and frequency of occurrence of water-affected surfaces in a typical plain basin of Santa Fe Province (Argentina). The analysis was based on MNDWI time series, obtained from Landsat 8 and MODIS images of the period 2000-2021. By MNDWI thresholding, Open Water and Mixed Water surfaces were identified. In addition, the temporal fluctuation of water-affected surfaces in response to the seasonal cycle of precipitation was explored, which would be influenced by the antecedent water storage. Most of the water-affected surfaces are composed of Mixed Water, Open Water surfaces are made up of certain water bodies with a high frequency of occurrence, located in the lower part of the basin. A sector of accumulation in the upper part coincides with an area of "cañadas". In other sectors of the basin, the surfaces affected by water have low frequencies of occurrence. These results contribute to the knowledge of water dynamics of the study area, and are very useful for the planning and management of the region’s water resources.
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