1) high precipitation
大降水带
1.
Annual precipitation at the equilibrium line varies from 500 to 3000 mm, and a high precipitation zone is in the gla.
大降水带的成因主要归于冷下垫面和高湿度场的作用。
2) zone of maximum precipitation
最大降水高度带
1.
Based on the data observed,it was found that: 1) summer precipitation displayed a decreasing trend from east to west in the intermediate altitude with a rate of approximately 80 mm·(100 km-1);2) the zone of maximum precipitation lay between 4 500 to 4 700 m a.
(100 km)-1;最大降水高度带位于海拔4 500~4 700 m左右,年降水量为485 mm,该高度带与本区最大相对湿度高度层(海拔4 600 m左右)以及夏季气温零温层高度(海拔4 680 m左右)相一致。
3) atmospheric precipitation
大气降水
1.
Kuitun environmental monitoring station monitored acid rain in 2002 for mastering atmospheric precipitation status and major contamination of Kuitun city.
为了解奎屯市大气降水状况及主要污染物,奎屯市监测站于2002年对大气降水进行了为期一年的酸雨监测。
2.
Through statistical analysis on dada of atmospheric precipitation samples of 8 cities from 1992 to 1997,this paper deliberated on temporal and spatial variation of pH of atmospheric precipitation in Jinlin province,China.
通过对吉林省８ 个代表城市１９９２ － １９９７ 年大气降水观测数据的统计分析，对大气降水ｐＨ 值的时空分异进行了探讨。
3.
The water source is regarded as atmospheric precipitation,and the heat source is regarded as that the groundwater is heated by itself deep circulation.
认为其水源为大气降水,热源为深循环加热,热储温度96℃,环流深度3 000~4 000 m。
4) meteoric water
大气降水
1.
Components of fluid is similar with meteoric water.
马家窑金矿床是胶东地区比较典型的石英脉型金矿床代表,属中低温热液矿床,成矿流体盐度较低,气相成分以H2O,CO2为主,其次是Na+,Ca+和Cl-,K+和F-较贫,流体的成分与大气降水热液相类似。
2.
Metallogenetic epoch was late Yanshanian and fluid derived from meteoric water.
成矿流体来源主要为大气降水。
3.
It is concluded that Zjinshan deposit formed mainly by the convective circulation of meteoric water.
认为该矿床主要由大气降水的环流形成。
5) Precipitation
[英][prɪ,sɪpɪ'teɪʃn] [美][prɪ'sɪpə'teʃən]
大气降水
1.
Analysis on the Origin and Characteristics of Chemical Composition of Precipitation in Jinhua;
金华市大气降水的化学组成特征及来源解析
2.
Establishment of Chinese Network of Isotopes in Precipitation (CHNIP) Based on CERN;
基于CERN的中国大气降水同位素观测网络
3.
A study on hydrogen and oxygen isotopes composition of precipitation in Xiamen;
厦门大气降水的氢氧同位素研究
6) Heavy rainfall
大降水
1.
This paper analysed the contributin g factor of a heavy rainfall process i n October of 2001.
对哈密2001年10月大降水天气过程的降水成因进行了分析,表明低空急流和上升运动是其形成的重要机制,同时在哈密地区大降水天气短期预报着眼点方面获得了一些有益的启示。
2.
This paper describs the main influencing system lead to a heavy rainfall in southern Hami in June 23 in 2000,for example Southern Xinjiang trough, northern cold- air and Middle- low level shear etc,and analyzes its character base on thermodynamics and dynamics factors.
对造成哈密南部“2000·6·23”大降水的主要影响系统:南疆低槽、北方冷空气、中低层切变等进行了描述,并从热力因素、动力因素两方面对其特征予以剖析,得到哈密南部大降水预报的某些着眼点。
补充资料：板带轧制速度规程(见板带轧制规程设计)
板带轧制速度规程(见板带轧制规程设计)
speed schedule for plate and strip rolling
bandai zhazhi sudu guieheng板带轧制速度规程(speed seheduxe fo:plateand strip rolling)见板带札制规程设计。
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