摘要
建立了一个水量平衡模型，并用１９９８、１９９９年淮河流域能量和水循环试验（ＨＵＢＥＸ）期间获得的史灌河流域（ＨＵＢＥＸ水文试验区）加密观测资料来率定模型中的参数。结论表明：（１）水量平衡的要素计算合理；（２）梅山、鲇鱼山、蒋集土壤含水量的平均值系列基本上反映了流域蓄水量的变化过程；（３）流域蓄水量的衰减系数、蒸发能力的折算系数比较稳定，不应通过调整这些系数来实现水量平衡。
Water balance models discussed in the paper are based on the drainage basin scale vision of the equation of continuity. The various continuous water movement processes included in hydrological cycle are lumped over finite time intervals and areas. Water balance models (simple version likes equation P= E1 + R+ I+ S, etc.) are constituted, some parameters related to water balance equation are estimated from the observed date in IOP of 1998 and 1999 in the Shiguan river catchment which was an experimental region for HUBEX. Pertinent analysis and results are presented in this study.
出处
《气候与环境研究》
CSCD
2001年第2期234-239,共6页
Climatic and Environmental Research
基金
国家自然科学基金资助项目49794030
