| 1. | The spatial and temporal distribution features of onset period of mean rainy season over asian monsoon region
亚洲季风区平均雨季起始期的时空分布特征 |
| 2. | Tropical biennial oscillation of moisture sink over asian - australian monsoon region and its relationship with atmospheric circulation
亚澳季风区内水汽汇的准两年振荡及其与大气环流的关系 |
| 3. | The results show that the strongest heat source heating center was located over the north - east of the bay of bengal in summer
结果表明：夏季亚洲季风区最强的热源中心位于孟加拉湾东北部一带。 |
| 4. | The study on precipitation field pointed out that most precipitation occurs in the monsoon area where exists the obvious rainy and dry season
指出降水量最大的区域主要在季风区，在季风降水区域，有明显的雨季和旱季。 |
| 5. | One can see that the maximum precipitation occurs in the monsoon areas , and their standard deviation is bigger in monsoon areas than the others
指出降水量最大的区域主要在季风区，而且季风区的降水均方差较大；降水在纬带分布上有着较大的连贯性。 |
| 6. | The study on the distribution feature of global land rainfall for march - may during 1948 - 2001 points out that the maximum precipitation occurs in the monsoon areas , and their standard deviation is bigger in monsoon areas than the others
分析了全球陆地3 - 5月降水量的分布特点。指出降水量最大区域主要在季风区，而且季风区降水均方差较大，降水在纬带分布上有着较大的连贯性。 |
| 7. | 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。 |
| 8. | In this study , we have analyzed the time - space variation characteristics of global cross - equatorial flow ( cef ) at the lower and upper rroposphere . especially for the monsoon region of the eastern hemisphere . the ncep / ncar reanalysis dataset used in this study are from 1958 to 1997
本文利用1958 1997年ncep / ncar逐月再分析资料，分析了全球各经度不同层次上越赤道气流( cef )的时空分布特征，尤其是东半球季风区夏季的越赤道气流。 |
| 9. | Climatological characteristics , which can provide some drought or flood years with large - scale background , are investigated for large - scale water vapor transport over asian - australian monsoon region based on vertically integrated water vapor flux by pentad from 1980 to 1997 . at the same time , the differences of moisture transport over the yangtze river basin between drought and flood and the moisture budgets over eastern china from april to september are examined . major results are as follows : i
使用1980 ? 1997年垂直积分的整层水汽输送通量资料，从气候平均的角度分析了亚澳季风区大尺度水汽输送演变和偏南风水汽输送在东亚地区推进的气候特征，为研究异常年份旱涝事件的产生提供了相应的大尺度背景；同时还讨论了长江流域旱涝年水汽输送的差异以及4 - 9月我国东部各区域的水分收支情况。 |
| 10. | Seasonal variations of water vapor transport over east asia monsoon region are studied , especially that in summer season . the results indicate that there are four vapor inflow corridors to fetch china : southwest corridor , south china sea corridor , southeast corridor and northwest corridor . it shows impact of south asia monsoon , south china sea monsoon , subtropical monsoon and middle latitude westerly belt on summer rainfall anomaly over china , respectively
分析了东亚季风区水汽输送的季节变化，并着重研究了夏季东亚季风区的水汽输送特征，指出夏季东亚季风区水汽输送有四条通道到达中国大陆：西南通道、南海通道、东南通道和西北通道，分别体现了南亚季风、南海季风、副热带季风和中纬度西风带对中国夏季降水的影响。 |
