1) strong convective cloud
强对流云团
1.
Based on EOS/MODIS multi-channel remote sensing data,the characteristics of a strong convective cloud were analysed qualitatively according to a heavy rainfall in the northern of Anhui province from 30, June to 1,July in 2006.
根据EOS/MODIS多通道遥感数据,针对2006年6月30日20:00～2006年7月1日20:00安徽省北部出现的一次强降水,定性地分析了产生暴雨的强对流云团的特征,揭示了强对流降水云团的云系特征和结构特征,并用地面雨量观测资料开展验证分析。
2) convective cloud
对流云团
1.
Hail s strength are associated with convective cloud s evolution and strength.
北疆夏季两次冰雹天气过程的对比分析发现,充足的水汽、足够大的上升运动和不稳定的层结是冰雹天气出现的必备条件,而降雹的强弱则与对流云团的发展和强度有关。
2.
The first strong precipitation is caused by strengthening local convective clouds generated in the subtropical high,vapor transportation and dynamic conditions offered by strengthened easterly flow in bottom of the troposphere air promote the development of convection;New clouds in the humid air environment will be rapidly strengthened and developed.
通过对常规气象资料分析,发现①第一时段的强降水由副热带高压内部产生的局地对流云团加强造成,对流层底层东风气流的加强提供的水汽输送和动力抬升作用,促进了对流发展;②新生云团进入潮湿的大气环境中能够得到迅速的发展加强。
3) convective cloud cluster
对流云团
1.
Based on analysing 9 cases of mesoscale convective cloud cluster over clod front cloud system during 1994~2002, it was found that the origin in which the mesoscale convective cloud was outgrowth located in middle and southern parts of Guizhou province .
通过对1994～2002年间9次由冷锋云系中尺度对流云团分析,发现广西前汛期冷锋云系中尺度对流云团的源地主要是黔西南和黔中;移动方向是东或东南;当环境云场强度指数≥28有利对流云团的发展,≤26时不利对流云团的发展;初步研究了中尺度对流云团生命史不同阶段的卫星云图形态特征,给出了中尺度对流云团降水的时空分布特征。
2.
The mainly features of mesoscale convective cloud clusters during four heavy rainfall stages in Changjiang River Basin have been studied by using GMS TBB data of every hour on every day from June to August in 1998.
运用１９９８年６～８月逐日逐时ＧＭＳ辐射亮度温度ＴＢＢ资料，统计和分析了长江 流域４个大暴雨时段中各自中尺度对流云团活动的一些主要特征，指出长江流域的这场罕见 大水是在特定的环流形势下，由３１５个β中尺度和α中尺度对流云团直接造成的。
4) convective cloud cell splitting
对流云团提取
5) convective cloud clusters
孟湾对流云团
1.
This paper analyses the northward movement and activity of convective cloud clusters over the Bay of Bengal through May to June.
结果表明:初夏孟湾对流云团活动对低纬高原的初夏降水有明显影响;孟湾北部及其东部海域和沿岸是对流云团北上频数最多的地区;下风方伴随风速大值区的西南气流有利于孟湾云团北上;孟湾云团北上与西太平洋副热带高压的活动和位置关系密切。
6) Tropical convective cloud cluster
热带对流云团
补充资料：上海益昌薄板有限公司强对流全氢罩式热处理炉
上海益昌薄板有限公司强对流全氢罩式热处理炉
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