Gravelly soil slope surface shape and criticality under rainfall conditions
降雨作用下砾石土斜坡坡面形态及临界特性
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In general, the annual rainfall in these regions is less than annual water loss by evaporation.
总的来说, 这些地区的年降雨量比一年内由于蒸腾而失去的水分要少.
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The stability of expansive soil slope was studied considering the effect of rainfall.
在此基础上,研究了考虑降雨入渗影响的膨胀土基坑边坡稳定性问题.
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讨论了非饱和土边坡在入渗、蒸发条件下的三类边界条件表达形式.
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大豆是我国重要的经济作物和养地作物,南方大豆在其生长期降雨比较集中,容易遭受涝害。
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Dams maintain river flows during the winter and reduce flood peaks during the high rainfall period.
水坝在冬季帮助保持河水流量,在多雨时节则用来减小洪峰.
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Heavy rainfall makes a river rise while continuous dry weather makes a river sink.
大量降雨会使河水上涨,而连续干旱又会使河流水位下降.
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NCAR thinks the climate would be hotter and wetter, with rainfall about 10% heavier than now.
NCAR认为,气候将变得更炎热、潮湿,降雨量比目前增加10%。
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雨水利用工程的适用条件、水量平衡计算、下垫面径流系数的确定等是《建筑与小区雨水利用工程技术规范》编制中需要解决的关键技术。
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Perennial Cold Dews, the rainfall in southern China has increasingly reduced.
常年寒露期间,华南雨量亦日趋减少。
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以红壤丘陵景观中相对独立且整体性强的集水区为基本单元,重点研究了集水区内降水、蒸散、水量蓄存等地表水资源的年变化。
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The mean annual rainfall was 311.4 mm, most of which falling between May to Sept.
年平均降水量为311.4mm,降水集中在5-9月份。
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In a period of freezing weather, water in 0-20 cm soil layer mainly comes from rainfall in Sept.
封冻期020cm土层水分主要来源于910月份的降水。
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为流域分布式降雨-径流模型提供了可靠的实际蒸散量模拟方法。
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WRF模式分辨率对新疆异常降雨天气要素模拟的影响
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在分析全球季节降水量与ENSO的关系中,指出春季是春夏秋三季中最不显著的。
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