| 1. | Study on heat and water vapour transport during a rainstorm process in south china
一次华南暴雨过程中水汽输送和热量的研究 |
| 2. | In may and june , the moisture transports from " key regions " are all important to shandong summer rainfall
5 6月来自上述“关键区”水汽输送对山东夏季降水异常均有贡献。 |
| 3. | The strong convergence areas , which are coincide to the big rain belt , mostly lie in the planetary - scale water vapor transport . iii
夏季垂直积分的水汽输送通量强辐合区大多位于行星尺度水汽输送大值带中，和降水大值区之间有很好的对应关系。 |
| 4. | Big scope south airflow and vapor transport and convergence brought by meso - scale jet , offer vapor condition which rainstorm occur and develop
大范围偏南气流及其中的中尺度急流带来的水汽输送及辐合，为暴雨天气的发生、发展提供了低层水汽条件。 |
| 5. | The climate characteristics of global water vapor transport and global water balance are analyzed by using the ncep / ncar reanalysis data set from 1958 to 1998
利用ncep / ncar1958 1998年再分析资料分析了全球水汽输送时空分布的气候特征和全球水分平衡。 |
| 6. | The change of transport pattern from winter to summer closely relates with the change of the direction of the cross equatorial moisture transports , especially nearl 05 e and 45 e . ii
水汽输送形势的季节转变跟南北半球间的越赤道输送的转向密切相关，尤其是在105 e 、 45 e附近。 |
| 7. | ( 2 ) the yearly vapor water transport in northwest china is mainly consist of the west - southly air stream from the center - west of qinghai - xizang plateau and the east - southly air stream from the south of shanxi province
( 2 )西北地区全年水汽输送主要来自与其南面相邻的青藏高原中西部的西南暖湿气流以及陕西南部的东南暖湿气流。 |
| 8. | It is hard to satisfy the conditions of cold air and vapor together for torrent rainfall , in particularly the transportation of vapor in low atmosphere , f ) . it is one of the main reasons for the arid climate in ningxia
宁夏特殊的地理位置和地形特征造成了水汽输送的阻碍，且冷空气与水汽难以配合，这也是宁夏降水不足、气候干旱的天气学根本原因之一。 |
| 9. | The northward march of the southerly moisture transport with the summer monsoon transport over the east asian ( 110 - 130 e ) shows the feature of staged jumps . each jump relates with the large - scale important weather incident in china
( 2 )气候平均状态下，夏季偏南风水汽输送在东亚地区( 110 ? 130 e )的向北推进有阶段式跳跃的特点，每次跳跃均与影响我国的大型天气事件相联系。 |
| 10. | The 1st time coefficient shows the staged feature of the progression of the moisture transport over asian - australian monsoon region , which relates with the large - scale important weather incidents in asian - australian monsoon region . iv
第一特征向量对应的时间系数图表现了亚澳季风区4 - 9月份的水汽输送阶段性的时间演变特征，可反映夏季亚澳季风区的大型天气事件的发生变化过程。 |
