1) moisture frontal zone
湿度锋
1.
The results show that unbalance force of atmospheric motion and the coupling reaction among convective cloud cluster and moisture frontal zone and low level jet lead to the continuation of strong c.
分析结果发现,大气运动非平衡强迫、凝结降水的非均匀分布与强烈垂直风切变的耦合作用、“湿度锋”与低空急流的耦合相互作用通过促进低空辐合流的维持,导致了对流云团和暴雨天气的持续。
2) Humidity front frontogenesis
湿度锋锋生
3) low-level moisture frontal zone
低层湿度锋区
1.
In the Meiyu season most of the severe MCSs(mesoscale convective systems) with torrential rain may form,develop,move and newly emerge up and down-stream along such "low-level moisture frontal zone".
结果表明,与积云对流加热场有最密切关系的低层湿度条件及其水平分布不均匀性质都对扰动的波速和稳定度有重要影响,最有利出现不稳定发展的地方是在“低层湿度锋区”南界附近,因此这里是中尺度对流系统(MCS)的活跃地带。
4) wetting front
湿润锋
1.
Study on the wetting front of water infiltration and soil water redistribution in aeolian sandy soil
风沙土水分入渗与再分布过程中湿润锋运移试验研究
2.
Results show that precipitation intensity has a large impact on moisture wetting front distribution, with reasonable agreement between model simulation and measured data.
建立了一维垂直非饱和土壤水分运动的数学模型,并采用有限差分方法对模型进行数值求解,模拟了不同降雨强度条件下水分分布的动态规律,数值模拟结果表明:降雨强度的大小直接影响着土壤水分湿润锋的分布,并且所建立的模型与实验测试结果吻合较好,验证了模型的可靠性,从而可为定量化研究填埋气体和浸出液释放提供理论根据。
3.
The accumulated infiltration and wetting front in different infiltration heads were studied by horizontal column in this paper.
通过对不同入渗水头下的土壤累积入渗量及湿润锋进行分析,得出了累积入渗量与不同入渗水头以及湿润锋与不同入渗水头之间的变化规律,即随着入渗水头的增加,其累积入渗量和湿润锋在整体上有增加的趋势,但其增加的趋势并非像恒定水头时的土壤累积入渗量那样呈乘幂分布,而是具有一定的阶梯性,呈阶梯形增加。
5) wetted front
湿润锋
1.
A series of experiments about the effect of dripper discharge,amount of applied water and dripper distance on soil wetted front had been researched under interference.
通过模拟试验,研究了不同滴头流量、灌水量和滴头间距下双点源滴灌水分交汇作用对湿润锋运动规律的影响,结果表明:在交汇界面,湿润锋水平和垂直入渗距离与入渗时间符合多项式关系,在未发生交汇的平面符合幂函数关系。
2.
Through indoor soil infiltration experiment in earth tank,the movement of the wetted front,the shape and size of the wetted zone were observed and measured.
为了了解插入式渗灌灌水器的土壤湿润特性,并确定其插入阻力,通过室内土箱灌水试验,观察、测定了插入式渗灌的湿润锋运移情况及湿润区形状、尺寸等数据资料,同时还通过室内、室外土壤插入试验,对灌水器在不同容重土壤中的插入阻力、插入方法等进行了探讨。
3.
Through observing the wetted front, it was found to move faste.
通过对湿润锋的观测 ,发现出流量较大的滴头 ,其湿润锋向上运移速度较快。
6) ratio of wetting front
湿润锋比值
补充资料：凝结湿度表(见露点湿度表)
凝结湿度表(见露点湿度表)
川呀j一e sh，d日biao凝结湿度表见露点湿度表。
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