1) runoff depth
径流深
1.
The calculation of runoff depth for hydrological forecast was made by auto calculating function of Excel 2003 and IF function statement of computer.
利用Excel 2003的自动计算功能,配合IF函数语句进行水文预报的径流深计算,具有准确、快捷、方便等特点。
2.
Based on the observation and statistics of soil erosion and water loss in the sloping field,it is clear that the runoff depth and erosion would change along with the gradient,farming measures and vegetation.
基于四川省遂宁水土保持试验站坡耕地水土流失的观测数据统计,通过探讨降雨产生的地表径流深及冲刷量随坡度的变化,以及耕作措施和植被对坡面侵蚀的影响,提出坡耕地在降雨时的产流产沙规律:相同前提下,产流产沙量随坡度增加而增加;横坡耕作时,产流产沙量剧减,而顺坡耕作时产流产沙增加;种植农作物时,较之坡面植草,产流量减少,但产沙量增加。
3.
The result shows that the higher the river network fractal dimension is,the more complex the river network will be,which is represented by higher Hurst exponent of runoff depth,so the runoff process is more simple.
研究表明,流域水系分维数越高,水系越复杂,其径流深序列Hurst指数则越高,其径流过程则越简单,反之亦然。
2) deep runoff
深部径流
3) annual runoff
年径流深
1.
Inferences of the past annual runoff of the early and middle Holocene for Quzhou area, the southern Hebei Plain;
曲周地区早、中全新世古年径流深状况的推估
4) annual runoff depth
年径流深度
5) flood runoff depth
场洪径流深
6) saturated flow depth
饱和径流深
补充资料：热深厥深
热深厥深 热深厥深 病证名。指热厥证的征象。指邪热越深入，四肢厥冷的症状越严重，皆因阳气被遏，邪气内闭所致。属真热假寒证。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条