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- W3151014657 abstract "水存储为全球、本地的领域的理解水周期并且为监视气候和环境变化有重要意义。作为在水文学的一个关键变量，水存储变化代表降水，蒸发，表面流量，土壤水和地下水交换的和。在 20032008 的时期期间浇存储变化数据因为黄河的来源区域从严肃恢复和气候实验(优雅) 卫星数据是镇定的。每月实际的蒸发根据水平衡方程被估计。模仿的实际蒸发是显著地一致的并且有不仅观察平底锅(20 厘米) 的关联词数据，而且 2 简单生物圈建模的版本的模仿的结果。在在春天，夏天，秋天和冬季的蒸发是 130.9 公里， 275.2 公里， 74.3 公里和 26.1 公里的地方， Tangnaihai 盆的平均年度蒸发是 506.4 公里，并且分别地说明了 25.8% 平均年度蒸发， 54.3% ， 14.7% 和 5.2% 。降水稍微增加了，实际蒸发显示出明显的减少。黄河的来源区域的水存储变化从 2003 ～ 2008 每月显示了 0.51 公里的增加，它显示存储能力显著地增加了，可能由永久冻土的降级和活跃的层的厚度的增加引起了。实际蒸发的衰落和水存储能力的增加导致了河流量的增加。" @default.
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- W3151014657 date "2013-01-01" @default.
- W3151014657 modified "2023-09-24" @default.
- W3151014657 title "Estimation of water balance in the source region of the Yellow River based on GRACE satellite data" @default.
- W3151014657 hasPublicationYear "2013" @default.
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