S - stratiform 中文 - EN166

stratiform adj.成層狀的；顯出層理的；層狀的〔如云層〕。

stratify
There is a vaporizing layer below 0 layer and it is far thick , which may be one of the important reasons of small precipitation on ground ; in the paper the cloud and the rain drop size distribution in warm layer of stratiform cloud are calculated and analyzed . it is found that n ( d ) = n0dnexp ( - a d ) can express the size distributions of little cloud drops , big cloud drops and rain drops . the observational and calculated results are well matched 在零度層以下蒸發層的存在，且比較深厚，應是導致地面雨強較小的重要因素之一；本文對暖層的云滴譜和雨滴譜進行了計算，對小云滴、大云滴和雨滴分布可以用同一種形式的分布密度函數多階函數n ( d ) = n _ 0d ~ nexp ( - d )來表示。
This work aims at studying multi - scale structures of large - scale stratiform precipitating clouds typical of henan province of central - eastern china in spring and autumn drought periods of china , the potentials and techniques of artificial rain increase . through analysis of historical weather / climate and cloud physical data , developed are a number of multi - scale observational schemes including intensive observational items , and space / time resolutions of data for integrative field observations to obtain real - time measurements of the structures at large - , medium - , small - and micro - scale . from analysis of observed separate items , their integrative treatment and numerical simulation we place focus on case studies and their integration in investigating such structures of stratiform precipitating clouds over the target region , rainfall physical mechanisms and exploitation of artificial rainfall increase potentials , whereupon a conceptual model is constructed and a range of catalysis schemes are proposed to improve smaller - scale forecasting accracy and techniques for the rainfall increase , with the dominant results given below 以地處中原、具有典型代表意義的河南層狀降水云系為主要研究對象，在對該地歷史天氣氣候和云物理等資料分析的基礎上，研究設計云系多尺度觀測方案(包括加密觀測項目、觀測時空分辨率) ，實施有設計的外場綜合觀測，獲取云系結構多尺度(大、中、小、微)配套的實時觀測資料；通過對各種觀測資料的分項和綜合處理分析，以典型個例觀測和數值模擬分析研究為重點，綜合多個例分析，研究河南層狀降水云系多尺度宏微觀結構特征、降水物理機制和人工增雨潛力條件，建立典型層狀云系人工增雨概念模型，研究科學的人工增雨作業技術系統。
In this paper aircraft has made vertical and synthetic detecting flying purposefully on 9 . 17 , 2003 according to cloud ' s macro and microstructure . vertical layers and representative places of stratiform cloud on 9 . 17 , 2003 are analyzed using the observational data of particle measurement system ( pms ) , combined with satellite data , radar data , and precipitation data on ground . by this we have got cloud ' s microphysical structure and physical process of the natural precipitation , and the physical effect evidence has been testified according to observational data after lco2 seeding 本文用綜合觀測的方法，利用機載pms云粒子探測系統，根據云系的宏微觀結構特征進行有針對性的垂直探測飛行，配合衛星、雷達、地面雨量、雨強計網觀測資料對2003年9月17日延安降水性層狀云系中那些有代表性的部位或垂直分層做細致的觀測分析，獲得云系的微物理結構和自然降水形成的物理過程，并用觀測事實來驗證人工增雨引晶催化后的物理響應判據。
There are a series of lead - zinc polymetallic deposits , such as fozichong , dongtao , xiashui , wenlongjing and jilongding distributed along the fault zone . these deposits have some similiar features : ? ll of them are bounded in the strata of lower palaeozoic group ; ? ain orebodies occur as stratiform or stratoid form with occurrence consistent with that of host strata ; ? tratiform skam or baritic rock are the direct country rock of orebodies ; ? ypical syngenetic sedimentary fabric preserved in the ore . these deposits may be included in the same metallogenic series 佛子沖、東桃、下水、文龍徑、雞籠頂等一系列鉛鋅多金屬礦床沿該斷裂帶分布，這些礦床雖然在成礦規模、賦礦層位和礦石礦物組成等方面存在一些差異，但均產于下古生界地層中；主要礦體呈層狀、似層狀產出，與地層產狀大體一致；直接賦礦圍巖為層狀綠色巖或重晶石巖；礦石中保留有典型的同生沉積組構。
The green - rock has following features : ? he stratiform green - rock ' s mode of occurrence is conformable with that of the strata , and there are typical syngenetic sedimentary structure in the rock ; ( 2 ) the stratiform green - rock is constituted mainly by bistagite without zonal distribution around magmatic rocks 作者首次提出賦礦的綠色巖建造概念。其中層狀綠色巖是佛子沖礦田層狀、似層狀礦體的直接賦礦圍巖，這種層狀綠色巖一直被視為矽卡巖。
Stratiform clouds are layered clouds formed mainly by uplifting of air on a large scale , commonly seen near a front , which signifies the interface of warm , moist air climbing up cold air on encountering the latter 烏云接日頭，半夜雨稠稠的層狀云天氣：層狀云主要由大范圍的氣流上升運動形成，常見于鋒面附近，即暖濕空氣碰到冷氣團，向上爬升的交界面上。
Therefore , two mineralization periods ore divided , which can be called as hot - water sedimention period and telescoping period . stratiform green - rock is the direct country rock of bedded orebodies . the rock was called as skam in the past 作者將本區成礦過程劃分出兩個成礦期，即早志留世熱水沉積成礦期和燕山期巖漿?熱液疊生改造成礦期。
There is an active growth layer and super cooled water exists with ice crystals that may be an important feature layer to occur rain in stratiform cloud 過冷水滴和冰晶共存層存在，且冰晶活躍增長，此層的存在可能是發生降水的關鍵。
Atmospheric systems responsible for stratiform precipitating clouds in henan during spring and autumn are low pressure ? cold front , and surface cyclone 造成河南春秋季層狀降水云系的主要天氣系統有低槽冷鋒和地面氣旋兩大類。
It was sunny most of the time that day , but by dusk stratiform clouds could be faintly seen approaching from the west left hand side 象站向北面拍攝的天氣照片。當天日間普遍天晴，黃昏時隱約可見層狀云正從西方左面移近。
It was sunny most of the time that day , but by dusk stratiform clouds could be faintly seen approaching from the west ( left hand side ) 當天日間普遍天晴，黃昏時隱約可見層狀云正從西方（左面）移近。
The auther regards the stratiform green - rock as a kind of exhalative sedimentary rock which is different from contact - metasomatic skarn 此類綠色巖是一類區域性展布的特殊類型的噴流巖。
The stratiform skarns of hydrothermal fluid sedimentary origin are well developed in kendekoke gold deposit , qinhai province 摘要熱水沉積成因層矽卡巖在青海省肯德可克金礦區非常發育。
The rain from thick stratiform clouds usually lasts longer than showers although the intensity is lighter 由深厚層狀云產生的降水，通常比驟雨持續的時間長，但雨勢較小。
Numerical simulation on the mesoscale structure and organization of a stratiform cloud system in henan province 河南省層狀降水云系中尺度結構的數值模擬
As the warm , moist air goes up , the moisture therein will condense into extensive stratiform clouds 當暖濕空氣抬升時，水汽冷卻凝結成大范圍的層狀云。
Investigation on catalyst dosage in aircraft cloud seeding in stratiform clouds 層狀云飛機增雨催化劑用量研究
Exploration programmes are based on drilling for the stratiform deposits along projections of established trends . 勘探計劃依靠鉆探，鉆探層狀礦床沿著已知走向的延伸部分進行。