| 1. | Positive vertical velocity existed between 700hpa and 500hpa
暖区700 500hpa之间一般存在上升气流。 |
| 2. | " the warm zones are spreading in this region into areas that weren ' t warm before
温暖区域正向在这个地区的非暖区扩大。 |
| 3. | But the air temperature change in chongqing karst region was complicated , not only occuring warming region , but also colding region
但岩溶区气温变化很复杂，既有变暖区又存在变冷区。 |
| 4. | The institute concentrates on the study of forming mechanism , physical process , forecasting technology of mesoscale heavy rain especially jianghuai meiyu front rain gush or heavy rain in prefrontal warmer area
研究重点是我国陆地暴雨，特别是江淮梅雨锋暴雨和锋前暖区暴雨，同时开展我国北方暴雨的比较研究。 |
| 5. | The ncep / ncar globally tropospheric 1 1 reanalysis data have been employed to select six landfall typhoon cases in order to diagnose variations of typhoon warm sectors in atmospheric boundary layer during their whole life periods
摘要采用ncep / ncar全球对流层1 1再分析格点资料，选取6个登陆台风个例，分析了不同发展阶段台风大气边界层暖区变化的特征及其与强度变化的关系。 |
| 6. | Heavy rainfall occurred in the warm area , and maximum rainfall lay in the windward slope where the width of raindrop size distribution was b roadened and sometimes it was bimodal spectrum . the shape of rain band in cold area was zonal , and the area of rain band was small
暖区有明显的强降水中心，雨强极大值出现在山区迎风坡，降水雨滴谱谱宽较大，有时滴谱呈双峰型分布；冷区降水区常呈带状分布，雨区范围大，雨滴谱较窄，雨滴谱为单峰型。 |
| 7. | The region getting warm appeared in the northeast of chongqing , the characteristics of which was that maximum air temperature became warmer than minimum air temperature . the regions getting cold took place in the middle and southeast of chongqing , mainly resulting from maximum air temperature
变暖区发生在渝东北的岩溶区，主要特征是最高、最低气温都变暖，但最高气温变暖幅度更大，变冷区在渝中和渝东南的岩溶区，主要是由最高气温的变冷造成的。 |
| 8. | It was well known that the main process of precipitation formation was collecting cloud water in the warm area and ice phase particles melting in the cold area . positive vertical velocity existed between 700hpa and 500hpa in the warm area and near surface in the cold area . wind convergence existed at the height of 700hpa , and divergence existed above and below the height of 700hpa
通过对降水云系的综合研究，建立了河南省春季层状云降水概念模型：暖区降水主要通过云水碰并形成，冷区降水机制以冰粒子融化等冷云过程为主;暖区700一50ohpa通常有上升气流，冷区上升气流分布在近地面附近: 700冲a存在风场的辐合，其上下则主要是辐散区;水汽主要集中在7o0hpa高度上，暖区水汽来自南、东南方向，冷区水汽以西南输送为主;暖区位势不稳定分布在o 。 |
| 9. | The width of raindrop size distribution in the warm area was narrow and its shape was single model . simulating results of one - dimension stratus model showed that the content of cloud water that grew up by deposition process was the largest in the warm area , and cloud water existed between 2km and 6km . in the warm area , the formation of rain water which existed between 1km and 4km was behind of the formation of cloud water , and the development of rainwater was depend on collecting cloud water
一维层状云模式模拟结果表明，暖区以凝华增长的云水为主，云水分布在2 6km高度；雨水在云水形成后产生，分布在1 4km之间，主要通过碰并云水增长；霰在雨水形成后产生，主要通过碰并云水增长，分布在云水区的中下层，霰形成后，雨水主要由霰融化产生。 |
| 10. | Rainfall is started mainly in cold portions . microphysics for ground rainfall consists of low - level warm portions in which precipitating particles are produced , growing through collision with cloud water and when descending into the warm portions below , ice - phase particles melt and continue to grow by collecting cloud water there . 4 )
降水主要以冷雨过程发动，地面降水形成的微物理过程分别为低层暖云过程产生并通过碰并云水增长、降落到暖区的冰相粒子融化和融化的冰相粒子在云的暖区收集云水继续长大等三部分组成。 |
