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1)  precipitation and P-E
降水和有效降水
2)  efficient precipitation
有效降水
3)  effective precipitation
有效降水
1.
The causes of climate dry in loess plateau area of Gansu province are autumn rain precipitations, great variation in year-to-year precipitation, less effective precipitation, air drying and windy, therefore,freguent natural disaster can lead forest ecological construction more and more difficult.
秋雨型降水、降水年际变化大、有效降水少、大气干燥多风等因素叠加在一起,构成了甘肃省黄土高原区气候干旱的本质所在,频繁的自然灾害进一步导致该区林业生态建设难上加难。
4)  precipitation effectiveness
降水有效性
5)  Effective precipitation
有效降水量
1.
After statistically analyzing the relationship of the 10 days total precipitation as the landslide occurring on 1 615 samples of Chongqing, it can be obtained the relationship of the rainfall, the time of the landslide taking place and the probability of the landslide taking place,which is given landslides induced by the effective precipitation definitions, calculati.
通过对重庆1615个滑坡个例与其发生前10d降水量值做统计分析,揭示了降水量、滑坡发生时间、滑坡发生概率三者之间的关系,由此给出了诱发滑坡的有效降水量定义、计算思路和计算公式,并依此建立了强降水诱发的滑坡预报模型。
2.
through the analysis on relationship and change trend between the precipitation and effective precipitation in growth period of winter wheat,effective precipitation calculation models under different time scale were given in Xinxiang area,which to meet the demand of regional agricultural development and water resources optimization management.
通过模拟结果分析冬小麦生长期降水量和有效降水量相互关系及变化趋势,确定了该地区不同时长尺度下冬小麦生育期有效降水量适宜计算模式,以满足区域农业发展规划及水资源优化配置管理的需求。
6)  effective rainfall
有效降水量
1.
Based on the pertinent iterature,the calculation methods of effective rainfall in growing period on dry crop was analysed and summarized in this paper,which combines with research situation of calculation methods of effective rainfall.
在查阅国内外相关文献的基础上,对目前有效降水量的研究方法进行了简要的评述,并结合现有有效降水量计算模式,对它们的适应性和计算结果的可靠性进行了对比分析。
2.
Based on the small-scale hydrology theory and the effective rainfall,a new soil water resources calculating model was put forward,which calculated the soil water resources by water balance principle.
依据小尺度水文学原理,提出了基于有效降水量的土壤水资源计算模型,利用水量平衡原理计算土壤水资源量。
补充资料:降水
降水
precipitation

   从云雾降落到地面的液态水或固态水。常见的形式有雨、雪、冰雹等。按降水的性质又可分为连续性、阵性和间歇性降水。阵性降水开始和停止都比较突然,降水强度变化大;连续性降水持续时间较长,降水强度变化不大;间歇性降水的降水强度较弱,并常有一定长时间的断续现象。降水的形成主要决定于上升气流的强弱和水汽供应量充足与否。产生降水的主要过程有:①天气系统的发展,暖而湿的空气与冷空气交汇,促使暖湿空气被冷空气强迫抬升,或由暖湿空气沿锋面斜坡爬升。②夏日的地方性热力对流,使暖湿空气随强对流上升形成小型积雨云和雷阵雨。③地形的起伏,使其迎风坡产生强迫抬升,但这是一个比较次要的因素。多数情况下,它和前两种过程结合影响降水量的地理分布。
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